Presentation at 2016 GeoConvention in Calgary, Alberta. Presentation covered best practices for the collection of samples then using advanced geochemistry and geoforensics to identify source zones of SCVFs.
The sole producer of the pigment Xirallic, used in metallic automotive paints, suffered significant damage from the 2011 Tōhoku earthquake and tsunami in Japan. This caused a shortage of the pigment, forcing Ford and Chrysler to limit some vehicles in red and black paints. The shortage also impacted other automakers, showing that a disruption in the supply chain of critical materials can have major consequences.
This document summarizes a student's geology research project analyzing soil transitions between amphibolite and mica schist outcrops. The student collected soil core samples along a slope using various techniques, including pH analysis and X-ray diffraction, to characterize the transition zone between the two lithologies. Analysis found a substantial change in soil pH and minerals between boreholes 3 and 4, identifying this as the transition zone. While XRD analysis proved unreliable due to weathered soil samples, comparison of hand samples best indicated the change in lithology. The research concluded the transition between the amphibolite and mica schist outcrops occurs between borehole sites 3 and 4.
Faulting is a geological process that involves the movement of rock masses along fractures or surfaces known as faults. Faults are common features in the Earth's crust, and they play a crucial role in shaping the Earth's surface. The causes and dynamics of faulting are complex and can result from various tectonic, geological, and stress-related factors
This document discusses metamorphic and metamorphosed ore deposits. It explains that metamorphic ore deposits form through the isochemical metamorphic re-equilibration and recrystallization of pre-existing materials. Contact metamorphism near magmatic bodies causes changes to fabric, mineralogy, and chemistry through processes like dewatering. Regional metamorphism can reach temperatures of 1100°C and pressures of 30 kbar, driving off volatiles and causing grain coarsening and foliation. Metamorphic fluids liberate economically valuable metals and elements and can form ore deposits as they circulate through metamorphosing rock.
A List Of Precious And Semi Precious Gemstones - Himalya QuartzHimalyaquartz1
Gems are minerals, rocks, or organic materials that have been popular for their beauty, durability, and rarity. Gems are used in polished to make jewelry or other human decorations. Most of the gems are hard, and some are too soft or can not be used in jewelry, so they are often displayed in museums. Basically, gems are made from minerals; But There are some exceptions, however, called organics. Pearls and amber are made by organic processes. That's why they are called Organics gem.
Carbonatite is an igneous rock consisting primarily of carbonate minerals crystallized from a carbonate magma. There are three main hypotheses for the origin of carbonatite melts: 1) immiscible separation of parental carbonated silicate magmas, 2) crystal fractionation of carbonated silicate magmas, and 3) low-degree partial melting of carbonated mantle peridotite. Carbonatites can be classified based on their main carbonate mineral component, such as dolomite-carbonatite or ferroan-carbonatite. They commonly occur as shallow intrusive bodies like volcanic necks, dykes, and cone-sheets associated with alkali-rich silicate ig
The sole producer of the pigment Xirallic, used in metallic automotive paints, suffered significant damage from the 2011 Tōhoku earthquake and tsunami in Japan. This caused a shortage of the pigment, forcing Ford and Chrysler to limit some vehicles in red and black paints. The shortage also impacted other automakers, showing that a disruption in the supply chain of critical materials can have major consequences.
This document summarizes a student's geology research project analyzing soil transitions between amphibolite and mica schist outcrops. The student collected soil core samples along a slope using various techniques, including pH analysis and X-ray diffraction, to characterize the transition zone between the two lithologies. Analysis found a substantial change in soil pH and minerals between boreholes 3 and 4, identifying this as the transition zone. While XRD analysis proved unreliable due to weathered soil samples, comparison of hand samples best indicated the change in lithology. The research concluded the transition between the amphibolite and mica schist outcrops occurs between borehole sites 3 and 4.
Faulting is a geological process that involves the movement of rock masses along fractures or surfaces known as faults. Faults are common features in the Earth's crust, and they play a crucial role in shaping the Earth's surface. The causes and dynamics of faulting are complex and can result from various tectonic, geological, and stress-related factors
This document discusses metamorphic and metamorphosed ore deposits. It explains that metamorphic ore deposits form through the isochemical metamorphic re-equilibration and recrystallization of pre-existing materials. Contact metamorphism near magmatic bodies causes changes to fabric, mineralogy, and chemistry through processes like dewatering. Regional metamorphism can reach temperatures of 1100°C and pressures of 30 kbar, driving off volatiles and causing grain coarsening and foliation. Metamorphic fluids liberate economically valuable metals and elements and can form ore deposits as they circulate through metamorphosing rock.
A List Of Precious And Semi Precious Gemstones - Himalya QuartzHimalyaquartz1
Gems are minerals, rocks, or organic materials that have been popular for their beauty, durability, and rarity. Gems are used in polished to make jewelry or other human decorations. Most of the gems are hard, and some are too soft or can not be used in jewelry, so they are often displayed in museums. Basically, gems are made from minerals; But There are some exceptions, however, called organics. Pearls and amber are made by organic processes. That's why they are called Organics gem.
Carbonatite is an igneous rock consisting primarily of carbonate minerals crystallized from a carbonate magma. There are three main hypotheses for the origin of carbonatite melts: 1) immiscible separation of parental carbonated silicate magmas, 2) crystal fractionation of carbonated silicate magmas, and 3) low-degree partial melting of carbonated mantle peridotite. Carbonatites can be classified based on their main carbonate mineral component, such as dolomite-carbonatite or ferroan-carbonatite. They commonly occur as shallow intrusive bodies like volcanic necks, dykes, and cone-sheets associated with alkali-rich silicate ig
This document provides a summary of alkali feldspar and plagioclase feldspar. It discusses their crystal structure, composition, physical and optical properties, paragenesis, and applications. Alkali feldspar includes orthoclase, sanidine, and microcline. Plagioclase feldspar is a solid solution between albite and anorthite. Both have important industrial uses such as in ceramics, glass, paints, plastics, and as gemstones. The document is presented by Atish Kumar Sahoo for his MTech course at the Department of Applied Geology.
Origin& evolution of magma ,magmatism related to plate tectonics.Devashish Sahu
This document summarizes a seminar on the origin and evolution of magma and its relationship to plate tectonics. It discusses how magma originates from partial melting of the solid earth due to increased temperature and pressure. Magma composition evolves through processes like fractional crystallization, assimilation, and magma mixing. Magmatism is related to plate tectonics through mechanisms like decompression melting at mid-ocean ridges and continental rifts, flux melting near subduction zones, and intraplate volcanism from mantle plumes not associated with plate boundaries. Examples discussed include the Deccan Traps basalts formed by a mantle plume in India.
This document discusses the mining of hydrothermal deposits from ocean vents. Hydrothermal vents on the ocean floor form when superheated water rich in dissolved minerals emerges from below the earth's crust. As the water cools upon contacting cold ocean water, minerals precipitate out and form chimney-like structures around each vent. Over time, these deposits can become massive sulfide ore bodies. The document outlines various methods proposed for mining valuable minerals from hydrothermal vent fluids, such as using pipes to bring the fluid to the surface for processing, but acknowledges challenges around maintaining minerals in solution during transport and environmental impacts.
plano de aula detalhado " Bruna e a galinha D'angola"Juciara Brito
trabalho realizado para apresentação em Amargosa Ba.
plano de aula do mes de novembro da escola José Soares dos Santos ( Ubaíra BA ) este plano encontra-se no portfólio apresentado ao PACTO em 2013.
The document provides information about the self potential (SP) method of geophysical surveying. It discusses the background of SP surveying and its applications in mineral exploration, groundwater mapping, and engineering. It describes the various types of potentials that can generate SP anomalies, including electrokinetic, diffusion, Nernst, mineral, and electrochemical potentials. The document outlines how SP is measured in the field using fixed-base and gradient methods. It also discusses interpreting SP data qualitatively based on anomaly shape, amplitude, and polarity and quantitatively by modeling anomaly sources as simple geometric shapes.
The document summarizes the theory of supercontinent cycles, where the Earth's continents periodically assemble into a single landmass called a supercontinent and then break apart over hundreds of millions of years. It describes how Pangaea formed approximately 300 million years ago before breaking apart, and how earlier supercontinents like Rodinia and Columbia also existed. It explains that the movement of tectonic plates will likely cause the continents to reconverge into a new supercontinent in about 200 million years. This cyclical assembly and breakup of supercontinents over billions of years has shaped the Earth's geography and geology.
The document discusses lead and zinc deposits found in India. It describes the chief ores of lead (galena, cerussite, anglesite) and zinc (sphalerite, smithsonite). It then discusses several major lead-zinc deposits in India, including Rampura-Agucha and Zawar belts, characterized by stratabound sedimentary hosted deposits. Other deposits mentioned include Sargipalli and Mamandur, which also feature sedimentary hosted lead-zinc mineralization. The document provides details on the geology, mineralization, and genesis of these important deposits.
Paired metamorphic belts occur where zones of high-pressure low-temperature metamorphism are parallel to zones of low-pressure high-temperature metamorphism. They were first recognized in Japan and form due to subduction of oceanic crust beneath continental crust. Paired metamorphic belts support the theory of plate tectonics, as the contrasting pressure-temperature conditions in the two parallel belts can be explained by ocean-continent convergence. Examples of paired metamorphic belts are found throughout the basement rocks of the former Gondwanaland supercontinent.
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
Petrology is the branch of geology that studies rocks. It includes the origin and formation of rocks (petrogenesis) and their classification and description (petrography). There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma or lava. Sedimentary rocks form from the compaction and cementation of sediments. Metamorphic rocks form from changes to existing igneous and sedimentary rocks via heat, pressure, and chemical reactions.
Stratigraphy of Layered mafic Intrusions in the The Stillwater complexSharik Shamsudhien
The document summarizes the stratigraphy and characteristics of the Stillwater Complex, a layered mafic intrusion in Montana. It describes the different rock series that make up the Complex from bottom to top, including a Basal Series containing ores, an Ultramafic Series with peridotite and orthopyroxenite zones exhibiting rhythmic layering, and a Banded Series containing norites and gabbros. It notes the Complex was uplifted and eroded, exposing its steeply dipping layers. The document also provides general characteristics of layered intrusions, such as their perpendicular layering that can be cryptic or rhythmic and extend over large areas.
Amphibole is a type of silicate mineral that commonly forms long prismatic crystals and has two cleavages that intersect at 124 degrees. Some common varieties of amphibole include cummingtonite, grunerite, hornblende, tremolite, actinolite, glaucophane, and riebeckite. Amphibole has a variety of uses including as gemstones, facing stone on buildings, floor tiles, crushed for highway construction, and decorative materials.
The document discusses the Sandur schist belt located in eastern Dharwar craton, India. It describes the belt's stratigraphy consisting of six formations deposited in different environmental conditions. SHRIMP U-Pb dating of zircon from volcanic rocks in the Vibudigudda formation provided ages of 2658±14 and 2691±18 million years. The belt was metamorphosed approximately 2700 million years ago due to intrusion of the younger Closepet granite. It underwent folding and thrusting during the deformation associated with the granite emplacement.
Kutch is an East-west Oriented pericraton Rift basin Situated between Nagar Parkar Fault in North and Kathiawar Uplift in South.
Here we will discuss Geology and its Sequence Stratigraphy.
Igneous rock forms through the cooling and solidification of magma or lava. It is classified based on several properties including genesis, texture, color, and chemical composition. Based on genesis, igneous rocks are classified as plutonic (cooled at depth), hypabyssal (cooled at shallow depth), or volcanic (cooled on the surface). Texture classifications include phaneritic, aphenitic, porphyritic, and poikilitic. Color classifications are based on the percentage of mafic minerals and include leucocratic, mesocratic, melanocratic, and hypermelanic. Chemical composition classifications include peraluminous, metaaluminous, subaluminous, and several
O documento discute os processos geomorfológicos que moldam o relevo, incluindo a erosão, transporte e deposição de sedimentos. Apresenta os principais tipos de relevo resultantes da interação entre forças endógenas e exógenas, como cuestas, domos, falhas e horsts & grabens. Também aborda a classificação da vulnerabilidade dos solos à erosão e métodos de controle, como a plantação em nível e plantio direto.
This document provides an overview of sedimentary rocks, including their classification and common types. It discusses how sedimentary rocks form from sediments produced by weathering and are later cemented. The document classifies sedimentary rocks into detrital rocks (formed from rock fragments), chemically formed rocks like limestone, and residual deposits like laterite and soils. Detrital rocks like sandstone and shale are the most abundant sedimentary rocks, comprising around 95% of sedimentary layers and 4% and 0.75% of the Earth's crust, respectively.
The Rb-Sr dating method uses the radioactive decay of rubidium-87 to strontium-87 to date rocks and minerals. It works by measuring the ratio of rubidium to strontium, and the ratio of radiogenic strontium-87 to strontium-86, in samples. By plotting these ratios on a graph called an isochron, scientists can determine the age of the sample from the slope of the line. The method relies on the samples forming a closed system and not being altered after formation. It is useful for determining the age of igneous and metamorphic rocks.
The document outlines the design of a wetland methane flux chamber to measure methane emissions from forest soils and marshes. The objectives are to design a portable chamber compatible with a LiCor 7810 Trace Gas Analyzer that can cover 2m tall wetland vegetation. A literature review informed the design process. A prototype chamber was built out of PVC and tested in the laboratory by collecting soil samples and measuring methane levels over time. The results were analyzed to calculate methane flux and compare different soils and chamber setups.
The document outlines the design of a methane flux chamber to measure methane emissions from wetland environments. It discusses the background on methane emissions from wetlands and the need to accurately measure these emissions. The objectives are to design, build, and test a portable chamber that can cover 2m tall vegetation and interface with a Licor 7810 Trace Gas Analyzer. A literature review informed the design process. Methods will involve building a prototype chamber, testing it on campus, and taking it to field sites to obtain methane emission data from marshes. Recommendations for improvements to the design are provided.
This document provides a summary of alkali feldspar and plagioclase feldspar. It discusses their crystal structure, composition, physical and optical properties, paragenesis, and applications. Alkali feldspar includes orthoclase, sanidine, and microcline. Plagioclase feldspar is a solid solution between albite and anorthite. Both have important industrial uses such as in ceramics, glass, paints, plastics, and as gemstones. The document is presented by Atish Kumar Sahoo for his MTech course at the Department of Applied Geology.
Origin& evolution of magma ,magmatism related to plate tectonics.Devashish Sahu
This document summarizes a seminar on the origin and evolution of magma and its relationship to plate tectonics. It discusses how magma originates from partial melting of the solid earth due to increased temperature and pressure. Magma composition evolves through processes like fractional crystallization, assimilation, and magma mixing. Magmatism is related to plate tectonics through mechanisms like decompression melting at mid-ocean ridges and continental rifts, flux melting near subduction zones, and intraplate volcanism from mantle plumes not associated with plate boundaries. Examples discussed include the Deccan Traps basalts formed by a mantle plume in India.
This document discusses the mining of hydrothermal deposits from ocean vents. Hydrothermal vents on the ocean floor form when superheated water rich in dissolved minerals emerges from below the earth's crust. As the water cools upon contacting cold ocean water, minerals precipitate out and form chimney-like structures around each vent. Over time, these deposits can become massive sulfide ore bodies. The document outlines various methods proposed for mining valuable minerals from hydrothermal vent fluids, such as using pipes to bring the fluid to the surface for processing, but acknowledges challenges around maintaining minerals in solution during transport and environmental impacts.
plano de aula detalhado " Bruna e a galinha D'angola"Juciara Brito
trabalho realizado para apresentação em Amargosa Ba.
plano de aula do mes de novembro da escola José Soares dos Santos ( Ubaíra BA ) este plano encontra-se no portfólio apresentado ao PACTO em 2013.
The document provides information about the self potential (SP) method of geophysical surveying. It discusses the background of SP surveying and its applications in mineral exploration, groundwater mapping, and engineering. It describes the various types of potentials that can generate SP anomalies, including electrokinetic, diffusion, Nernst, mineral, and electrochemical potentials. The document outlines how SP is measured in the field using fixed-base and gradient methods. It also discusses interpreting SP data qualitatively based on anomaly shape, amplitude, and polarity and quantitatively by modeling anomaly sources as simple geometric shapes.
The document summarizes the theory of supercontinent cycles, where the Earth's continents periodically assemble into a single landmass called a supercontinent and then break apart over hundreds of millions of years. It describes how Pangaea formed approximately 300 million years ago before breaking apart, and how earlier supercontinents like Rodinia and Columbia also existed. It explains that the movement of tectonic plates will likely cause the continents to reconverge into a new supercontinent in about 200 million years. This cyclical assembly and breakup of supercontinents over billions of years has shaped the Earth's geography and geology.
The document discusses lead and zinc deposits found in India. It describes the chief ores of lead (galena, cerussite, anglesite) and zinc (sphalerite, smithsonite). It then discusses several major lead-zinc deposits in India, including Rampura-Agucha and Zawar belts, characterized by stratabound sedimentary hosted deposits. Other deposits mentioned include Sargipalli and Mamandur, which also feature sedimentary hosted lead-zinc mineralization. The document provides details on the geology, mineralization, and genesis of these important deposits.
Paired metamorphic belts occur where zones of high-pressure low-temperature metamorphism are parallel to zones of low-pressure high-temperature metamorphism. They were first recognized in Japan and form due to subduction of oceanic crust beneath continental crust. Paired metamorphic belts support the theory of plate tectonics, as the contrasting pressure-temperature conditions in the two parallel belts can be explained by ocean-continent convergence. Examples of paired metamorphic belts are found throughout the basement rocks of the former Gondwanaland supercontinent.
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
Petrology is the branch of geology that studies rocks. It includes the origin and formation of rocks (petrogenesis) and their classification and description (petrography). There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma or lava. Sedimentary rocks form from the compaction and cementation of sediments. Metamorphic rocks form from changes to existing igneous and sedimentary rocks via heat, pressure, and chemical reactions.
Stratigraphy of Layered mafic Intrusions in the The Stillwater complexSharik Shamsudhien
The document summarizes the stratigraphy and characteristics of the Stillwater Complex, a layered mafic intrusion in Montana. It describes the different rock series that make up the Complex from bottom to top, including a Basal Series containing ores, an Ultramafic Series with peridotite and orthopyroxenite zones exhibiting rhythmic layering, and a Banded Series containing norites and gabbros. It notes the Complex was uplifted and eroded, exposing its steeply dipping layers. The document also provides general characteristics of layered intrusions, such as their perpendicular layering that can be cryptic or rhythmic and extend over large areas.
Amphibole is a type of silicate mineral that commonly forms long prismatic crystals and has two cleavages that intersect at 124 degrees. Some common varieties of amphibole include cummingtonite, grunerite, hornblende, tremolite, actinolite, glaucophane, and riebeckite. Amphibole has a variety of uses including as gemstones, facing stone on buildings, floor tiles, crushed for highway construction, and decorative materials.
The document discusses the Sandur schist belt located in eastern Dharwar craton, India. It describes the belt's stratigraphy consisting of six formations deposited in different environmental conditions. SHRIMP U-Pb dating of zircon from volcanic rocks in the Vibudigudda formation provided ages of 2658±14 and 2691±18 million years. The belt was metamorphosed approximately 2700 million years ago due to intrusion of the younger Closepet granite. It underwent folding and thrusting during the deformation associated with the granite emplacement.
Kutch is an East-west Oriented pericraton Rift basin Situated between Nagar Parkar Fault in North and Kathiawar Uplift in South.
Here we will discuss Geology and its Sequence Stratigraphy.
Igneous rock forms through the cooling and solidification of magma or lava. It is classified based on several properties including genesis, texture, color, and chemical composition. Based on genesis, igneous rocks are classified as plutonic (cooled at depth), hypabyssal (cooled at shallow depth), or volcanic (cooled on the surface). Texture classifications include phaneritic, aphenitic, porphyritic, and poikilitic. Color classifications are based on the percentage of mafic minerals and include leucocratic, mesocratic, melanocratic, and hypermelanic. Chemical composition classifications include peraluminous, metaaluminous, subaluminous, and several
O documento discute os processos geomorfológicos que moldam o relevo, incluindo a erosão, transporte e deposição de sedimentos. Apresenta os principais tipos de relevo resultantes da interação entre forças endógenas e exógenas, como cuestas, domos, falhas e horsts & grabens. Também aborda a classificação da vulnerabilidade dos solos à erosão e métodos de controle, como a plantação em nível e plantio direto.
This document provides an overview of sedimentary rocks, including their classification and common types. It discusses how sedimentary rocks form from sediments produced by weathering and are later cemented. The document classifies sedimentary rocks into detrital rocks (formed from rock fragments), chemically formed rocks like limestone, and residual deposits like laterite and soils. Detrital rocks like sandstone and shale are the most abundant sedimentary rocks, comprising around 95% of sedimentary layers and 4% and 0.75% of the Earth's crust, respectively.
The Rb-Sr dating method uses the radioactive decay of rubidium-87 to strontium-87 to date rocks and minerals. It works by measuring the ratio of rubidium to strontium, and the ratio of radiogenic strontium-87 to strontium-86, in samples. By plotting these ratios on a graph called an isochron, scientists can determine the age of the sample from the slope of the line. The method relies on the samples forming a closed system and not being altered after formation. It is useful for determining the age of igneous and metamorphic rocks.
The document outlines the design of a wetland methane flux chamber to measure methane emissions from forest soils and marshes. The objectives are to design a portable chamber compatible with a LiCor 7810 Trace Gas Analyzer that can cover 2m tall wetland vegetation. A literature review informed the design process. A prototype chamber was built out of PVC and tested in the laboratory by collecting soil samples and measuring methane levels over time. The results were analyzed to calculate methane flux and compare different soils and chamber setups.
The document outlines the design of a methane flux chamber to measure methane emissions from wetland environments. It discusses the background on methane emissions from wetlands and the need to accurately measure these emissions. The objectives are to design, build, and test a portable chamber that can cover 2m tall vegetation and interface with a Licor 7810 Trace Gas Analyzer. A literature review informed the design process. Methods will involve building a prototype chamber, testing it on campus, and taking it to field sites to obtain methane emission data from marshes. Recommendations for improvements to the design are provided.
Using environmental forensics techniques to identify fugitive methane. Techniques included VOCs, fixed gases, stable isotopes, and radioactive carbon to identify soil gas samples from a variety of urban settings.
Increasing interest by governments worldwide on reducing CO2 released into the atmosphere form a nexus of of opportunity with enhanced oil recovery which could benefit mature oil fields in nearly every country. Overall approximately two-thirds of original oil in place (OOIP) in mature conventional oil fields remains after primary or primary/secondary recovery efforts have taken place. CO2 enhanced oil recovery (CO2 EOR) has an excellent record of revitalizing these mature plays and can dramatically increase ultimate recovery. Since the first CO2 EOR project was initiated in 1972, more than 154 additional projects have been put into operation around the world and about two-thirds are located in the Permian basin and Gulf coast regions of the United States. While these regions have favorable geologic and reservoir conditions for CO2 EOR, they are also located near large natural sources of CO2.
In recent years an increasing number of projects have been developed in areas without natural supplies, and have instead utilized captured CO2 from a variety of anthropogenic sources including gas processing plants, ethanol plants, cement plants, and fertilizer plants. Today approximately 36% of active CO2 EOR projects utilize gas that would otherwise be vented to the atmosphere. Interest world-wide has increased, including projects in Canada, Brazil, Norway, Turkey, Trinidad, and more recently, and perhaps most significantly, in Saudi Arabia and Qatar. About 80% of all energy used in the world comes from fossil fuels, and many industrial and manufacturing processes generate CO2 that can be captured and used for EOR. In this 30 minute presentation a brief history of CO2 EOR is provided, implications for utilizing captured carbon are discussed, and a demonstration project is introduced with an overview of characterization, modeling, simulation, and monitoring actvities taking place during injection of more than a million metric tons (~19 Bcf) of anthropogenic CO2 into a mature waterflood.
Longer versions of the presentation can be requested and can cover details of geologic and seimic characterization, simulation studies, time-lapse monitoring, tracer studies, or other CO2 monitoring technologies.
Use of GCxGC-TOFMS in litigious mixed condensate plumes: Environmental forens...Chemistry Matters Inc.
Authors: Court D. Sandau and Lisa N. Kates
Chemistry Matters Inc.
Abstract; Condensate is a complex mixture of light petroleum hydrocarbons that is primarily used to dilute heavy crude oil for transport through pipelines. Many heavy oils, especially bitumen from the oil sands in northern Alberta, use condensate to dilute the bitumen to allow the product to flow to refineries where the oil can be upgraded. This is where the term ‘Dilbit’ was derived. Condensate is valuable; it can be recycled and reused and is frequently transported through the North American pipeline network. Pipelines gather at pipeline terminals where there can be multiple sources and multiple suppliers of different types of condensates. When leaks occur at these terminals, it can be difficult to determine the exact source of the leak, especially if pipeline integrity seems intact. GCxGC-TOFMS is the ideal technique to examine mixed condensate plumes as it allows the comprehensive fingerprint of the condensate to be determined and simultaneously provides substantial data to evaluate weathering and plume movement. In addition, the amount of chemicals measured using GCxGC-TOFMS can allow source apportionment of multiple sources so that allocation of the cleanup responsibility can be made. This presentation will discuss the use of GCxGC-TOFMS in legal case studies involving mixed condensate plumes. Real scenarios of condensate plumes will be presented showing how GCxGC-TOFMS data clarified the results compared to conventional analysis. This presentation will also cover the hurdles of using a novel and unconventional technique for litigation proceedings.
The document discusses using forensic techniques to identify sources of fugitive methane found in subsurface soils in a municipality. Level 1 analysis using fixed gas composition, hydrocarbon fingerprinting, and VOC analysis ruled out thermogenic sources but could not differentiate between landfill and sewage sources. Level 2 analysis using carbon dating, and stable isotope analysis of methane indicated one sampling point was likely degrading landfill material and another was a mixed source of landfill and organic soils. The analysis identified potential methane sources to help the client determine appropriate actions.
Presentation from 2007 to AWMA conference on vapour intrusion. Presentation covers the environmental forensics investigation of gases to identify the sources of the potential vapour intrusion. Techniques used both standard gas analysis as well as isotopic analysis of selected gases to identify the likely sources.
Presentation given by Alexandre Morin of SINTEF Energy Research on "IMPACTS - The impact of the quality of CO2 on transport and storage behaviour" at the EC FP7 Projects: Leading the way in CCS implementation event, London, 14-15 April 2014
La ricerca e l’innovazione tecnologica per il Servizio Idrico IntegratoServizi a rete
The document summarizes research projects conducted by SMAT Research Center in Turin, Italy. It describes the center's facilities and partnerships. It then provides brief summaries of multiple research projects, including estimating the vulnerability of groundwater resources to climate change, testing hydrodynamic cavitation for drinking water disinfection, modeling wastewater treatment plants, and developing biomethane production and an early warning water monitoring system.
OLADE-Slide-Deck-compressed para ver.pdfHenryApaza12
The document introduces Norm Sacuta and Brittney Musleh, who will present on carbon capture and storage. It then provides an overview of the Petroleum Technology Research Centre (PTRC), including that it is a not-for-profit research organization that has studied CO2 utilization and storage for 23 years through projects like Aquistore and Weyburn-Midale. The presentation outline indicates it will cover topics ranging from capture and transport technologies to monitoring CO2 storage sites.
- Pioneer Energy has developed a portable system that can generate high-purity CO2 and electricity from raw field gas or biomass on-site at oil fields.
- The fully portable system fits on a semi-trailer and can produce 200-1,000 mcf/day of CO2. A prototype has been built and tested.
- The system addresses the lack of available and affordable CO2 for fracking and enhanced oil recovery (EOR) projects. It provides an on-site source of CO2 without the need for pipelines or trucking.
- By using flare gas, a wasted resource, the system also addresses environmental issues. It has the potential to enable more small-
Cost (& Time) Optimization of Hydrogeological StudiesGidahatari Agua
Cost optimization has to identify the most common problems to the hydrogeological investigation as travel time and transport issues, seasonal restrictions, personal availability, protocols, etc. This post is focused on strategies and best practices for cost (& time) optimization, specially for hydrogeological investigation on mining projects.
Advanced Fossil Energy Technologies: Presentation by the US Dept of Energy Of...atlanticcouncil
This document discusses the goals and activities of the US Department of Energy's Office of Clean Coal, including its vision of enabling the environmentally-sound use of coal and fossil fuels through research into carbon capture and storage technologies. It outlines four goals: demonstrating near-zero emission fossil technologies; gaining public and regulatory acceptance of CO2 storage; conducting high-risk R&D on advanced coal technologies; and driving international collaboration on CCS. It also provides an overview of the office's major CCS demonstration projects currently underway or planned, which involve capturing and storing millions of tons of CO2 annually through techniques like pre- and post-combustion capture at coal power plants and industrial facilities.
Development of an aqueous ammonia-based post-combustion capture technology fo...Global CCS Institute
To highlight the research and achievements of Australian researchers, the Global CCS Institute with ANLEC R&D will hold a series of webinars throughout 2016. Each webinar highlights a specific ANLEC R&D research project and the relevant report found on the Institute’s website. The fifth webinar of the series looked at the development of an aqueous ammonia-based post-combustion capture technology for Australian conditions.
CSIRO has been developing aqueous ammonia (NH3)-based post-combustion CO2 capture (PCC) technology for its application under Australian conditions since 2008. Previous pilot-plant trials at Delta Electricity’s Munmorah Power Station demonstrated the technical feasibility of the process and confirmed some of the expected benefits. With further support from the Australian Government and ANLEC R&D, CSIRO has worked closely with universities in Australia and China to develop an advanced aqueous NH3-based CO2 capture technology. The advanced technology incorporates a number of innovative features which significantly improve its economic feasibility. This webinar presented the advancements made from a recently completed project funded by ANLEC R&D, and was presented by Dr Hai Yu and Dr Kangkang Li from CSIRO Energy.
Saudi Aramco has developed a comprehensive technology roadmap for carbon management that focuses on CO2 capture, storage, and utilization. As part of this roadmap, Saudi Aramco plans to implement a CO2-EOR demonstration project in Saudi Arabia by 2013/2014. This project will inject CO2 into an oil field using 4 injectors and 4 producers to test CO2-EOR and monitor CO2 storage. It aims to evaluate CO2 potential for EOR and storage while testing new monitoring and surveillance technologies to track the CO2 plume and changes in oil saturation.
Workers were evacuated from Metropolitan Colliery on March 21st 2019 after gas levels rose in the longwall return. At 6:00pm, high CO2 was detected at the longwall face, causing operations to stop. At 7:15pm, all underground workers began withdrawing as CH4 levels continued rising. By 8:45pm all workers had been withdrawn and accounted for on the surface. Gas levels in the longwall return reached 16.1% CH4 and 15.9% CO2, while levels in the main upcast shaft were 3.01% CH4 and 4.16% CO2. Workers remained out of the mine for seven days as 2.9 million cubic metres of 38% CH
This presentation summarizes the findings of an air emissions and odour sampling program conducted on the Baytex Reno Field. The data was collected in response to local resident complaints of odours in the area. The study collected samples using industry standard procedures and analyzed by state of the art analytical equipment. The results showed that no human health effects were exceeded and that no odour thresholds were exceeded. This study exemplifies how odours may be detected even though the standard analytical practices are not able to measure the odiferous compounds. PAHs were measured in the study and show a petrogenic ligher signature present the ambient air in the region as well as diesel markers from the trucking activity. This summary report was presented on January 22, 2014 to the Peace River AER Public Proceeding (1769924).
CCUS in the USA: Activity, Prospects, and Academic Research - plenary presentation given by Alissa Park at the UKCCSRC Cardiff Biannual Meeting, 10-11 September 2014
Similar to GeoConvention2016_Identifying Surface Casing Vent Flows (SCVF) Using Geoforensics (20)
Fixing False Negatives, Using 2DGC-TOFMS to Correctly Identify Ignitable Liqu...Chemistry Matters Inc.
Wildfires continue to grow in frequency and intensity. Over 80% of wildfires are human caused, with over 20% being attributed to acts of arson. The ability to detect ignitable liquid residues (ILRs) in wildfire debris samples can be very problematic compared to structural fire debris samples.
Forensic methods used in the analysis of wildfire debris are complicated by the presence of natural interferences. Wildfires provide exceptionally difficult matrices compared to structural fires due to the facts that: ILRs are present at lower concentrations; ILRs are more dispersed; natural compounds are present at very high concentrations; structural similarity of natural compounds to ILR compounds; and matrix combustion forms other interfering compounds.
The resolving power of comprehensive two-dimensional gas chromatography (GCxGC, 2DGC) combined with the sensitivity of a TOF-MS permits superior separation and detection of ILRs compared to conventional gas chromatography (1DGC). The high abundance of natural interferences dwarfs the ILR compounds in size and will mask their detection using conventional 1DGC. As arsonous wildfires can ignite with very low volumes of accelerants, better detection limits are required in order to find and identify ILRs in wildfire debris samples.
Case samples analyzed on both 1DGC and 2DGC showed re-analysis by 2DGC changed 7% of negative samples to positive for ILR, and 22% went from tentative to positive for ILR. Inspection of the Stauffer compounds shows some groups are more useful for ILR identification than others. The Three Musketeers Group was ubiquitous, while the Twin Towers and Five Fingers Groups were non-detects by 1DGC but present in up to 90% of positive samples by 2DGC. In addition, the use of 2DGC allows expansion of the targeted list of compounds to expand to all compounds present in gasoline which increase to over 2000 compounds, potentially allowing for gasoline fingerprinting.
Unscrambling Contaminant Mixtures to Determine their Chemical FingerprintsChemistry Matters Inc.
Many contaminated sites have mixed plumes or contaminants of concern from multiple potential sources. Examples of mixed plumes could include mixed free phase petroleum plumes (e.g. condensate) or polycyclic aromatic hydrocarbons (PAHs) from crude oil spills mixing with upstream or local anthropogenic sources (storm water runoff) of PAHs in sediments.
There are several advanced statistical techniques that can be used to determine the number and different sources of contaminant present on the site. In addition, these statistical tools can also apportion the amount of contaminants in each sample, thereby allowing liability to be distributed according the chemistry of the contaminants and those responsible for the release. Apportionment is important for litigious cases as it allows the calculation of who should pay for what portion of the cleanup.
Tools using positive matrix factorization (PMF) have been developed by US EPA but are no longer being supported are still publicly available to use. These techniques can be applied to many different chemical mixtures such as condensates or mixed petroleum hydrocarbon plumes. We have successfully applied the technique to PAHs from sediment data to allocate the source of the PAHs in the sediments to sources identified by the models. Unfortunately, these models are not definitive and provide multiple conclusions depending on their starting point which can make interpretation difficult and sometimes questionable, especially for litigation proceedings.
This presentation provides a summary of statistical tools used for chemical fingerprinting as well as the use of PMF and Bayesian modelling in order to provide some guidance on model usage for contaminant apportionment. The models need to be applied conservatively and require chemistry interpretation to elucidate what end members have been identified by the model and if those end members make sense. The models will be applied to a real case study scenarios to demonstrate their application.
Lawyers, regulators and environmental professionals involved in spill monitoring and liability determination will find this presentation educational in how these statistical models are able to determine sources and amounts of those sources of contaminants on site.
River sediment contains natural organic material, largely derived from allochthonous sources, meaning a source from outside the river. This is particularly important when regarding polycyclic aromatic hydrocarbons (PAHs), which can have sources hundreds of kilometers from a sampling point within the river catchment. In fact, every river can contain PAHs from a source other than that which is the focus of a remedial investigation, and consideration of this is very important.
Presentation of the detection of PAHs in relation to guidelines is a requirement for regulatory purposes. However, if those PAHs are natural, or at least originate from a source that is unrelated to the investigation, why take responsibility for them?
In order to determine the source of PAHs it is important to collect the right kind of samples (fine grained, highly organic sediment), analyse for the right kind of chemical package (include alkylated PAHs), and interpret the results using the right kind of techniques.
This presentation will describe the correct, and incorrect use of environmental forensics techniques using example datasets from our work in Canadian oil spill response and US CERCLA investigations. It will focus on how to construct and interpret PAH fingerprints and ratios, and the use of statistics such as PCA. Environmental professionals involved in spill remediation or site monitoring will find this presentation applicable.
This document provides an outline for a presentation on using statistical analysis of soil data from site investigations to better understand environmental conditions at a site. It discusses a case study of a 50+ year old facility where extensive soil data had been collected over many years but significant remediation was still planned. The presentation aims to show how applying some basic statistics to compare the soil data to guidelines can reveal useful insights hidden in the data and potentially avoid unnecessary remediation costs. Key points that will be covered include reviewing site management practices, examining the soil data in detail, applying statistical analysis techniques, and reviewing the outcomes of a case study that incorporated these elements.
Multiple Lines of Evidence of PAH Fingerprinting and Source Apportionment of ...Chemistry Matters Inc.
Polycyclic aromatic hydrocarbons (PAHs) are ubiquitous in the environment. They are produced naturally through forest fires with some congeners having biogenic origins. They are also produced anthropogenically through all burning or combustion processes.
Profiling ignitable liquid residues (ILRs) and potential interfering compound...Chemistry Matters Inc.
During the 8th Multidimensional Chromatography Workshop 2017 in Toronto, Ontario, Dr. Court Sandau presented on profiling ignitable liquid residues (ILRs) and potential interfering compounds during arson and arsonous wildfire investigations.
245TCP - Perspectives on PCDD/Fs from a Review of Industrial Processes and Hi...Chemistry Matters Inc.
This document discusses the production of 245-TCP and the formation of PCDD/Fs during this process. It summarizes that the production process and any impurities in the starting materials can result in different PCDD/F fingerprints. Historical production methods, process diagrams, and experimental data are reviewed to understand how different fingerprints may form depending on the specific industrial process used. Determining these fingerprints can help identify sources of dioxin contamination at historical industrial sites.
Demystifying the Chain of Custody & Forensic Arson Analysis - IAAI 2017Chemistry Matters Inc.
The results for ignitable liquid residue (ILR) analysis depend on early decisions. Sometimes, results depend on decisions made before the investigator even leaves for the arson investigation site.
How to Maintain Legal Chain of Custody
Legal chain of custody is not only about documentation. You do need to document samples and sampling procedures, but as the custodian of samples, you should also be implementing processes and procedures that prevent cross contamination.
During this course, the legal sampling and legal chain of custody process will be discussed along with implications of the sampling process on the analytical results. This will include a discussion on appropriate sampling containers and how it can impact your results.
With this course, you will learn how sampling can impact the chemistry of your results and what you can do about it as well as developing a complete understanding of chain of custody for your courtroom defense.
ILR Analysis Methods
The sampling at the investigation site provides the best opportunity to optimize the detection of ILRs. Several points will be discussed on how to accomplish the best results possible.
Once samples are submitted to the laboratory, they are processed to determine if ILRs are present and what type of ILRs are on the samples. There are different methods for analysis of ILRs and these methods will be discussed.
ILR chemical analysis requires the determination of compounds present in samples collected from the investigation. These compounds need to be present at certain concentrations (above the laboratory detection limits), in certain ratios (patterns match known ILR patterns), and have enough of the marker compounds to determine the type of ILR used on the investigation.
Not all methods and results are equal. Learning the basics of ILR analysis will allow you to ask the hard and appropriate questions about your sample results. It may also help explain apparent false positives from canine detection units.
The Importance of Reference Samples
The topic of reference samples, sometimes incorrectly referred to as 'control samples' will be discussed.
All matrices collected at fire investigations can contain marker compounds used for ILR identification but are not present on those materials because of arson. Reference samples are key samples to any arson investigation and must be collected with purpose for every investigation.
The interferences present in reference samples can help ILR analysis determine the compounds that are present in background locations. This provides further insight for the investigation.
The use of reference samples is especially important in arsonous wildfire investigations. Since ILR marker compounds can be formed in the combustion process, ILR detection in arsonous wildfire samples can be inconclusive if not considered properly.
Using Fingerprinting Techniques and Multivariate Statistics to Identify Natur...Chemistry Matters Inc.
This document presents the findings of a study using fingerprinting techniques and multivariate statistics to distinguish between natural and anthropogenic salinity in soil samples. Radar plots and statistical analysis of parameters like chloride, calcium, sodium, and sulfate concentrations were used to group 54 site samples. Three distinct fingerprint patterns were identified, with two samples having natural salinity fingerprints similar to background samples, 48 samples having anthropogenic fingerprints different than background, and 3 samples having another separate fingerprint. Spatial analysis found the sample groupings correlated with wellsite features. The techniques were able to distinguish anthropogenic impacts despite low overall salinity levels.
Arson: The Science of Fire and Chemical Fingerprints Left Behind - MRU 2017Chemistry Matters Inc.
Wildfire frequency, severity and damages are increasing as climate change causes earlier snow melts and overall drier conditions. Forest fire can be caused by natural through lightning strikes, but the majority of wildfires are caused by humans. Of the 1200 wildfires reported in Alberta each year, over half are human caused. It is the job of a fire investigator to gather evidence at wildfires to determine the origin and causes of the wildfire. Roles of the investigator may include fire scene examination through to delivering court room evidence.
Fire investigations require the highest quality in sampling, legal chain of custody & sample handling, and testing & interpretation of ignitable liquid residues (ILRs). This role can be ideally filled by a chemist/scientist who has an in depth understanding of how all facets of a field program and how the analysis of samples can impact the interpretation and results. Ultimately, prosecution will depend on reliable ILR results and relaying these results to the fire investigators.
Dr. Sandau, and his team at Chemistry Matters, are one of Canada’s leading resources for wildfire arson investigation and have led investigations for some of the largest wildfires in North America. This presentation will explore the chemistry behind wildfire investigations. The chemistry starts from the field work and sampling with the use of canine detection units. It is then carried forward to the instrumentation used for laboratory analysis which is used for the interpretation and ending in testifying in a courtroom setting. This presentation will examine the evolution of our detection systems that allow us to measure molecules at the lowest levels and use their patterns to chemically fingerprint the ignitable liquid residues and other products used which provides valuable cutting edge evidence for potential convictions.
Where Does Toluene Come From? - Petrogenic families and biogenic loners, AGAT...Chemistry Matters Inc.
Specific ecological niches support the accumulation of biologically formed toluene, and the concentrations can easily be found in excess of remedial guidelines. The presence of biogenic toluene in environmental samples can confound remedial investigations of petroleum impacts. However,the determination of the origin of toluene that is acceptable by regulatory bodies requires a scientifically creditable demonstration using a forensic analytical approach, and forensic data interpretation.
This presentation demonstrates the application of established arson analysis methodology and forensic data interpretation methods that can distinguish the origin of toluene as either biogenic or petrogenic. Arson analysis methods are conducted for crime scene investigators to provide legal proof for the presence of petroleum distillates,if present, in relation to arson investigations. This same method can be applied in the environmental field for the defensible determination of the origin of toluene.
Chemistry Matters Inc.and the AGAT Forensic Laboratory provide analysis for arson investigations for the Government of Alberta and have applied this methodology successfully for the demonstration of biogenic toluene at a number of wetland investigation sites. Example data from wetland environments and a range of petrogenic types are presented to explain the operation of the method. Environmental professionals involved in spill remediation or site monitoring should find this presentation applicable.
Where Does Toluene Come From? - Petrogenic Families and Biogenic Loners, Wate...Chemistry Matters Inc.
The seasonal accumulation of toluene by microbiological processes within specific wetland environments is a locally-recognized, but little understood, process. It has not been documented within the peer-reviewed literature. Currently, there is no legally defensible method of distinguishing the origin of toluene in environmental samples.
The presence of biogenic toluene can confound environmental investigations relating to petroleum releases within wetland environments, which comprise a large area of northern Alberta as well as other provinces.
This presentation discusses the results from the application of an established ASTM method, which is already accepted for arson analysis, for the investigation of the origin of toluene in wetland peat samples. The analytical method and environmental forensic data interpretation are capable of readily distinguishing biogenic and petrogenic origins of toluene in a legally-defensible manner. This is conducted by using plant biomarker chemistry to identify natural toluene sources, monocyclic aromatic hydrocarbon fingerprints and diagnostic ratios, which are possible due to substantially improved detection limits compared with conventional BTEX analysis.
Environmental professionals involved in spill remediation or site monitoring will find this presentation applicable.
Final day of the Dioxin 2016 conference in Florence, Italy, Dr. Court Sandau presented a summary of the analytical talks and posters presented at the Dioxin conference this year. Discussed the biggest highlights on PFAs, PBDEs, the history of Dioxin analysis and his impressions of where biomonitoring is going.
Closing plenary talk given at the International Network of Environmental Forensics (INEF) 2016 conference held in Orebro, Sweden. Presentation covered the history of PCBs and dioxins and their roles in the birth of environmental forensics. The talk discussed a new definition of the term “Environmental Forensics” and provided five main points regarding environmental forensics investigations.
Presentation provides overview of different case studies that used environmental forensics to investigate sources of petroleum releases. Case studies include biomarker analysis to aid in identifying phytogenic and petrogenic hydrocarbons, volatile organic compounds for emission source apportionment and polycyclic aromatic hydrocarbons (PAHs) in sediments.
This document is the curriculum vitae of Court D. Sandau, which provides information about his education, career experience, areas of expertise, and selected project experiences. It outlines that Dr. Sandau has a PhD in Chemistry and is the principal and senior chemist at Chemistry Matters, with over 20 years of experience in environmental forensics, expert witness work, and scientific investigations. It also provides details on 3 litigation support projects involving chemical fingerprinting to determine the source of environmental contamination.
Introduction to talk to be presented on Nov 17, 2015. The introduction shows the multiple compounds that are present in crude oil and refined products which can be used to determine sources of releases and identify products used in arson cases. Such compounds include polycyclic aromatic hydrocarbons, alkylated benzenes, and petroleum biomarkers.
Training seminar for Fire Investigators Association of Alberta on arson laboratory analysis and process. Presentation goes through the process of collection and analyzing arson samples for the presence of ignitable liquid residues.
Presentation was presenting in part on January 21, 2011 for Exova's Environmental Seminar held in Calgary, Alberta. The presentation covers some important points and considerations for those conducting environmental sampling where the data could be used for litigious or litigation matters. Legal sampling is much more intense for procedures and documentation than regular sampling and those doing the work, need to be knowledgeable about those differences. The presentations illustrates the differences using case studies the author has been involved in.
This document discusses characterizing the source zones of surface casing vent leaks using geochemistry. It provides examples of case studies where they used fluid and gas samples from surface casing vents and production casings to fingerprint the source zones through isotopic analysis. In complex cases, they combined fluid and gas characterization along with mudgas logs to identify the source zone within a 200-300m range. In simpler high gas flow cases, advanced isotopic models were needed to identify the source as a similar zone, since bulk gas compositions could implicate different zones. High quality samples, accurate isotope analysis, and accounting for microbial effects are needed to conclusively determine leak sources.
Emerging Earth Observation methods for monitoring sustainable food productionCIFOR-ICRAF
Presented by Daniela Requena Suarez, Helmholtz GeoResearch Center Potsdam (GFZ) at "Side event 60th sessions of the UNFCCC Subsidiary Bodies - Sustainable Bites: Innovating Low Emission Food Systems One Country at a Time" on 13 June 2024
The modification of an existing product or the formulation of a new product to fill a newly identified market niche or customer need are both examples of product development. This study generally developed and conducted the formulation of aramang baked products enriched with malunggay conducted by the researchers. Specifically, it answered the acceptability level in terms of taste, texture, flavor, odor, and color also the overall acceptability of enriched aramang baked products. The study used the frequency distribution for evaluators to determine the acceptability of enriched aramang baked products enriched with malunggay. As per sensory evaluation conducted by the researchers, it was proven that aramang baked products enriched with malunggay was acceptable in terms of Odor, Taste, Flavor, Color, and Texture. Based on the results of sensory evaluation of enriched aramang baked products proven that three (3) treatments were all highly acceptable in terms of variable Odor, Taste, Flavor, Color and Textures conducted by the researchers.
(Q)SAR Assessment Framework: Guidance for Assessing (Q)SAR Models and Predict...hannahthabet
The webinar provided an overview of the new OECD (Q)SAR Assessment Framework for evaluating the scientific validity of (Q)SAR models, predictions, and results from multiple predictions. The QAF provides assessment elements for existing principles for evaluating models, as well as new principles for evaluating predictions and results. In addition to the principles, assessment elements, and guidance for evaluating each element, the QAF includes a checklist for reporting assessments.
This new Framework provides regulators with a consistent and transparent approach for reviewing the use of (Q)SAR predictions in a regulatory context and increases the confidence to accept alternative methods for evaluating chemical hazards. The OECD worked closely together with the Istituto Superiore di Sanità (Italy) and the European Chemicals Agency (ECHA), supported by a variety of international experts to develop a checklist of criteria and guidance for evaluating each criterion. The aim of the QAF is to help establish confidence in the use of (Q)SARs in evaluating chemical safety, and was designed to be applicable irrespective of the modelling technique used to build the model, the predicted endpoint, and the intended regulatory purpose.
The webinar provided an overview of the project and presented the main aspects of the framework for assessing models and results based on individual or multiple predictions.
Monitor indicators of genetic diversity from space using Earth Observation dataSpatial Genetics
Genetic diversity within and among populations is essential for species persistence. While targets and indicators for genetic diversity are captured in the Kunming-Montreal Global Biodiversity Framework, assessing genetic diversity across many species at national and regional scales remains challenging. Parties to the Convention on Biological Diversity (CBD) need accessible tools for reliable and efficient monitoring at relevant scales. Here, we describe how Earth Observation satellites (EO) make essential contributions to enable, accelerate, and improve genetic diversity monitoring and preservation. Specifically, we introduce a workflow integrating EO into existing genetic diversity monitoring strategies and present a set of examples where EO data is or can be integrated to improve assessment, monitoring, and conservation. We describe how available EO data can be integrated in innovative ways to support calculation of the genetic diversity indicators of the GBF monitoring framework and to inform management and monitoring decisions, especially in areas with limited research infrastructure or access. We also describe novel, integrative approaches to improve the indicators that can be implemented with the coming generation of EO data, and new capabilities that will provide unprecedented detail to characterize the changes to Earth’s surface and their implications for biodiversity, on a global scale.
Exploring low emissions development opportunities in food systemsCIFOR-ICRAF
Presented by Christopher Martius (CIFOR-ICRAF) at "Side event 60th sessions of the UNFCCC Subsidiary Bodies - Sustainable Bites: Innovating Low Emission Food Systems One Country at a Time" on 13 June 2024