Environmental Conservation & Reclamation
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Photos from class work in the conservation & reclamation major of Lakeland College's 2-year environmental sciences diploma.
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Field and lab assignment pp
This document contains a field and lab assignment for Courtney Perry that lists different types of rocks collected - basalt, amphibolite, quartzite, and gabbro. It also lists topics covered in part two such as fault, the weathering process, mass wasting and erosion, sedimentary environments including continental, marine, and transitional. The final section discusses uses of practical geology.
Sedimentary questions
1) Neomorphism refers to the combined processes of inversion and recrystallization in carbonate rocks. Inversion is when one mineral changes to a polymorph like aragonite to calcite. Recrystallization changes the size or shape of crystals with little chemical change.
2) Two major carbonate cement types are calcite and aragonite. Calcite cement forms in phreatic and meteoric zones by dissolution of unstable aragonite. Aragonite forms fibrous cements in hypersaline or shallow marine conditions. Calcite spar crystals fill pores and fractures.
3) Sedimentary structures like convolute bedding and massive bedding in sediments can indicate past earthquakes. Convolute
Sulphur biogeochemistry of agro ecosystems
Sulphur (S) is a ubiquitous on earth and statistically S is available in adequate amounts to satisfy globally plant growth. Nevertheless S deficiency is an important nutrient disorder in agricultural production on all continents (Haneklaus et al., 2003). The S biogeochemical cycle of agro-ecosystems involves the processes like mineralization, immobilization, oxidation, reduction, adsorption, desorption and atmospheric S emissions. Das et al. (2012) reported that the organic C and clay play an important role in regulating sulphur availability in some rapeseed-growing soils of Assam. Examination of soils after incubation revealed that the mineralized S was mainly derived from the C-bonded S and non-reducible organic S pool, while the majority of mineralized S under soil S exhaustion by rice was derived from the C–O–S pool (Zhou et al., 2005). The agronomic efficiency and apparent S recovery by wheat-soybean system decreased with an increase in S application, while the percent response increased with increasing in levels of S. Due to S application, the content of available S was found to increase and the increase was more in surface soils than lower layers (Singh et al., 2014). In a pot culture study, the pesticides like endosulfan, dithane M-45 served a detrimental effect on transformation of S, whereas 2, 4-D created a favourable beneficial effect on S transformation in soil environment (Giri et al., 2011). Long-term human intervention markedly changed the molecular- level composition of soil organic S and led to a shift in the apparent oxidation state of organic S from undisturbed grassland soils primarily composed of S moieties in highly reduced and intermediate oxidation states toward managed agro-ecosystems dominated by organic S rich in strongly oxidized or high-valence S species (Solomon et al., 2011). The XANES (X-ray Absorption Near-Edge Structure Spectroscopy) indicated that the long-term FYM application shifted S species composition from highly oxidized towards intermediate oxidization (Boye et al., 2011). Long term studies related to land use changes may help to understand the soil S cycle in cropping and agro-forestry systems and enrich the knowledge about S management (Jiang et al., 2007). Future research should include evaluation of all components of S cycle collaborating with others to asses environmental impact and sustainability of feedstock production.
Surface creep, saltation and suspension with large and medium aggregates: a w...
Mr Eduardo A. Rienzi, Cátedra de Manejo y Conservación de Suelos FAUBA, Argentina. Global Symposium on Soil Erosion (GSER19), 15 - 17 May 2019 at FAO HQ.
Land Use Changes on Soil Carbon Dynamics, Stocks in Eastern Himalayas, India
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Parmar Brajendra, from Indian Institute of Rice Research - India, in FAO Hq, Rome
Soil ppt
what things are visible which instruments are used, what are the major functions of the instrument used and which is the best technique used by the scientific officer to compare whether two soil samples are from same area or different area.
Introduction of foraminifera in oil exploration
This document discusses the application of foraminifera in oil exploration. It begins with an introduction to foraminifera and their importance in oil exploration due to their sensitivity to environmental changes. It then covers the conditions required for oil formation, concepts in using foraminifera for oil exploration like biostratigraphy and paleoenvironment interpretation, and micropaleontological techniques. Foraminifera are useful for biostratigraphic correlation, interpreting depositional environments, and reconstructing the geologic history of sedimentary basins to aid in oil exploration.
Chemical & Microbial analysis of farm & forest soil
The document analyzes and compares the chemical and microbial composition of farm soil and forest soil.
The farm soil had lower organic content than the forest soil but was better suited for plant growth. The forest soil had higher organic content which supported more microorganisms but the acidity levels needed to be adjusted to protect nitrogen-fixing bacteria. Overall, both soils benefited from organic amendments but the farm soil required additional organic matter to support beneficial microbes and earthworms.
Recommended
Field and lab assignment pp
This document contains a field and lab assignment for Courtney Perry that lists different types of rocks collected - basalt, amphibolite, quartzite, and gabbro. It also lists topics covered in part two such as fault, the weathering process, mass wasting and erosion, sedimentary environments including continental, marine, and transitional. The final section discusses uses of practical geology.
Sedimentary questions
1) Neomorphism refers to the combined processes of inversion and recrystallization in carbonate rocks. Inversion is when one mineral changes to a polymorph like aragonite to calcite. Recrystallization changes the size or shape of crystals with little chemical change.
2) Two major carbonate cement types are calcite and aragonite. Calcite cement forms in phreatic and meteoric zones by dissolution of unstable aragonite. Aragonite forms fibrous cements in hypersaline or shallow marine conditions. Calcite spar crystals fill pores and fractures.
3) Sedimentary structures like convolute bedding and massive bedding in sediments can indicate past earthquakes. Convolute
Sulphur biogeochemistry of agro ecosystems
Sulphur (S) is a ubiquitous on earth and statistically S is available in adequate amounts to satisfy globally plant growth. Nevertheless S deficiency is an important nutrient disorder in agricultural production on all continents (Haneklaus et al., 2003). The S biogeochemical cycle of agro-ecosystems involves the processes like mineralization, immobilization, oxidation, reduction, adsorption, desorption and atmospheric S emissions. Das et al. (2012) reported that the organic C and clay play an important role in regulating sulphur availability in some rapeseed-growing soils of Assam. Examination of soils after incubation revealed that the mineralized S was mainly derived from the C-bonded S and non-reducible organic S pool, while the majority of mineralized S under soil S exhaustion by rice was derived from the C–O–S pool (Zhou et al., 2005). The agronomic efficiency and apparent S recovery by wheat-soybean system decreased with an increase in S application, while the percent response increased with increasing in levels of S. Due to S application, the content of available S was found to increase and the increase was more in surface soils than lower layers (Singh et al., 2014). In a pot culture study, the pesticides like endosulfan, dithane M-45 served a detrimental effect on transformation of S, whereas 2, 4-D created a favourable beneficial effect on S transformation in soil environment (Giri et al., 2011). Long-term human intervention markedly changed the molecular- level composition of soil organic S and led to a shift in the apparent oxidation state of organic S from undisturbed grassland soils primarily composed of S moieties in highly reduced and intermediate oxidation states toward managed agro-ecosystems dominated by organic S rich in strongly oxidized or high-valence S species (Solomon et al., 2011). The XANES (X-ray Absorption Near-Edge Structure Spectroscopy) indicated that the long-term FYM application shifted S species composition from highly oxidized towards intermediate oxidization (Boye et al., 2011). Long term studies related to land use changes may help to understand the soil S cycle in cropping and agro-forestry systems and enrich the knowledge about S management (Jiang et al., 2007). Future research should include evaluation of all components of S cycle collaborating with others to asses environmental impact and sustainability of feedstock production.
Surface creep, saltation and suspension with large and medium aggregates: a w...
Mr Eduardo A. Rienzi, Cátedra de Manejo y Conservación de Suelos FAUBA, Argentina. Global Symposium on Soil Erosion (GSER19), 15 - 17 May 2019 at FAO HQ.
Land Use Changes on Soil Carbon Dynamics, Stocks in Eastern Himalayas, India
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Parmar Brajendra, from Indian Institute of Rice Research - India, in FAO Hq, Rome
Soil ppt
what things are visible which instruments are used, what are the major functions of the instrument used and which is the best technique used by the scientific officer to compare whether two soil samples are from same area or different area.
Introduction of foraminifera in oil exploration
This document discusses the application of foraminifera in oil exploration. It begins with an introduction to foraminifera and their importance in oil exploration due to their sensitivity to environmental changes. It then covers the conditions required for oil formation, concepts in using foraminifera for oil exploration like biostratigraphy and paleoenvironment interpretation, and micropaleontological techniques. Foraminifera are useful for biostratigraphic correlation, interpreting depositional environments, and reconstructing the geologic history of sedimentary basins to aid in oil exploration.
Chemical & Microbial analysis of farm & forest soil
The document analyzes and compares the chemical and microbial composition of farm soil and forest soil.
The farm soil had lower organic content than the forest soil but was better suited for plant growth. The forest soil had higher organic content which supported more microorganisms but the acidity levels needed to be adjusted to protect nitrogen-fixing bacteria. Overall, both soils benefited from organic amendments but the farm soil required additional organic matter to support beneficial microbes and earthworms.
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Environmental threats and reclamation after underground mining 1
Underground gem mining in Sri Lanka provides economic and social benefits but also poses significant environmental threats if not properly managed. Traditional pit mining damages water and soil quality, destroys habitats, and endangers humans. Effective mine reclamation, including stabilizing land, restoring vegetation and water flows, and closing pits, is needed to mitigate long-term environmental impacts and allow the pre-mining land use to resume after mining ceases. While gem mining provides livelihoods, greater regulation and enforcement is required to minimize damage to the environment.
The waste land reclamation
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wasteland reclamation
Wasteland reclamation involves reclaiming degraded or unused land to make it suitable for agriculture, habitation, or cultivation. India has significant areas of wasteland that can be reclaimed. Wastelands can be classified based on difficulty of reclamation - easily reclaimable for agriculture; reclaimable with some difficulty for agroforestry; and reclaimable with extreme difficulty only for forestry. Methods of reclamation include afforestation, reforestation, contour ploughing, and changing crop practices. A case study highlights Jatropha plantation on wastelands in Rajasthan as a promising crop that provides income while reclaiming land.
Agroforestry
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Land degradation leads to various environmental and economic problems. Wastelands can be reclaimed through different methods depending on their condition. Easily reclaimable wastelands can be used for agriculture by improving soil quality. Marginal wastelands can use agroforestry which plants trees and crops together. Extremely degraded wastelands may only support forestation or natural ecosystem restoration. Jatropha plantations show potential for wasteland reclamation but farmers face challenges like lack of technical knowledge, long growth periods, and climate issues. The oil and press cake of jatropha have many useful applications.
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wasteland reclamation
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