This document provides an overview of gas hydrates, including their significance as an energy source, historical discoveries, identification methods, and exploitation techniques. It specifically examines gas hydrate occurrences in the Indian Exclusive Economic Zone, using the Krishna-Godavari Basin as a case study. Seismic data from the basin shows distinct bottom-simulating reflectors indicative of gas hydrates. While gas hydrates represent a potentially large energy resource, challenges to their safe and economic production include modeling their physical behavior, transporting the gas, and maintaining well stability during hydrate dissociation.
It is a power point presentation on Gas Hydrates.
It consist of Energy Scenario, Basic Definition, methodology,
Methane Hydrate formation condition.
Future Scope
Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth's fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists.
It is a power point presentation on Gas Hydrates.
It consist of Energy Scenario, Basic Definition, methodology,
Methane Hydrate formation condition.
Future Scope
Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth's fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists.
A presentation illustrating the phenomena of NGH including a brief introduction about the NGH , the conditions required for their initiation , different structures , suitable environments , different detection methods , major challenges , extraction methods , importance and distribution of reserves worldwide.
Marine methane Hydrate Field Research plan 2013ramist
This Marine Methane Hydrate Field Research Plan
concludes with a series of recommendaƟ ons concerning
the most important methane hydrate research challenges
and how scienƟ fi c drilling can advance our understanding
of methane hydrates in nature.
Clathrates ; Hydrate ; Gas Hydrate; Hydrates Fundamentals; Typical Hydrate forming Gases; STRUCTURAL GEOMETRIES OF GAS HYDRATES; CONCERN ASSOCIATED WITH GAS HYDRATE; TYPES OF METHANE HYDRATE DEPOSITS; The stability of methane hydrate in nature; GAS HYDRATE PETROLEUM SYSTEM:; Gas hydrate stability conditions; WORLD GAS HYDRATE RESOURCE; Resource Pyramid for Gas Hydrates; Do We have the Technology to Extract Methane from Gas Hydrates?; DEPOSITIONAL ENVIRONMENT OF METHANE HYDRATE ; Where are Gas Hydrates Located?; PRODUCTION FROM HYDRATES; Gas Production Methods form Hydrates’ Thermal Stimulation; Depressurization; Inhibitor Injection; CO2 Sequestration; THE FUTURE OF METHANE HYDRATES
Gas hydrate
To prepare natural gas for sale, its undesirable components (water, H2S and CO2) must be removed. Most natural gas contains substantial amounts of water vapor due to the presence of connate water in the reservoir rock. At reservoir pressure and temperature, gas is saturated with water vapor
Conversion of sea water into liquid hydrogen fuel...
future technology, renewable energy technology, liquid hydrogen fuel, environment friendly, hydrocarbon fuel, jet engine fuel, future revolution in the world.....
Presentation given at the 2012 Alaska LNG Summit by Mark Myers, Vice Chancellor Research University of Alaska Fairbanks & former Director of U.S. Geological Survey.• US market transformation: Low gas prices and declining import needs of Lower 48.
• Valdez LNG economics and global gas demand forecasts
• Post-Fukushima: Asia in need of an energy alternative and the Alaskan LNG answer – how does Valdez LNG compare to Japan’s gas supply alternatives?
• Growing interest in LNG exports from the USA: market opportunities
• A spotlight on Alaska’s vast energy resources – tapping into a giant
A presentation illustrating the phenomena of NGH including a brief introduction about the NGH , the conditions required for their initiation , different structures , suitable environments , different detection methods , major challenges , extraction methods , importance and distribution of reserves worldwide.
Marine methane Hydrate Field Research plan 2013ramist
This Marine Methane Hydrate Field Research Plan
concludes with a series of recommendaƟ ons concerning
the most important methane hydrate research challenges
and how scienƟ fi c drilling can advance our understanding
of methane hydrates in nature.
Clathrates ; Hydrate ; Gas Hydrate; Hydrates Fundamentals; Typical Hydrate forming Gases; STRUCTURAL GEOMETRIES OF GAS HYDRATES; CONCERN ASSOCIATED WITH GAS HYDRATE; TYPES OF METHANE HYDRATE DEPOSITS; The stability of methane hydrate in nature; GAS HYDRATE PETROLEUM SYSTEM:; Gas hydrate stability conditions; WORLD GAS HYDRATE RESOURCE; Resource Pyramid for Gas Hydrates; Do We have the Technology to Extract Methane from Gas Hydrates?; DEPOSITIONAL ENVIRONMENT OF METHANE HYDRATE ; Where are Gas Hydrates Located?; PRODUCTION FROM HYDRATES; Gas Production Methods form Hydrates’ Thermal Stimulation; Depressurization; Inhibitor Injection; CO2 Sequestration; THE FUTURE OF METHANE HYDRATES
Gas hydrate
To prepare natural gas for sale, its undesirable components (water, H2S and CO2) must be removed. Most natural gas contains substantial amounts of water vapor due to the presence of connate water in the reservoir rock. At reservoir pressure and temperature, gas is saturated with water vapor
Conversion of sea water into liquid hydrogen fuel...
future technology, renewable energy technology, liquid hydrogen fuel, environment friendly, hydrocarbon fuel, jet engine fuel, future revolution in the world.....
Presentation given at the 2012 Alaska LNG Summit by Mark Myers, Vice Chancellor Research University of Alaska Fairbanks & former Director of U.S. Geological Survey.• US market transformation: Low gas prices and declining import needs of Lower 48.
• Valdez LNG economics and global gas demand forecasts
• Post-Fukushima: Asia in need of an energy alternative and the Alaskan LNG answer – how does Valdez LNG compare to Japan’s gas supply alternatives?
• Growing interest in LNG exports from the USA: market opportunities
• A spotlight on Alaska’s vast energy resources – tapping into a giant
Growing power: Exploring energy needs in smallholder agricultureIIED
The presentation of Sarah Best, IIED's senior researcher (energy and extractives) at IIED's seminar “Growing Power: Exploring Energy Needs in Smallholder Agriculture” on 30 April 2014.
Drawing on Best’s “Growing Power” discussion paper (http://pubs.iied.org/16562IIED.html), the presentation considers the ‘why’, ‘what’ and ‘how’ of addressing the huge gap in access to modern energy and equipment smallholder-based agri-food chains.
It examines the diversity of energy needs, the approaches of the energy and agri-food sectors, and highlights key priorities, lessons-learned and knowledge gaps.
More information: http://www.iied.org/energy
Objective Capital's Industrial Metals, Minerals & Mineable Energy Investment Summit 2011
Ironmongers' Hall, City of London
3 November 2011
Speaker: Deepak Lalwani OBE, LalCap
The current assignment discusses the formation of natural gas hydrates in gas transmission pipelines. Hydrates are crystalline compounds, consisting of a gas molecule and water, which form under certain thermodynamic conditions, which include high pressure and low temperature. Natural gas hydrates are responsible for pipeline plugging and corrosion. Thus, handling the issue of the formation is a matter of vital importance for the industry. At the theoretical background of the assignment the topic is presented and analyzed towards the hydrate structure and development, the formation, the consequences and, finally, the solutions as well as the inspection processes. In order to provide the optimal strategy in dealing with hydrate formation, it is of vital importance to have an understanding of the conditions that cause hydrate formation. The most accurate predictions can be conducted with the use of computer software. In the current assignment the chemical simulations software Aspen Hysys is used for studying the formation conditions. Three potential natural gas streams, with different compositions, were modeled and studied towards the conditions of hydrate formation.
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contact me : gr.linkedin.com/in/fotiszachopoulos
Effect of CO2 sequestration on soil liquefaction in geological pitsijiert bestjournal
This paper deals with review of the previous related research on evaluation of soil liquefaction due to Carbon sequestration by various Carbon Capture Sequestration processes in geological pits. It provides critical literature recommendations on evaluation of soil liqu efaction potential assessment. The detection of soil liquefaction by using seismic records has been developed by various researchers. With this information,the evaluation of soil liquefaction are well under stood and this lead to a more precise and confident output. Gaining support for CCS will require engaging the interest and building the support of a variety of stakeholders,each with differ ent perspectives and goals. Although,CCS builds upon a technology base developed over more than half a century by the oil and gas industry. In the past,the industrially released CO 2 had been introduced to ocean which was harming the aquatic animals. In view of this,the sequestration of CO 2 into ocean was internationally banned. Hence,now much of the Carbon sequestration process is done by various industries in geolog ical pits. This creates a major threat to the earth quake problems worldwide. With the enhanced frequenc y of earthquakes all around the world,it is presumed by many environment scientists that the CO 2 sequestration pits leads to soil liquefaction and hence it results in more frequent earth quakes. T herefore,this paper summarises,different methods to evaluate liquefaction potential of soil by usi ng studies from seismic waves generated in earth,it is also propose it is also explains different me thodology for an eco friendly technology to reduce CO 2 from environment.
Delineation of Hydrocarbon Bearing Reservoirs from Surface Seismic and Well L...IOSR Journals
Hydrocarbon reservoir has been delineated and their boundaries mapped using direct indicators from 3-D seismic and well log data from an oil field in Nembe creek, Niger Delta region. Well log signatures were employed to identify hydrocarbon bearing sands. Well to seismic correlation revealed that these reservoirs tied with direct hydrocarbon indicators on the seismic section. The results of the interpreted well logs revealed that the hydrocarbon interval in the area occurs between 6450ft to 6533ft for well A, 6449ft to 6537ft for well B and 6629ft to 6704ft for well C; which were delineated using the resistivity, water saturation and gamma ray logs. Cross plot analysis was carried out to validate the sensitivity of the rock attributes to reservoir saturation condition. Analysis of the extracted seismic attribute slices revealed HD5000 as hydrocarbon bearing reservoir.
This presentation is all about Petroleum Engineering, Prospecting oil and gas, drilling and various drilling methods, logs and its types, different Drive Mechanisms, etc......
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Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
How to Create Map Views in the Odoo 17 ERPCeline George
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The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
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The Indian economy is classified into different sectors to simplify the analysis and understanding of economic activities. For Class 10, it's essential to grasp the sectors of the Indian economy, understand their characteristics, and recognize their importance. This guide will provide detailed notes on the Sectors of the Indian Economy Class 10, using specific long-tail keywords to enhance comprehension.
For more information, visit-www.vavaclasses.com
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Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
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This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
Instructions for Submissions thorugh G- Classroom.pptx
Gas hydrates Anomalies and Identifications
1. Gas Hydrates: Anomalous behavior of gas
hydrates in Indian Exclusive Economic Zones
with Advances in Exploration and
Exploitation Techniques – A Review
16th March, 2013.
4. A REVIEW OF THE PAST
First observed in 1810 in the laboratory of Sir Humphrey Davy
as Chlorine hydrate.
In 1930s, Hammerscgmidt discovered hydrates as “pipeline
blockage”.
Later in 1970’s, Russian scientists made an allegation that gas
hydrates can be entrapped in water and can have large
reserves formed under natural environment.
Investigations were followed by the discovery of gas hydrates
in:
Siberian permafrost regions (Makogon et al. 1971)
Mackenzie Delta, Canada (Bily and Dick 1974)
6. Geophysical Proxies for Gas Hydrate
Pockmark
Wipeouts
Gas chimney
Seafloor collapse
Transparent zone
Amplitude reduction
Diapir
VAMPS
Mud volcano
Venting
Fluid flow along faults
(Wood et al., 2002)
7. LOGGING TOOLS
Logging tools most commonly used for refinement of
estimates :
Type of Log
Response to Hydrates
Mud Log
Increase of gas in Drilling mud
SP
Less negative compared to free gas
zone
Acoustic Transit Time Decreases relative to water or free
gas
Resistivity
Higher relative to free gas
Density
Very small decrease
Neutron Porosity
Nearly same as liquid water
Caliper
Oversized drill hole
8. QUANTIFICATION USING CORES
Two common ways of identifying
hydrates in cores:
IR imaging
Pressurized core sampling systems
A third method of sensing hydrates
is by use of chlorinity
A fourth rapidly evolving method:
CT scanning
Applies x-ray imaging techniques
11. KRISHNA GODAVARI BASIN
Area of about 28,000 sq. km onshore and 145,000
sq. km extending in the offshore.
National Geophysical Research Institute (NGRI)
acquired 2-D multi channel seismic (MCS) data
between 500 to 1500 m water depths.
12. Locations of seismic profiles (black lines) showing MCS data acquired
in KG basin. The identified BSRs have been marked white. Red and
green lines locate seismic sections that exhibit representative BSRs in
next Figure (Journal Geological Society of India, 2012).
13. Distinct BSR on specimen seismic sections along the (a) red and (b)
green lines, shown in above figure in KG basin. The CDP interval is 12.5
m (Journal Geological Society of India, 2012).
14. KRISHNA GODAVARI BASIN
The predicted GHSZ thickness below the seafloor is
around 300m.
The BSR being the primary proxy, other proxies that
have been identified in K-G basin:
Polarity reversal
Pockmarks
Gas chimneys
Crosscuts different lithological boundaries
Amplitude blanking
Pore water chemistry (To infer sulfate and chloride anomalies)
15. KRISHNA GODAVARI BASIN
The gas hydrate occurrence in KG offshore is
associated with fractured clay.
Microbiological studies (mainly enumeration of
sulfate and nitrate reducing bacteria and nitrifiers)
indicate the sediments are conducive for growth of
different bacteria.
The good concentration of TOC in the cores adds
value to the suitability for Gas hydrate exploration.
17. CHALLENGES/PROBLEMS
• Some of the common challenges/problems as
recorded in history are:
oAppropriate modeling of gas hydrates
response.
oPipeline construction for their transportation.
oHigh water and sand production.
oInstability of the surface hole during hydrate
dissociation.
oSlugging and Liquid loading.
oLack of proven conventional technology world
over.
18. CONCLUSION
Large potential source of energy requires proper
identification.
Understanding of the fluid behavior including phase
change, liquid accumulation, flow
regime, velocity, temperature, and pressure profile to
make that the proactive decisions regarding operation
and management of the system.
Indian offshore has vast reserves of gas hydrates and
the need is of potential recovery with the implication
of the recovery methods.
Suitability of the recovery methods depends on proper
understanding of the mechanism of their formation
and proper treatments.
19. REFERENCES
Sloan, Koh (2008). Clathrate Hydrates of Natural
Gases, third edition. CRC Press.
Carroll, J. (2009). Natural Gas Hydrates A Guide for
Engineers, second edition. Elsevier.
Sanjeev Rajput*, M. K. (2009). Seismic indicators of
gas hydrates and associated free gas, SEG
International Exposition and Annual Meeting.
Houston .
Muhammad Iqrar Qadir, M. A. (Nov. 2011). Gas
Hydrates: A Fuel for Future but Wrapped in Drilling
Challenges, SPE 156516.
Kalachand sain, M. o. (June 2012). Gas-hydrates in
Krishna-Godavari and Mahanadi Basins. New
Data, journal geological society of india.