This document discusses carbon sequestration in soils through various agricultural management practices. It outlines concepts of carbon sequestration and greenhouse gases. It then discusses specific practices like conservation tillage, cover cropping, animal manure application, improved grassland management, and agroforestry that can sequester carbon in soils at rates of 0.1 to 1+ Mg C/ha/yr. The document emphasizes that a diversity of practices which increase carbon inputs and minimize losses can help mitigate rising greenhouse gases and restore degraded lands.
Soil Organic Carbon Sequestration: Importance and State of ScienceExternalEvents
This presentation was presented during the Plenary 1, GSOC17 – Setting the scientific scene for GSOC17 of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Rattan Lal from Carbon Management and Sequestration Center – USA , in FAO Hq, Rome
Part of a climate-smart agriculture metrics webinar series co-hosted by the World Business Council on Sustainable Development, the CGIAR Research Program on Climate Change, Agriculture and Food Security (CCAFS) and the University of Vermont.
This session, Mitigation potential of soil carbon sequestration, took place on July 17, 2018.
Speakers:
Meryl Richards, Science Officer, Low Emissions Development | CCAFS and UVM
Keith Shepherd, Principal Soil Scientist | World Agroforestry Centre (ICRAF)
Ciniro Costa Jr., Climate and Agriculture Analyst | IMAFLORA
Axelle Bodoy , Global Milk and Farming Sustainability Manager| Danone
Benefits of Soil Organic Carbon - an overviewExternalEvents
The presentation was given by Mr. Niels H. Batjes, ISRIC, during the GSOC Mapping Global Training hosted by ISRIC - World Soil Information, 6 - 23 June 2017, Wageningen (The Netherlands).
This presentation was presented during the Plenary 1, Opening Ceremony of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Luca Montanarella from EU Commission’s Joint Research Centre, in FAO Hq, Rome
Soil is the largest carbon reservoir pool of terrestrial ecosystem and plays a key role in the global carbon budget and greenhouse effect. It contains 3.5% of the earth’s carbon reserve as compared with 1.7% in the atmosphere , 8.9% in the fossil fuels, 1.0% in the biota and 84.95% in the oceans. Soil reserves about 1550 GT of carbon as Soil Organic Carbon (SOC) and 1700 GT as carbonate carbon (Soil Inorganic Carbon , i,e SIC).Soil carbon(C) plays an important role in exchange of CO2 between atmosphere and biosphere. SOC and SIC are important as it determine ecosystem and agro-ecosystem functions influencing soil structure ,soil fertility ,water holding capacity , cation exchange capacity and other soil characteristics.
Soil Organic Carbon Sequestration: Importance and State of ScienceExternalEvents
This presentation was presented during the Plenary 1, GSOC17 – Setting the scientific scene for GSOC17 of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Rattan Lal from Carbon Management and Sequestration Center – USA , in FAO Hq, Rome
Part of a climate-smart agriculture metrics webinar series co-hosted by the World Business Council on Sustainable Development, the CGIAR Research Program on Climate Change, Agriculture and Food Security (CCAFS) and the University of Vermont.
This session, Mitigation potential of soil carbon sequestration, took place on July 17, 2018.
Speakers:
Meryl Richards, Science Officer, Low Emissions Development | CCAFS and UVM
Keith Shepherd, Principal Soil Scientist | World Agroforestry Centre (ICRAF)
Ciniro Costa Jr., Climate and Agriculture Analyst | IMAFLORA
Axelle Bodoy , Global Milk and Farming Sustainability Manager| Danone
Benefits of Soil Organic Carbon - an overviewExternalEvents
The presentation was given by Mr. Niels H. Batjes, ISRIC, during the GSOC Mapping Global Training hosted by ISRIC - World Soil Information, 6 - 23 June 2017, Wageningen (The Netherlands).
This presentation was presented during the Plenary 1, Opening Ceremony of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Luca Montanarella from EU Commission’s Joint Research Centre, in FAO Hq, Rome
Soil is the largest carbon reservoir pool of terrestrial ecosystem and plays a key role in the global carbon budget and greenhouse effect. It contains 3.5% of the earth’s carbon reserve as compared with 1.7% in the atmosphere , 8.9% in the fossil fuels, 1.0% in the biota and 84.95% in the oceans. Soil reserves about 1550 GT of carbon as Soil Organic Carbon (SOC) and 1700 GT as carbonate carbon (Soil Inorganic Carbon , i,e SIC).Soil carbon(C) plays an important role in exchange of CO2 between atmosphere and biosphere. SOC and SIC are important as it determine ecosystem and agro-ecosystem functions influencing soil structure ,soil fertility ,water holding capacity , cation exchange capacity and other soil characteristics.
about...Carbon sequestration, Co2 capture technology, types of carbon sequestration, Co2 separation, carbon sources and carbon sinks, benefits of soil sequestration of carbon, conclution.
soil organic carbon- a key for sustainable soil quality under scenario of cli...Bornali Borah
The global soil resource is already showing a sign of serious degradation (Banwart et al. 2014) which has ultimately negative impact on sustained crop yield and environmental quality. Due to intense rainfall and concurrent rise in temperature with changing climate, the fertile top soil is prone to severe degradation with depletion of SOC. Most soils in agricultural ecosystems have lost soil C ranging from 30 to 60 t C ha-1 with the magnitude of 50 to 75% loss (Lal, 2004). Hence, restoration of soil quality through different carbon management options will enhance soil health, mitigate climate change and provide sustained agricultural production.
carbon Sequestration and its method in plants ESHAASIF
CO2 is one of the main greenhouse gases that is causing global warming and forcing climate change.
The continued increased in CO2 concentration in the atmosphere is believed to be accelerated by human activities such as burning of fossil fuels and deforestation.
One of the approaches to reducing CO2 Concentration in the atmosphereCARBON SEQUESTRATION
Carbon Sequestration is the placement of CO2 into a depository in such way that it remains safely and not released back to the atmosphere.
Sequestration means something that is locked away for safe keeping. the trapping of a chemical in the atmosphere or environment and its isolation in a natural or artificial storage area.
is carbon sequestration
Soil management strategies to enhance carbon sequestration potential of degra...koushalya T.N
Reclamation of degraded lands has huge potential for carbon (C) sequestration to counteract the climate change. It was estimated that about 1,964 Mha of land is degraded worldwide and in India 146.8 Mha of land is degraded ( Bai et al., 2008). The major land-degradation processes in the World and in Asia are water erosion, wind erosion, salinity, alkalinity, nutrient depletion and metal pollution. Enrichment of soil organic carbon (SOC) stocks through sequestration of atmospheric CO2 in agricultural soils and degraded lands is important because of its impacts on improving soil quality and agronomic production, and also for adaptation to mitigation of climate change. Various management strategies like conservation agriculture, integrated nutrient management, afforestation, alternate land use, plantations and amendments and use of biochar hold promise for long-term C sequestration. It can be concluded that land degradation is a serious problem in India which need to be tackled because shrinking of land resource base will lead to a substantial decline in food grain production which in turn would hamper the economic growth rate and there would also be unprecedented increase in mortality rate owing to hunger and malnutrition.
Nutrient budgets are becoming accepted tools to describe nutrient flows within cropping system and to assist in the planning of the rotational cropping and mixed farming system
Depending on the farm management and the balance of inputs and outputs of nutrient N,P and K budgets have been shown to range from deficit to surplus in cropping system
Budgets are the outcome of simple nutrient accounting process which details all the inputs and outputs to a given defined system over fixed period of time
A soil surface nutrient budget accounts for all nutrients that enter the soil surface and leave the soil through crop uptake.
Impact of soil properties on carbon sequestrationyoginimahadule
Carbon sequestration is an important global phenomenon that plays a significant role in maintaining a balanced global carbon cycle and sustainable crop production. Carbon Sequestration is the placement of CO2 into a depository in such way that it remains safely and not released back to the atmosphere.
Among the soil factors, texture plays an important role in C sequestration. The observation that the decrease in clay- and silt associated C and N upon cultivation of soils was generally less than the decrease in C and N in the particle size fraction > 20 µm confirms that clay and sift particles protect C against microbial degradation (Hassink, 1997).
Increase in SOC concentration with conservation tillage was partly responsible for the increased macroaggregation near the soil surface.( Zhang et al. 2013)
Electrical conductivity in soils affects the organic carbon content by reducing the uptake of minerals and water by the plant which ultimately results in less plant growth. A higher electrical conductivity causes less decomposition in soils which consequently reduces the accumulation of humus meanwhile, the values of acidity; percentage of organic matter, organic carbon and the sequestration of carbon in soils containing T. kotschyiwas more than the values observed in soils containing T. aphylla and the soil of the control which contained no plants.
Nitrogen applicaton at optimum rate help to sequester carbon in soil.(Jiang et al. 2019). Integrated nutrient application in long-term rice-wheat cropping system would be a suitable option with respect to its potentiality of increasing yield, nutrient availability, and sequestering soil organic carbon for sustainable soil health management in partially reclaimed sodic soils of the north Indian subcontinent. He concluded that FYM application increase passive pool of soil while green manure increase active and labile pool. (Choudhury et al. 2018)
Six et al. (2006) by various observation of different sites concludes changes in the relative abundance and activity of bacteria and fungi may significantly affect C cycling and storage, due to the unique physiologies and differential interactions with soil physical properties of these two microbial groups. It has been hypothesized that C turnover is slower in fungal-dominated communities in part because fungi in corporate more soil C into biomass than bacteria and because fungal cell walls are more recalcitrant than bacterial cell walls. Same result by Aliasgharzad et al. 2016).
Tsai et al. (2013) showed positive correlation of soil organic carbon with elevation
Carbon sequestration in agricultural soils: The “4 per mil” programExternalEvents
Carbon sequestration in agricultural soils: The “4 per mil” program presented by Hervé Saint Macary, Centre de coopération internationale en recherche agronomique pour le développement (CIRAD), Montpellier, France
about...Carbon sequestration, Co2 capture technology, types of carbon sequestration, Co2 separation, carbon sources and carbon sinks, benefits of soil sequestration of carbon, conclution.
soil organic carbon- a key for sustainable soil quality under scenario of cli...Bornali Borah
The global soil resource is already showing a sign of serious degradation (Banwart et al. 2014) which has ultimately negative impact on sustained crop yield and environmental quality. Due to intense rainfall and concurrent rise in temperature with changing climate, the fertile top soil is prone to severe degradation with depletion of SOC. Most soils in agricultural ecosystems have lost soil C ranging from 30 to 60 t C ha-1 with the magnitude of 50 to 75% loss (Lal, 2004). Hence, restoration of soil quality through different carbon management options will enhance soil health, mitigate climate change and provide sustained agricultural production.
carbon Sequestration and its method in plants ESHAASIF
CO2 is one of the main greenhouse gases that is causing global warming and forcing climate change.
The continued increased in CO2 concentration in the atmosphere is believed to be accelerated by human activities such as burning of fossil fuels and deforestation.
One of the approaches to reducing CO2 Concentration in the atmosphereCARBON SEQUESTRATION
Carbon Sequestration is the placement of CO2 into a depository in such way that it remains safely and not released back to the atmosphere.
Sequestration means something that is locked away for safe keeping. the trapping of a chemical in the atmosphere or environment and its isolation in a natural or artificial storage area.
is carbon sequestration
Soil management strategies to enhance carbon sequestration potential of degra...koushalya T.N
Reclamation of degraded lands has huge potential for carbon (C) sequestration to counteract the climate change. It was estimated that about 1,964 Mha of land is degraded worldwide and in India 146.8 Mha of land is degraded ( Bai et al., 2008). The major land-degradation processes in the World and in Asia are water erosion, wind erosion, salinity, alkalinity, nutrient depletion and metal pollution. Enrichment of soil organic carbon (SOC) stocks through sequestration of atmospheric CO2 in agricultural soils and degraded lands is important because of its impacts on improving soil quality and agronomic production, and also for adaptation to mitigation of climate change. Various management strategies like conservation agriculture, integrated nutrient management, afforestation, alternate land use, plantations and amendments and use of biochar hold promise for long-term C sequestration. It can be concluded that land degradation is a serious problem in India which need to be tackled because shrinking of land resource base will lead to a substantial decline in food grain production which in turn would hamper the economic growth rate and there would also be unprecedented increase in mortality rate owing to hunger and malnutrition.
Nutrient budgets are becoming accepted tools to describe nutrient flows within cropping system and to assist in the planning of the rotational cropping and mixed farming system
Depending on the farm management and the balance of inputs and outputs of nutrient N,P and K budgets have been shown to range from deficit to surplus in cropping system
Budgets are the outcome of simple nutrient accounting process which details all the inputs and outputs to a given defined system over fixed period of time
A soil surface nutrient budget accounts for all nutrients that enter the soil surface and leave the soil through crop uptake.
Impact of soil properties on carbon sequestrationyoginimahadule
Carbon sequestration is an important global phenomenon that plays a significant role in maintaining a balanced global carbon cycle and sustainable crop production. Carbon Sequestration is the placement of CO2 into a depository in such way that it remains safely and not released back to the atmosphere.
Among the soil factors, texture plays an important role in C sequestration. The observation that the decrease in clay- and silt associated C and N upon cultivation of soils was generally less than the decrease in C and N in the particle size fraction > 20 µm confirms that clay and sift particles protect C against microbial degradation (Hassink, 1997).
Increase in SOC concentration with conservation tillage was partly responsible for the increased macroaggregation near the soil surface.( Zhang et al. 2013)
Electrical conductivity in soils affects the organic carbon content by reducing the uptake of minerals and water by the plant which ultimately results in less plant growth. A higher electrical conductivity causes less decomposition in soils which consequently reduces the accumulation of humus meanwhile, the values of acidity; percentage of organic matter, organic carbon and the sequestration of carbon in soils containing T. kotschyiwas more than the values observed in soils containing T. aphylla and the soil of the control which contained no plants.
Nitrogen applicaton at optimum rate help to sequester carbon in soil.(Jiang et al. 2019). Integrated nutrient application in long-term rice-wheat cropping system would be a suitable option with respect to its potentiality of increasing yield, nutrient availability, and sequestering soil organic carbon for sustainable soil health management in partially reclaimed sodic soils of the north Indian subcontinent. He concluded that FYM application increase passive pool of soil while green manure increase active and labile pool. (Choudhury et al. 2018)
Six et al. (2006) by various observation of different sites concludes changes in the relative abundance and activity of bacteria and fungi may significantly affect C cycling and storage, due to the unique physiologies and differential interactions with soil physical properties of these two microbial groups. It has been hypothesized that C turnover is slower in fungal-dominated communities in part because fungi in corporate more soil C into biomass than bacteria and because fungal cell walls are more recalcitrant than bacterial cell walls. Same result by Aliasgharzad et al. 2016).
Tsai et al. (2013) showed positive correlation of soil organic carbon with elevation
Carbon sequestration in agricultural soils: The “4 per mil” programExternalEvents
Carbon sequestration in agricultural soils: The “4 per mil” program presented by Hervé Saint Macary, Centre de coopération internationale en recherche agronomique pour le développement (CIRAD), Montpellier, France
Barry Jones, General Manager - Asia Pacific for the Global CCS Institute, provides an overview of carbon capture and storage technology including its rationale and a summary of current projects. The presentation also examines impediments to its deployment and recommendations for how to overcome them.
Prime Carbon: Soil Enhancement & Carbon Sequestration ProgramCarbon Coalition
Deborah Burden is CEO Prime CArbon. She explains how Australia's first regional carbon trading scheme works. This presentation was given at the Carbon Farming Expo & Conference Orange 18-19 November, 2008. Orange is in new South Wales, Australia.
Carbon Farming, A Solution to Climate Change.pptxNaveen Prasath
Global warming and climate change refer to an increase in average global temperatures over a very long period of time. Natural events and human activities are believed to be contributing to an increase in average global temperatures, This is caused primarily by increases in “greenhouse” gases such as Carbon Dioxide (CO2).
Indicators
Global Green House Gas emission
Atmospheric concentration of green house gases
Change in Temperature pattern
Change in precipitation pattern
Heat related deaths
Melting of Ice
Rise in sea level
Affecting crop production
Green house gases released by power plant, automobiles, deforestation etc
According to IPCC WG AR-5 the Earth’s average temperature has increased by one degree Fahrenheit to its highest level in the past four decade – believed to be the fastest rise in a thousand years.
Research found that if emissions of heat-trapping carbon emissions aren’t reduced, average surface temperatures could increase by 3 to 10 degrees Fahrenheit by the end of the century.
Professor Peter Grace says carbon rich soil is "your superannuation", it's not about carbon credits, it's about productivity. He sketches the potential for rangelands to sequester carbon.
NOTE: The presentation and data therein is for information only and can only be reproduced with permission of the author.
Global food production now faces greater challenges than ever before due to changing climate, increasing land degradation and decreasing nutrient use efficiency. Nutrient mining is a major cause of low crop yields in parts of the developing world. Especially nitrogen and phosphorus move beyond the bounds of the agricultural field due to inappropriate management practices as well as failure to achieve good congruence between nutrient supply and crop nutrient demand (Pandian et al. 2014). Climate changes raised a serious issue of soil health maintenance for future generations. Rise in temperature and unprecedented changes in precipitation pattern lead to soil degradation by the erosion of top fertile soil, loss of carbon, nitrogen and increasing area under saline, sodic and acid soils. The climate is one of the key elements impacting several cycles connected to soil and plant systems, as well as plant production, soil quality and environmental quality. Due to heightened human activity, the rate of CO2 is rising in the atmosphere. Changing climatic conditions (such as temperature, CO2 and precipitation) influence plant nutrition in a range of ways, comprising mineralization, decomposition, leaching and losing nutrients in the soil. In order to meet the food demand of the growing population, global food production must be increased substantially over the next several decades. Sustainable intensification of agriculture, based on proven technologies, can increase food production on existing land resources. Therefore, conservation and organic agriculture, precision farming, recycling of crop residues, crop diversification in soils and ecosystems, integrated nutrient management and balanced use of agricultural inputs are the proven technologies of sustainable intensification in agriculture. More importantly, among the climate smart agricultural practices, the selection of appropriate measures must be soil or site specific for sustaining resource base for future generations. Further, presentation must be initiated to fine-tune the existing climate-smart agriculture to suit different nutrient management practices.
Soil Carbon & its Sequestration for Better Soil HealthBiswajitPramanick4
Carbon sequestration is the long- term storage of carbon in oceans, soils, vegetation (especially forests), and geologic formations. Although oceans store most of the Earth's carbon, soils contain approximately 75% of the carbon pool on land — three times more than the amount stored in living plants and animals.
Biochar is a product rich in carbon that comes from the pyrolysis of biomass, generally of vegetable origin. It is obtained by the decomposition of organic matter exposed to temperatures between 350-600°C in an atmosphere with low oxygen availability (pyrolysis), which can be slow, intermediate or fast. The objective of this review is to show how biochar (BC) can be obtained and its effects on the physicochemical properties of soils and physiological behavior of cultivated plants. However, most studies reported positive effects of biochar application on soil physical and chemical properties, soil microbial activities, plant biomass and yield, and potential reductions of soil GHG emissions. This review summarized the general findings of the impacts of biochar application on different aspects from soil physical, chemical, and microbial properties, to soil nutrient availabilities, plant growth, biomass production and yield, greenhouse gases (GHG) emissions, and soil carbon sequestration. The biochar applications in soil remediation in the past years were summarized and possible mechanisms were discussed. Finally, the potential risks of biochar application and the future research directions were analyzed to verify the mechanisms involved in biochar-soil-microbial-plant interactions for soil carbon sequestration and crop biomass and yield improvements.
Climate change impacts on soil health and their mitigation and adaptation str...Rajendra meena
The increasing concentration of greenhouse gases (GHGs) is bringing about major changes to the global environment resulting in global warming, depletion of ozone concentration in the stratosphere, changes in atmospheric moisture and precipitation and enhanced atmospheric deposition. These changes impact several soil processes, which are influence soil health. Soil health refers to the capacity of soil to perform agronomic and environmental functions. A number of physical, chemical and biological characteristics have been proposed as indicators of soil health. Generally, biological processes in soil such as decomposition and storage of organic matter, C and N cycling, microbial and metabolic quotients are likely to be influenced greatly by climate change and have thus high relevance to assess climate change impacts (Allen et al., 2011). Soil organic matter (SOM) exerts a major influence on several soil health indicators and is thus considered a key indicator of soil health. An optimal level of SOM is essential for maintaining soil health and alleviating rising atmospheric CO2 concentration. Elevated CO2 has increased C decay rates generally but in some cases elevated CO2 increases soil C storage (Jastrow et al., 2016). Enhancing the soil organic carbon pool also improves agro-ecosystem resilience, eco-efficiency, and adaptation to climate change. Healthy soils provide the largest store of terrestrial carbon, when managed sustainably; soils can play an important role in climate change mitigation by storing carbon (carbon sequestration) and decreasing greenhouse gas emissions in the atmosphere (Paustian et al., 2016).
Wright et al., (2005) reported that no tillage increase soil organic carbon (SOC) and nitrogen (SON) 11 and 21% in corn and 22 and 12 % in cotton than conventional tillage. Agroforestry system at farmers’ field enhance soil biological activity and amongst trees, P. cineraria based system brought maximum and significant improvement in soil biological activity (Yadav et al ., 2011).
Soil organic carbon stock changes under grazed grasslands in New ZealandExternalEvents
This presentation was presented during the 2 Parallel session on Theme 3.2, Managing SOC in: Grasslands and livestock production systems, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. David Whitehead, from University of Waikato – New Zealand, in FAO Hq, Rome
Concept of Agro ecosystem
Difference between manipulated Agroecology and Natural Ecology
Sustainable Agriculture
Biodiversification and Agroecology
Sustainable Agroecosystems
Agroecology and the Design of Sustainable Agroecosystems
Global assessment for organic resources and waste management: Assessment of technologies for optimal organics management processes and enlightened environmental policies
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
Presented by The Global Peatlands Assessment: Mapping, Policy, and Action at GLF Peatlands 2024 - The Global Peatlands Assessment: Mapping, Policy, and Action
different Modes of Insect Plant InteractionArchita Das
different modes of interaction between insects and plants including mutualism, commensalism, antagonism, Pairwise and diffuse coevolution, Plant defenses, how coevolution started
Epcon is One of the World's leading Manufacturing Companies.EpconLP
Epcon is One of the World's leading Manufacturing Companies. With over 4000 installations worldwide, EPCON has been pioneering new techniques since 1977 that have become industry standards now. Founded in 1977, Epcon has grown from a one-man operation to a global leader in developing and manufacturing innovative air pollution control technology and industrial heating equipment.
Top 8 Strategies for Effective Sustainable Waste Management.pdfJhon Wick
Discover top strategies for effective sustainable waste management, including product removal and product destruction. Learn how to reduce, reuse, recycle, compost, implement waste segregation, and explore innovative technologies for a greener future.
Microbial characterisation and identification, and potability of River Kuywa ...Open Access Research Paper
Water contamination is one of the major causes of water borne diseases worldwide. In Kenya, approximately 43% of people lack access to potable water due to human contamination. River Kuywa water is currently experiencing contamination due to human activities. Its water is widely used for domestic, agricultural, industrial and recreational purposes. This study aimed at characterizing bacteria and fungi in river Kuywa water. Water samples were randomly collected from four sites of the river: site A (Matisi), site B (Ngwelo), site C (Nzoia water pump) and site D (Chalicha), during the dry season (January-March 2018) and wet season (April-July 2018) and were transported to Maseno University Microbiology and plant pathology laboratory for analysis. The characterization and identification of bacteria and fungi were carried out using standard microbiological techniques. Nine bacterial genera and three fungi were identified from Kuywa river water. Clostridium spp., Staphylococcus spp., Enterobacter spp., Streptococcus spp., E. coli, Klebsiella spp., Shigella spp., Proteus spp. and Salmonella spp. Fungi were Fusarium oxysporum, Aspergillus flavus complex and Penicillium species. Wet season recorded highest bacterial and fungal counts (6.61-7.66 and 3.83-6.75cfu/ml) respectively. The results indicated that the river Kuywa water is polluted and therefore unsafe for human consumption before treatment. It is therefore recommended that the communities to ensure that they boil water especially for drinking.
Climate Change All over the World .pptxsairaanwer024
Climate change refers to significant and lasting changes in the average weather patterns over periods ranging from decades to millions of years. It encompasses both global warming driven by human emissions of greenhouse gases and the resulting large-scale shifts in weather patterns. While climate change is a natural phenomenon, human activities, particularly since the Industrial Revolution, have accelerated its pace and intensity
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
2. Presentation Outline
1. Carbon sequestration concepts and
rationale
2. Relevant management approaches to avoid
land degradation and foster carbon
sequestration
3. Summary of research quantifying soil
carbon sequestration
3. Global Concern is in the AirThe difference of radiant energy received by the Earth and energy radiated back to space
4. Greenhouse effect
The greenhouse effect is a process by which
thermal radiation from a planetary surface is
absorbed by atmospheric greenhouse gases,
and is re-radiated in all directions.
6. Why are Greenhouse Gases Important?
1. Global ecological concern for the anthropogenic
source of increasing concentration in the
atmosphere since 1750 (Intergovernmental Panel
on Climate Change, 2001):
CO2 – 31% increase
CH4 – 151% increase
N2O – 17% increase
1. Cause radiative forcing of the atmosphere, which
could alter global temperature and ecosystem
functioning
2. Can be manipulated by human activities
8. Managing Carbon Emission
Rising concentration of greenhouse gases has
been largely attributed to expanding use of fossil
fuels as an energy source, resulting in emission of
CO2 to the atmosphere
Reducing net greenhouse gas emission is possible:
1.Reduce fossil fuel combustion by becoming more energy
efficient
2.Rely more on low-carbon energy sources
• Solar energy capture
• Wind power generation
• Biomass fuels (fuel that contains energy from geologically recent carbon fixation. These fuels are
produced from living organisms.)
1.Carbon sequestration
9. Carbon Sequestration
Carbon sequestration is the process of capture and
long-term storage of atmospheric carbon dioxide and
may refer specifically to: "The process of removing
carbon from the atmosphere and depositing it in a
reservoir."
10. Carbon Sequestration
Long-term storage of carbon in:
1. Terrestrial biosphere
2. Underground in geologic formations
3. Oceans
so that the buildup of CO2 will reduce or slow
11. Terrestrial Carbon Sequestration
1. Increasing the net fixation of atmospheric CO2 by
terrestrial vegetation with emphasis on enhancing
physiology and rate of photosynthesis of vascular
plants
2. Retaining carbon in plant materials and
enhancing the transformation of carbon to soil
organic matter
3. Reducing the emission of CO2 from soils caused
by heterotrophic oxidation of soil organic carbon
4. Increasing the capacity of deserts and degraded
lands to sequester carbon
12. Terrestrial Carbon Sequestration
A t m o s p h e r ic
C O 2
P la n t
r e s p ir a t io n
A n im a l
r e s p ir a t io n
S o il r e s p ir a t io n
P h o t o s y n t h e s is
S o il
o r g a n is m s
S o il
o r g a n ic
m a t t e r
D is s o lv e d
C O
in w a t e r
2
L e a c h a t e
A t m o s p h e r ic
N 2
M in e r a liz a t io n
D e n it r if ic a t io n
B io lo g ic a l
N f ix a t io n
C a r b o n a t e
m in e r a ls
F o s s il f u e ls
C O 2
N
N O
N
2
2
O
N H
v o la t iliz a t io n
3
N H
f ix a t io n
4
P la n t
u p t a k e
F e r t iliz e r
Carbon
Input
Carbon
Output
Soil
Carbon
Sequestration
13. Focus on maximizing carbon input
Plant selection
• Species, cultivar, variety
• Growth habit (perennial / annual)
• Rotation sequence
• Biomass energy crops
Tillage
• Type
• Frequency
Fertilization
• Rate, timing, placement
• Organic amendments
Management Approaches
to Sequester Carbon
from Atmosphere to Biosphere
Integrated management
• Pest control
• Crop / livestock systems
ARS Image Number K5141-4
14. Focus on minimizing carbon loss from soil
Reducing soil disturbance
• Less intensive tillage
• Controlling erosion
Utilizing available soil water
• Promotes optimum plant growth
• Reduces soil microbial activity
Maintaining surface residue cover
• Increased plant water use and production
• More fungal dominance in soil
Management Approaches
to Sequester Soil Carbon
from Atmosphere to Biosphere
ARS Image Number K7520-2
15. Tree plantings
Conservation-tillage cropping
Animal manure application
Green-manure cropping systems
Improved grassland management
Cropland-grazingland rotations
Optimal fertilization
Management Practices
to Sequester Carbon
and Counter Land Degradation
ARS Image Number K5951-1
16. Tree plantings have the
advantage of accumulating
carbon in perennial biomass
of above- and below-ground
growth, as well as in soil
organic matter.
Tree Plantings
www.amityfoundation.org/
www.amityfoundation.org/
Issues of importance are:
• Climate
• Selecting adapted species
• Soil condition
• Plant density
• Intended use
• Type of intercropping
17. Tree Plantings
Data from Environment Australia (1998).
Plantation survey data in 400-600 mm/yr
zone. Mean carbon accumulation rate of
3.8 Mg C/ha/yr.
Years
0 10 20 30 40 50
Above-Ground
Carbon
Accumulation
(Mg / ha)
0
100
200
300
400
500
Using CENTURY and
RothC models in Sudan
and Nigeria, soil
organic C accumulation
with tree plantings was
estimated at 0.10 + 0.05
Mg C/ha/yr (Farage et
al., 2007, Soil Till. Res.)
Photo by Mamadou Doumbia
18. Minimal disturbance of the
soil surface is critical in
avoiding soil organic
matter loss from erosion
and microbial
decomposition.
Conservation-Tillage Cropping
19. In the USA and Canada, no-tillage cropping can
sequester an average of 0.33 Mg C/ha/yr.
Conservation-Tillage Cropping
Franzluebbers and Follett (2005) Soil Tillage Res. 83:1-8
Cold-dry region
(6 °C, 400 mm)
0.27 + 0.19 Mg C/ha/yr
Northwest
Hot-dry region
(18 °C, 265 mm)
0.30 + 0.21 Mg C/ha/yr
Southwest
Hot-wet region
(20 °C, 1325 mm)
0.42 + 0.46 Mg C/ha/yr
Southeast
Cold-wet region
(6 °C, 925 mm)
−0.07 + 0.27 Mg C/ha/yrNortheast
Mild region
(12 °C, 930 mm)
0.48 + 0.59 Mg C/ha/yr
Central
20. No tillage needs high-residue producing cropping
system to be effective.
Conservation-Tillage Cropping
Soil Organic Carbon Sequestration
in the Southeastern USA
----------------------------------------------------
0.28 + 0.44 Mg C/ha/yr
(without cover cropping)
0.53 + 0.45 Mg C/ha/yr
(with cover cropping)
Franzluebbers (2005) Soil Tillage Res. 83:120-147.
Photos of 2 no-tillage
systems in Virginia USA
21. From the 12th
year of an irrigated wheat-maize rotation
in the volcanic highlands of central Mexico, rate of
water infiltration, crop yield, and soil organic C
reflected differences in surface soil condition due to
residue management:
Conservation-Tillage Cropping
Govaerts et al. (2006) Soil Tillage Res. (in press)
Infiltration Yield (Mg ha-1
) 1996-2002
Tillage Residues (cm h-1
) Maize Wheat
------------------------------------------------------------------------------------------------
Zero Without
Zero With
------------------------------------------------------------------------------------------------
18
90
3.4
4.8
3.9
5.4
Retaining residues for 12 years significantly increased soil organic C,
but absolute treatment values were not reported.
22. Animal Manure Application
Since animal manure contains 40-60% carbon, its
application to land should promote soil organic C
sequestration.
Soil Organic C (Mg ha-1
)
Effect of manure application Without With
----------------------------------------------------------------------------------------------
----------------------------------------------------------------------------------------------
2-yr studies (n=6) 19.8 + 8.9 19.6 + 8.4
11 + 8-yr studies (n=8) 30.6 + 11.4 36.8 + 10.6
SOC sequestration for all (Mg ha-1
yr-1
) 0.26 + 2.15
SOC sequestration for >2-yr studies 0.72 + 0.67
Conversion of C in poultry litter
to soil organic C was 17 + 15%.
Note: Manure application
transfers C from one land to
another. Franzluebbers (2005) Soil Tillage Res. 83:120-147.
23. Animal Manure Application
Long-term studies on farmyard manure (FYM)
application to soil clearly show its benefit to soil
fertility, yield enhancement, and soil C storage:
Kapkiyai et al. (1999) Soil Biol. Biochem. 31:1773-1782
18-yr field experiment in Kenya (23 °C, 970 mm)
0.17 + 0.07 Mg C ha-1
yr-1
with 10 Mg ha-1
yr-1
FYM compared to
without FYM
9 + 3% of added C retained in soil
Crop yield with FYM (5.3 Mg ha-1
) > without FYM (3.3 Mg ha-1
)
Agbenin and Goladi (1997) Agric. Ecosyst. Environ. 63:17-24
45-yr field experiment in Nigeria (28 °C, 1070 mm)
0.21+ 0.01 Mg C ha-1
yr-1
with 5 Mg ha-1
yr-1
FYM compared to
without FYM
Total soil phosphorus increased with FYM (21 + 12 kg ha-1
yr-1
)
24. Animal Manure Application
Gupta et al. (1992) Arid Soil Res. Rehabil. 6:243-251
20-yr study in India
(26 °C, 440 mm)
Pearl millet–wheat
Farmyard Manure Rate (Mg
.
ha
-1
)
0 10 20 30 40 50
Soil
Organic
Carbon
(Mg
.
ha
-1
)
0
5
10
15
20
At the end of 20 years
Initially (9.4)
0
5
10
15
20
Percentage
of Carbon
Applied
as FYM
Retained
in Soil
(%)
25. Animal Manure Application
Soil carbon retention rate from manure application is
affected by climatic condition:
Temperate or frigid regions (23 + 15%)
Thermic regions (7 + 5%)
Moist regions (8 + 4%)
Dry regions (11 + 14%)
Percentage of carbon applied as manure retained in soil
(review of literature in 2001)
26. On an abandoned brick-making site in southeastern China (16.5 °C,
1600 mm) [Zhang and Fang (2006) Soil Tillage Res. (in press)],
Planting of ryegrass (Lolium perenne) under China fir (Cunninghamia
lanceolata) for 7 years resulted in soil organic C sequestration of
0.36 + 0.40 Mg C ha-1
yr-1
.
Green-Manure Cropping Systems
www.agroecology.org/cases/
greenmanure.htm
With soybean as a green manure for 8
years in Columbia (27 °C, 2240 mm)
(Basamba et al., 2006; Soil Tilllage
Res. 91:131-142):
Green
Response Control Manure
------------------------------------------------------------
Maize yield (Mg ha-1
) 3.5 4.2
Soil organic C (g kg-1
) 24.9 23.8
------------------------------------------------------------
27. Degradation of permanent grasslands can occur
from accelerated soil erosion, compaction, drought,
and salinization
Strategies to sequester carbon in soil should
improve quality of grasslands
Strategies for restoration should include:
Improved Grassland Management
Enhancing soil cover
Improving soil structure to
minimize water runoff and soil
erosion
28. Improved Grassland Management
Franzluebbers et al. (2001) Soil Sci. Soc. Am. J. 65:834-841 and unpublished data
Years of Management
0 1 2 3 4 5 6 7 8
Soil
Organic
Carbon
(Mg
.
ha
-1
)
12
14
16
18
20
22
24
Cut for hay
Years of Management
0 1 2 3 4 5 6 7 8
Soil
Organic
Carbon
(Mg
.
ha
-1
)
12
14
16
18
20
22
24
Cut for hay
Unharvested
Years of Management
0 1 2 3 4 5 6 7 8
Soil
Organic
Carbon
(Mg
.
ha
-1
)
12
14
16
18
20
22
24
Unharvested
Cut for hay
Low
grazing pressure
Years of Management
0 1 2 3 4 5 6 7 8
Soil
Organic
Carbon
(Mg
.
ha
-1
)
12
14
16
18
20
22
24
Unharvested
Cut for hay
Low
grazing pressure
High
grazing
pressure
Establishment of
bermudagrass
pasture following
long-term
cropping in
Georgia USA (16
°C, 1250 mm)
Soil organic carbon
sequestration rate
(Mg ha-1
yr-1
) (0-5 yr):
-------------------------------
-Hayed 0.30
Unharvested 0.65
Grazed 1.40
29. Summary and Conclusions
Greenhouse gas concentrations in the atmosphere
are increasing and the threat of global change
requires our attention
A diversity of agricultural management practices
can be employed to sequester more carbon in
plants and soil
Syntheses of available data are needed
Gaps in our knowledge need to be researched
Strategies to sequester soil carbon will also likely
restore degraded land and avoid further
degradation