- The document evaluates the benefits of biochar on soil quality and its effects on soil carbon sequestration as a pathway to sustainability. It discusses how tillage reduces soil carbon and biochar can increase carbon storage. Experiments were conducted on volcanic soils in Guam comparing no-tillage, reduced tillage, conventional tillage, and conventional tillage with biochar application. Results showed biochar can reduce carbon dioxide emissions and increase crop yields compared to other tillage methods. Further research on using biochar and other conservation practices can help sequester carbon and mitigate climate change.
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.
Dr Andrew Rawson: Soil Carbon Sequestration in a Changing ClimateCarbon Coalition
Dr Andrew Rawson of the NSW Department of the Environment and Climate Change, explains why climate change is blamed for more than it can be held to have caused. This presentation was given at the Carbon farming Expo & Conference in Orange NSW Australia in November 2008.
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.
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.
Dr Andrew Rawson: Soil Carbon Sequestration in a Changing ClimateCarbon Coalition
Dr Andrew Rawson of the NSW Department of the Environment and Climate Change, explains why climate change is blamed for more than it can be held to have caused. This presentation was given at the Carbon farming Expo & Conference in Orange NSW Australia in November 2008.
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.
Climate Smart Agriculture and Soil-Carbon SequestrationSIANI
Part of the Swedish seminar "Från kolkälla till kolfälla: Om framtidens klimatsmarta jordbruk"
8th May 2012, 13.00 - 16.30
Kulturhuset, Stockholm
Marja-Liisa Tapio-Biström, FAO, gives a global overview of carbon in soil.
PhD research presentation at the workshop of the Climate Food and Farming Network, Dec. 2-4 at Aarhus University, Foulum. The Climate Food and Farming Network is an initiative of Copenhagen U., Aarhus U., and the CGIAR Research Program on Climate Change, Agriculture and Food Security.
global warming solution, deposition of carbon in soils , why it is done , methods followed, steps in carbon sequestration,effects of excess carbon dioxide,carbon dating
Carbon sequestration is the process involved in carbon capture and the long-term storage of atmospheric carbon dioxide (CO
2)[1] and may refer specifically to:
"The process of removing carbon from the atmosphere and depositing it in a reservoir."[4] When carried out deliberately, this may also be referred to as carbon dioxide removal, which is a form of geoengineering.
Carbon capture and storage, where carbon dioxide is removed from flue gases (e.g., at power stations) before being stored in underground reservoirs.
Natural biogeochemical cycling of carbon between the atmosphere and reservoirs, such as by chemical weathering of rocks.
Challenges of soil organic carbon sequestration in drylandsExternalEvents
This presentation was presented during the 1 Parallel session on Theme 3.3, Managing SOC in: Dryland soils, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Rachid Mrabet , from INRA – Morocco, in FAO Hq, Rome
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
There is a renewed interest in the role of agriculture at the climate change negotiations, as evidenced by a number of interesting side-events during COP 16 in Cancun. The reason is simple: Agriculture and related activities account for a third of global greenhouse gas (GHG) emissions, most of which can be mitigated, an opportunity that policy makers simply cannot afford to miss. What’s more, some of the techniques that sequester carbon have the added advantage of building the water-retention capacity and nutrient content of soils, hence contributing to a triple-win situation where mitigation, adaptation and yield increases are all addressed.
In response to this, SIANI and Sida arranged a one-day workshop on the theme From Source to Sink: How to make Agriculture part of the Solution to Climate Change while contributing to Poverty Alleviation? The main purpose of the workshop was to link the multiple potentials of agriculture to other development goals such as over-all poverty alleviation and food security, with particular reference to the needs of smallholder farmers who make up 70% of the world’s poorest people.
Effect of Global Warming on Soil Organic CarbonAmruta Raut
Currently surface Temperature are rising by about 0.2 °C (0.36 °F) per decade so how it will affect soil organic carbon level and what are the different strategies to sequester carbon explain in detail
Climate Smart Agriculture and Soil-Carbon SequestrationSIANI
Part of the Swedish seminar "Från kolkälla till kolfälla: Om framtidens klimatsmarta jordbruk"
8th May 2012, 13.00 - 16.30
Kulturhuset, Stockholm
Marja-Liisa Tapio-Biström, FAO, gives a global overview of carbon in soil.
PhD research presentation at the workshop of the Climate Food and Farming Network, Dec. 2-4 at Aarhus University, Foulum. The Climate Food and Farming Network is an initiative of Copenhagen U., Aarhus U., and the CGIAR Research Program on Climate Change, Agriculture and Food Security.
global warming solution, deposition of carbon in soils , why it is done , methods followed, steps in carbon sequestration,effects of excess carbon dioxide,carbon dating
Carbon sequestration is the process involved in carbon capture and the long-term storage of atmospheric carbon dioxide (CO
2)[1] and may refer specifically to:
"The process of removing carbon from the atmosphere and depositing it in a reservoir."[4] When carried out deliberately, this may also be referred to as carbon dioxide removal, which is a form of geoengineering.
Carbon capture and storage, where carbon dioxide is removed from flue gases (e.g., at power stations) before being stored in underground reservoirs.
Natural biogeochemical cycling of carbon between the atmosphere and reservoirs, such as by chemical weathering of rocks.
Challenges of soil organic carbon sequestration in drylandsExternalEvents
This presentation was presented during the 1 Parallel session on Theme 3.3, Managing SOC in: Dryland soils, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Rachid Mrabet , from INRA – Morocco, in FAO Hq, Rome
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
There is a renewed interest in the role of agriculture at the climate change negotiations, as evidenced by a number of interesting side-events during COP 16 in Cancun. The reason is simple: Agriculture and related activities account for a third of global greenhouse gas (GHG) emissions, most of which can be mitigated, an opportunity that policy makers simply cannot afford to miss. What’s more, some of the techniques that sequester carbon have the added advantage of building the water-retention capacity and nutrient content of soils, hence contributing to a triple-win situation where mitigation, adaptation and yield increases are all addressed.
In response to this, SIANI and Sida arranged a one-day workshop on the theme From Source to Sink: How to make Agriculture part of the Solution to Climate Change while contributing to Poverty Alleviation? The main purpose of the workshop was to link the multiple potentials of agriculture to other development goals such as over-all poverty alleviation and food security, with particular reference to the needs of smallholder farmers who make up 70% of the world’s poorest people.
Effect of Global Warming on Soil Organic CarbonAmruta Raut
Currently surface Temperature are rising by about 0.2 °C (0.36 °F) per decade so how it will affect soil organic carbon level and what are the different strategies to sequester carbon explain in detail
La Convención de las Naciones Unidas de Lucha contra la Desertificación acaba de publicar un informe en el que se señala la importancia de carbono orgánico de los suelos orientado a los decisores políticos y que se presentará en la próxima reunión de la UNFCCC sobre cambio climático que se celebrará en París (COP21).
Mitigation Strategies to Greenhouse Gas Emission Control: A Database for Emis...IJSRD
With the advancement of Industrial Revolution, the anthropogenic activities have brought about increase in the quantities of greenhouse gases (GHGs) into the atmosphere leading to various climatic changes. The climate change is mainly caused by production of GHG emissions in the atmosphere. As the major population of the world seems to agree with the concept of ‘human development’ including the ‘environment’ factor, the various attempts for sustainability is not found to be interesting or beneficial. Therefore, the main motto of the world is to improve the standard of living by attaining suitable measures. However, most of the population on earth still do not get ‘bare minimum’ for development; the humanity faces the challenge of the “Climate Changeâ€Â. Various efforts need to address climate change through mitigation of GHG emissions and building of adaptive capacities to deal with the severe impacts of climate change.
Mitigation Strategies to Greenhouse Gas Emission Control: A Database for Emis...IJSRD
With the advancement of Industrial Revolution, the anthropogenic activities have brought about increase in the quantities of greenhouse gases (GHGs) into the atmosphere leading to various climatic changes. The climate change is mainly caused by production of GHG emissions in the atmosphere. As the major population of the world seems to agree with the concept of ‘human development’ including the ‘environment’ factor, the various attempts for sustainability is not found to be interesting or beneficial. Therefore, the main motto of the world is to improve the standard of living by attaining suitable measures. However, most of the population on earth still do not get ‘bare minimum’ for development; the humanity faces the challenge of the “Climate Changeâ€Â. Various efforts need to address climate change through mitigation of GHG emissions and building of adaptive capacities to deal with the severe impacts of climate change.
GSR's Monthly Newsletter. This month features a in-depth guest article about Carbon Sequestration through Sustainable Restorative Agriculture (SRA) by Chris Danch.
Global warming is a phenomenon of climate change characterized by a general increase in average temperatures of the Earth, which modifies the weather balances and ecosystems for a long time. It is directly linked to the increase of greenhouse gases in our atmosphere, worsening the greenhouse effect.
Multiple Benefits of SLCP Mitigation in Alpine and Polar RegionsInfoAndina CONDESAN
Presentation of Johan C.I. Kuylenstierna, Director of the Stockholm Environment Institute York Centre
It describe the main findings of an Integrated Assessment developed under UNEP and WMO on tropospheric ozone and black carbon. This has been put together by key experts around the globe, with Drew Shindell of NASA-GISS as the Chair of the Assessment and which has been coordinated by the Stockholm Environment Institute. Tropospheric ozone is ozone which is formed in the lower atmosphere – different from Stratospheric ozone layer. This ozone is not emitted but created in the atmosphere from emitted precursors, of which methane and carbon monoxide are important ones. Black carbon is emitted as particles of carbon – essentially the main compnent of soot. These substances warm the atmosphere and act as air pollutants and there has been a lot of interest recently in the potential for reducing climate warming by addressing these substances.
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
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Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
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
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Improving the viability of probiotics by encapsulation methods for developmen...Open Access Research Paper
The popularity of functional foods among scientists and common people has been increasing day by day. Awareness and modernization make the consumer think better regarding food and nutrition. Now a day’s individual knows very well about the relation between food consumption and disease prevalence. Humans have a diversity of microbes in the gut that together form the gut microflora. Probiotics are the health-promoting live microbial cells improve host health through gut and brain connection and fighting against harmful bacteria. Bifidobacterium and Lactobacillus are the two bacterial genera which are considered to be probiotic. These good bacteria are facing challenges of viability. There are so many factors such as sensitivity to heat, pH, acidity, osmotic effect, mechanical shear, chemical components, freezing and storage time as well which affects the viability of probiotics in the dairy food matrix as well as in the gut. Multiple efforts have been done in the past and ongoing in present for these beneficial microbial population stability until their destination in the gut. One of a useful technique known as microencapsulation makes the probiotic effective in the diversified conditions and maintain these microbe’s community to the optimum level for achieving targeted benefits. Dairy products are found to be an ideal vehicle for probiotic incorporation. It has been seen that the encapsulated microbial cells show higher viability than the free cells in different processing and storage conditions as well as against bile salts in the gut. They make the food functional when incorporated, without affecting the product sensory characteristics.
Presented by The Global Peatlands Assessment: Mapping, Policy, and Action at GLF Peatlands 2024 - The Global Peatlands Assessment: Mapping, Policy, and Action
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
1. Evaluating the benefits of ‘Biochar’ on soil quality
while determining its effect on ‘Soil Carbon
Sequestration – A pathway to Sustainability
Mohammad H. Golabi, Ph.D.
Soil and Environmental Scientist
COLLEGE OF NATURAL AND APPLIED SCIENCES
University of GuamUniversity of Guam
Presented at the:Presented at the:
72nd
Annual SWCS, Madison, Wisconsin
July 30th
- August 2nd
, 2017
2. Climate Change Indicators (cont‘d)
• The average temperature in the United States has risen more
than two degrees Fahrenheit in the past 50 years.
• Increasing temperatures are having wide-ranging effects on
forests and grasslands, including stream flow, precipitation
patterns, snowpack, insects, and invasive plant species, and
influencing drought, heat waves, and wildfire.
• These are just a few examples of the observed effects of
climate change around the United States, and most effects are
expected to continue and intensify during this century
Climate Change Resource Center
USDA-Forest services
3. Is it Real?!
• The climate is certainly changing as the
result of increased temperature. And, it
will continue to change therefore, we need
to work with a plausible range of future
climates behavior that incorporates the
variety of GHG emissions through various
pathways.
Climate Change Resource
Center USDA-Forest services
4. SOME OF GASES
RESPONSIBLE FOR
GREENHOUSE
EFFECT:
Carbon dioxide
Nitrous oxide
Methane gas
Water vapor
And others, ….
Climate Change Resource Center
USDA-Forest services
5. Which one of these gases is to be blamed for the
Climate Change?
a. Carbon dioxide (CO2) generated from the
fossil fuel burning?
b. Methane from the Cows?
c. Rice paddies in Asia?
1. nitrous oxide (N2O)
2. methane (CH4)
a. Carbon dioxide (CO2) from the ‘Soil’
b. All of the above?
c. None of the above?
6. The carbon factor
• Carbon is found in the soilsoil both in organic and
inorganic forms.
• In terrestrial ecosystem, ‘the soil’‘the soil’ represents
the major reservoir of organic carbon.
• At the global level, the soil organic matter
(SOM) pool (estimated to 1 meter depth)
contains about 1580 Pg of carbon (Pg = 1015
g)
Werner L. Michael et.al., 2009
7. The carbon factor (cont’d)
• Most of the soil organic carbon is in a continuous
dynamic state of accumulation as well as
decomposition.
• There is a continuous exchange of carbon
between the soil and the atmosphere, mostly as
carbon dioxide (CO2) and methane (CH4).
• Consequently, any net carbon loss from the soil
means increase of the CO2and/or CH4
concentration in the atmosphere.
8. The carbon factor (cont’d)
• This cycling of carbon between the soil and the
atmosphere (CO2 and CH4) amounts to 80Pg,
roughly 10 times10 times the annual flux of CO2 from all
the fossil fuel combustion combined and it is
increasingly influenced by land use and land
degradation activities
• Crucially soil disturbances (e.g., cultivation and
intensive agriculture) leads to significant soil
carbon losses of 50Pg carbon or more.
Climate Change Resource Center
USDA-Forest services
9. No. 1, Environmental Enemy in
Production Agriculture is:
Intensive Tillage
D.C. Reicosky
10.
11.
12. The carbon factor (cont’d)
• Conversely, Best Management Practices (BMP)
on the land-use can offer an opportunity for
sequestering (storing) atmospheric carbon in
the soil itself.
• The Soils Carbon hold a key role in reducing
atmospheric CO2 and CH4 levels and their
management is subject to; scientific as well as
political, and social analysis.
Werner L. Michael et.al., 2009
13. C
Soil organic matter is a mixture of residual of
plant material in various stages of decomposition
and microbial biomass and all their bi-products
and so:
The “key” component is :
Source: D.C. Reicosky
And Soil is the biggest source of Carbon →
14. Facts about Carbon (cont’d):
• On the other hand the more carbon (C) that
stays in the soil, the less CO2 will be emitted
into the atmosphere.
Therefore;
• Conservation Agriculture, especially no-tillage
(NT) farming, not only will control erosion, but
it will also have the added benefit of restoring
SoilSoil organic CarbonCarbon, thus keeping the
atmospheric CO2 emission down to minimum.
15. Tillage Type
MP SS MK YK RM NT
0
40
80
120
160
MP SS MK YK RM NT
Cum.CO2
Loss(gCO2
m
-2
)
0
20
40
60
80
5 hours after tillage 24 hours after tillage
59.8
31.7
11.5
4.7 3.4
1.4
159.7
66.2
26.7
19.4
15.4
7.2
D.C. Reicosky
16. When we till/plow, we lose tonesWhen we till/plow, we lose tones
ofof carboncarbon in two ways:in two ways:
• Oxidation of Carbon
C + O2 = CO2
• Microbial activities:
generates huge amount of carbon dioxide (CO2),
methane (CH4) and other gases (N2O) which can be
released into the atmosphere by extensive tilling.
17. Sink vs. Source Issues
Sources of CO2:
Fusil fuel burning, etc.
soil organic carbon
Methane gases
Nitrous oxide
etc.
Sinks:
Plants
Trees
Ocean
etc.
18. Atmospheric Carbon as CO2
Plant biomass and roots
left on-or-in the soil
contribute to Soil Carbon
or Soil Organic matter
and with all the
associated environmental
and production benefits.
Energy from
bio-ecosystem
CO2 CO2
Biological carbon cycle.Fossil carbon cycle.
CO2
CEnergy from
fossil fuels
RenewableNonrenewable
Source: D.C. Reicosky
Plant
s act
as
CO2
sinks
↓↓↓↓
↓↓↓↓
19. On the Other Hand;
• We have increased the SOURCES of CO2
emission↑ and reduced the SINKS↓ for the
CO2 Uptake
• Consequently:!
• (Next slide)
21. What to do?
• As soil scientist /environmentalists,
Agriculturists, what can we do to reduce the
CO2 emission into the atmosphere?
22. Case StudyCase Study
Multi-State ProjectMulti-State Project
Evaluate the effect ofEvaluate the effect of conservation tillageconservation tillage onon
carbon storage capacity on these soilscarbon storage capacity on these soils””:▼:▼
““Oxide rich, highly weathered acid soils (very fine,Oxide rich, highly weathered acid soils (very fine,
kaolinitic, isohypothermic oxic Haplustalf) derivedkaolinitic, isohypothermic oxic Haplustalf) derived
from the volcanic deposit”.from the volcanic deposit”.
Evaluate the effect of land application ofEvaluate the effect of land application of
‘‘BiocharBiochar’ on carbon dynamics and CO’ on carbon dynamics and CO22
emission into the atmosphere.emission into the atmosphere.
23. A typical volcanic (Haplustalf)Haplustalf) upland soils (badland)
in southern Guam
24. Challenges facing Guam’s agricultural workers
and soil scientists
Soil and agricultural scientists must develop
strategies to not only control erosion on the
farms, rangelands and the watershed areas
but also sequester (store) carbon.
New techniques must be introduced for soil
conservation and natural resources protection
both in the farm, rangelands as well as on the
watershed areas in the southern mountains.
34. What else can we do to:What else can we do to:
Conserve soilConserve soil, and, and SequesterSequester CarbonCarbon??
- Maintain Surface Cover- Maintain Surface Cover
-- Plant more treesPlant more trees (Sinks)(Sinks)
- Stop Burning (preserve forests)- Stop Burning (preserve forests)
- Farming with BMP’s- Farming with BMP’s
- Enhance SOM content (using- Enhance SOM content (using biocharbiochar))
- Use of- Use of Vetiver TechnologyVetiver Technology toto controlcontrol
erosionerosion andand sequestersequester carbon.carbon. Why/How?Why/How?
35. References and sources sited:
• Climate Change Resource Center, USDA-Forest
services. URL (2016).
• Werner L. Michael et.al., 2009
• D.C. Reicosky, personal communication
• Rattan Lal, 27 Jan., 2000
• Jim Kinsella, 1998
36. References (cont’d)
• Azhar Uddin, 2015. Univ. of Okayama
• (Rodeghiero, et.al., 2009)
• (Rodeghiero, et.al., 2009
Acknowledgement:
• USDA, NIFA for awarding the grant
• and for supporting this study.
Read slide contents.
Strip tillage tools and schematic of loosened soil.
Cumulative CO2 loss after various forms of strip tillage for 5 and 24 hours. Moldboard plow had the greatest loss and No-Till had the least loss. Forms of strip tillage were intermediate and relate to volume of soil loosened by the tool.