Related Experiment Video
Updated: Mar 19, 2026

07:32
Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
Published on: June 4, 2021
5.9K
Carbon storage in Ghanaian cocoa ecosystems
Askia M Mohammed1, James S Robinson2, David Midmore2
1CSIR-Savanna Agricultural Research Institute, Nyankpala, PO Box 52, Tamale, Ghana.
Carbon Balance and Management
|June 25, 2016
Summary
Ghana
Area of Science:
- Agricultural Science
- Environmental Science
- Soil Science
Background:
- Cocoa sector inclusion for carbon storage requires quantifying carbon stocks in Ghana.
- Understanding carbon sequestration in cocoa systems is crucial for national climate strategies.
Purpose of the Study:
- Quantify carbon stocks in shaded and unshaded cocoa systems in Ghana.
- Assess the potential of Ghana's cocoa sector for carbon storage.
Main Methods:
- Measured total ecosystem carbon (biomass C + soil C to 60 cm depth) in farmers' fields.
- Compared carbon stocks in Eastern (ER) and Western (WR) regions of Ghana.
Main Results:
- Total ecosystem carbon stocks ranged from 81.8 to 153.9 Mg C/ha.
- Soils accounted for the majority (~89%) of the carbon stock.
- Western Region cocoa systems showed higher carbon stocks (137.8 ± 8.6 Mg C/ha) than Eastern Region (95.7 ± 8.6 Mg C/ha).
Conclusions:
- Ghana's cocoa sector, covering 1.45 million hectares, could potentially store 118.6-223.2 Gg C.
- Inclusion of the cocoa sector in Ghana's national carbon accounting is justified.
- Shade management did not significantly affect carbon storage in cocoa systems aged within 30 years.
Related Concept Videos
The Carbon Cycle
45.4K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
45.4K
Carbon-dioxide Fixation
835
Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
835
Fats as Energy Storage Molecules
27.4K
Triglycerides are a form of long-term energy storage molecules. They are made of glycerol and three fatty acids. To obtain energy from fat, triglycerides must first be broken down by hydrolysis into their two principal components, fatty acids and glycerol. This process, called lipolysis, takes place in the cytoplasm. The resulting fatty acids are oxidized by β-oxidation into acetyl-CoA, which is used by the Krebs cycle. The glycerol that is released from triglycerides after lipolysis...
27.4K
Fats as Energy Storage Molecules
7.2K
7.2K
C4 Pathway and CAM
50.2K
Most plants use the C3 pathway for carbon fixation. However, some plants, such as sugar cane, corn, and cacti that grow in hot conditions, use alternative pathways to fix carbon and conserve energy loss due to photorespiration. Photorespiration is the process that occurs when the oxygen concentration is high. Under such conditions, the rubisco enzyme in the Calvin cycle binds O2 instead of CO2, which halts photosynthesis and consumes energy.
C4 Pathway
The C4 pathway is used by plants such as...
C4 Pathway
The C4 pathway is used by plants such as...
50.2K
Global Climate Change
29.6K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
29.6K

