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Journal ArticleDOI

Soil carbon sequestration impacts on global climate change and food security.

Rattan Lal
- 11 Jun 2004 - 
- Vol. 304, Iss: 5677, pp 1623-1627
TLDR
In this article, the carbon sink capacity of the world’s agricultural and degraded soils is 50 to 66% of the historic carbon loss of 42 to 78 gigatons of carbon.
Abstract
:The carbon sink capacity of the world’s agricultural and degraded soils is 50 to 66% of the historic carbon loss of 42 to 78 gigatons of carbon. The rate of soil organic carbon sequestration with adoption of recommended technologies depends on soil texture and structure, rainfall, temperature, farming system, and soil management. Strategies to increase the soil carbon pool include soil restoration and woodland regeneration, no-till farming, cover crops, nutrient management, manuring and sludge application, improved grazing, water conservation and harvesting, efficient irrigation, agroforestry practices, and growing energy crops on spare lands. An increase of 1 ton of soil carbon pool of degraded cropland soils may increase crop yield by 20 to 40 kilograms per hectare (kg/ha) for wheat, 10 to 20 kg/ha for maize, and 0.5 to 1 kg/ha for cowpeas. As well as enhancing food security, carbon sequestration has the potential to offset fossilfuel emissions by 0.4 to 1.2 gigatons of carbon per year, or 5 to 15% of the global fossil-fuel emissions.

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Book

Climate change and water.

TL;DR: The Intergovernmental Panel on Climate Change (IPCC) Technical Paper Climate Change and Water draws together and evaluates the information in IPCC Assessment and Special Reports concerning the impacts of climate change on hydrological processes and regimes, and on freshwater resources.
Journal ArticleDOI

The contentious nature of soil organic matter

TL;DR: It is argued that the available evidence does not support the formation of large-molecular-size and persistent ‘humic substances’ in soils, and instead soil organic matter is a continuum of progressively decomposing organic compounds.
Journal ArticleDOI

Stability of organic carbon in deep soil layers controlled by fresh carbon supply

TL;DR: It is proposed that a lack of supply of fresh carbon may prevent the decomposition of the organic carbon pool in deep soil layers in response to future changes in temperature.
References
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Journal ArticleDOI

Soil organic carbon sequestration rates by tillage and crop rotation : A global data analysis

TL;DR: In this article, the authors quantify potential soil organic carbon sequestration rates for different crops in response to decreasing tillage intensity or enhancing rotation complexity, and to estimate the duration of time over which sequestration may occur.
Journal ArticleDOI

Soil Erosion and the Global Carbon Budget

TL;DR: Soil erosion has a strong impact on the global C cycle and this component must be considered while assessing theglobal C budget and adoption of conservation-effective measures may reduce the risks of C emission and sequester C in soil and biota.
Journal ArticleDOI

The Anthropogenic Greenhouse Era Began Thousands of Years Ago

TL;DR: The anthropogenic era is generally thought to have begun 150 to 200 years ago, when the industrial revolution began producing CO2 and CH4 at rates sufficient to alter their compositions in the atmosphere as discussed by the authors.
Journal ArticleDOI

Soil organic matter, biota and aggregation in temperate and tropical soils - Effects of no-tillage

TL;DR: In this paper, the long-term stabilization of soil organic matter (SOM) in tropical and temperate regions is mediated by soil biota (e.g. fungi, bacte- ria, roots and earthworms), soil structure and their interactions.
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