Add to ORKGClimate is, in many instances, the dominant variable controlling the storage of carbon in soils. It has proven difficult, however, to determine how soil properties influenced by climate, such as soil temperature and soil moisture, actually operate to determine the rates of accumulation and decomposition of soil organic matter. Our approach has been to apply a relatively new tool, the comparison of C-14 in soil organic matter from pre- and post-bomb soils, to quantify carbon turnover rates along climosequences. This report details the progress made toward this end by work under this contract
Carbon dioxide release during soil organic carbon (SOC) turnover is a pivotal component of atmospher...
This is the final version. Available on open access from Nature Research via the DOI in this recordD...
Soils represent the largest carbon pool in the terrestrial biosphere, and climate change might affec...
The magnitude and timing of the response of the soil carbon reservoir to changes in land use or clim...
Understanding the mechanisms of soil carbon (C) formation and loss is essential for predicting the C...
Recent improvements in our understanding of the dynamics of soil carbon have shown that 20-40% of th...
Soil carbon, a major component of the global carbon inventory, has significant potential for change ...
The soil system stores more carbon than the atmosphere and biosphere combined. However, until recent...
Historically, attention on soil organic matter (SOM) has focused on the central role that it plays i...
Although soil contains about three times the amount of carbon present in the preindustrial atmospher...
Storing large amounts of organic carbon, soils are a key but uncertain component of the global carbo...
Measurements of CO2 flux, soil temperature, and moisture content of selected natural and disturbed s...
International audienceThe size of the organic carbon reservoir of the planet's soils is estimated to...
Comparison of C-14 (carbon-14) in archived (pre-1963) and contemporary soils taken along an elevatio...
Artículo de publicación ISISoils are an important site of carbon storage(1). Climate is generally re...
Carbon dioxide release during soil organic carbon (SOC) turnover is a pivotal component of atmospher...
This is the final version. Available on open access from Nature Research via the DOI in this recordD...
Soils represent the largest carbon pool in the terrestrial biosphere, and climate change might affec...
The magnitude and timing of the response of the soil carbon reservoir to changes in land use or clim...
Understanding the mechanisms of soil carbon (C) formation and loss is essential for predicting the C...
Recent improvements in our understanding of the dynamics of soil carbon have shown that 20-40% of th...
Soil carbon, a major component of the global carbon inventory, has significant potential for change ...
The soil system stores more carbon than the atmosphere and biosphere combined. However, until recent...
Historically, attention on soil organic matter (SOM) has focused on the central role that it plays i...
Although soil contains about three times the amount of carbon present in the preindustrial atmospher...
Storing large amounts of organic carbon, soils are a key but uncertain component of the global carbo...
Measurements of CO2 flux, soil temperature, and moisture content of selected natural and disturbed s...
International audienceThe size of the organic carbon reservoir of the planet's soils is estimated to...
Comparison of C-14 (carbon-14) in archived (pre-1963) and contemporary soils taken along an elevatio...
Artículo de publicación ISISoils are an important site of carbon storage(1). Climate is generally re...
Carbon dioxide release during soil organic carbon (SOC) turnover is a pivotal component of atmospher...
This is the final version. Available on open access from Nature Research via the DOI in this recordD...
Soils represent the largest carbon pool in the terrestrial biosphere, and climate change might affec...