Documenting changes in soil characteristics induced by agricultural practices is important in understanding how different management techniques affect the landscape. Three objectives of the research are: (1) to quantify soil organic carbon (SOC) content (2), to quantify soil morphological properties of the individual pedons, and (3) to determine soil quality relationship across three levels of pasture quality in the Chariton River Watershed, IA. Six pastures were studied in detail with two being each high quality, fair quality, and poor quality. Within each pasture, about ten pedons were collected in a summit-toeslope transect. Significant differences were found between pedons from the different pasture qualities with respect to SOC content...
The largest carbon pools in the world lie within underground. Soils have the ability to sequester C ...
Relatively little is known about soil organic carbon (SOC) dynamics in montane ecosystems of the sem...
Forest and pasture soils should have differing properties due, for example, to differing root charac...
Documenting changes in soil characteristics induced by agricultural practices is important in unders...
A carbon index (Cl) is one of many soil quality indicators that depends on organic carbon concentrat...
There are several factors that influence the retention of soil organic carbon (SOC) and total soil n...
It is crucial to investigate how land-use history and restoration impact soil to further our underst...
Soil organic carbon (SOC) fashions soil structure, which is a key factor of soil fertility. Existing...
The largest carbon (C) pools in the biosphere is in the soils. Thus, soils have the greatest potent...
Soil organic matter is recognized as an important component of soil quality through its influence on...
Increased awareness of the economic and environmental values of prairie and wetland ecosystems has r...
Improvement of carbon sequestration in soils for a more sustainable environment and prevention of cl...
Defining soil organic carbon (SOC) quality and understanding the effects of vegetation cover and cli...
‘‘Capsule’’: Pasture management can improve soil quality and soil carbon sequestration, especially i...
Soil carbon sequestration plays an important role in mitigating the anthropogenic increases in atmos...
The largest carbon pools in the world lie within underground. Soils have the ability to sequester C ...
Relatively little is known about soil organic carbon (SOC) dynamics in montane ecosystems of the sem...
Forest and pasture soils should have differing properties due, for example, to differing root charac...
Documenting changes in soil characteristics induced by agricultural practices is important in unders...
A carbon index (Cl) is one of many soil quality indicators that depends on organic carbon concentrat...
There are several factors that influence the retention of soil organic carbon (SOC) and total soil n...
It is crucial to investigate how land-use history and restoration impact soil to further our underst...
Soil organic carbon (SOC) fashions soil structure, which is a key factor of soil fertility. Existing...
The largest carbon (C) pools in the biosphere is in the soils. Thus, soils have the greatest potent...
Soil organic matter is recognized as an important component of soil quality through its influence on...
Increased awareness of the economic and environmental values of prairie and wetland ecosystems has r...
Improvement of carbon sequestration in soils for a more sustainable environment and prevention of cl...
Defining soil organic carbon (SOC) quality and understanding the effects of vegetation cover and cli...
‘‘Capsule’’: Pasture management can improve soil quality and soil carbon sequestration, especially i...
Soil carbon sequestration plays an important role in mitigating the anthropogenic increases in atmos...
The largest carbon pools in the world lie within underground. Soils have the ability to sequester C ...
Relatively little is known about soil organic carbon (SOC) dynamics in montane ecosystems of the sem...
Forest and pasture soils should have differing properties due, for example, to differing root charac...