Understanding the biogeochemistry of soil organic carbon (SOC) and SOC components is essential to assess soil quality and management practices in reclaimed croplands. Here we study the radiocarbon (C-14) ages in profiles to a depth of 500 cm for five cultivation timespans: 5, 15, 35, 60, and at least 70 years from the Gutun watershed on the Chinese Loess Plateau. We isolated an acid-extractable SOC component (F1), three temperature stepped-combustion SOC components: F2 (400 degrees C), F3 (600 degrees C), and F4 (900 degrees C), and measured their C-14 ages. Our results show that SOC stocks in reclaimed soils declined from cultivation times of 5 years (R5) to 15 years (R15), then increased with longer cultivation times, until 70 years (R70)...
Fine roots are the most dynamic portion of a plant's root system and a major source of soil organic ...
We collected soil samples from depths between 0 and 12–21 m at 33 sites across the Chinese Loe...
Intensive soil tillage is a significant factor in soil organic matter decline in cultivated soils. B...
Knowledge of soil carbon (C) dynamics following vegetation restoration is essential for evaluating c...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
Radiocarbon data from soil organic matter and soil respiration provide powerful constraints for dete...
Radiocarbon data from soil organic matter and soil respiration provide powerful constraints for dete...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
Quantification of the dynamics of soil organic carbon (SOC) pools under the influence of different c...
The vertical distribution and exchange mechanisms of soil organic and inorganic carbon (SOC, SIC) pl...
An accurate evaluation of soil organic C (SOC) stocks is important to C management and to understand...
There still exist uncertainties in the trend, magnitude and efficiency of carbon sequestration with ...
Soil organic carbon (SOC) content and radiocarbon concentration were measured in three particle-size...
Accelerator mass spectrometry (AMS) radiocarbon measurements were used to investigate the heterogene...
Fine roots are the most dynamic portion of a plant's root system and a major source of soil organic ...
We collected soil samples from depths between 0 and 12–21 m at 33 sites across the Chinese Loe...
Intensive soil tillage is a significant factor in soil organic matter decline in cultivated soils. B...
Knowledge of soil carbon (C) dynamics following vegetation restoration is essential for evaluating c...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
Radiocarbon data from soil organic matter and soil respiration provide powerful constraints for dete...
Radiocarbon data from soil organic matter and soil respiration provide powerful constraints for dete...
In a study addressing composition and recovery of soil carbon following pasture installation on arab...
Quantification of the dynamics of soil organic carbon (SOC) pools under the influence of different c...
The vertical distribution and exchange mechanisms of soil organic and inorganic carbon (SOC, SIC) pl...
An accurate evaluation of soil organic C (SOC) stocks is important to C management and to understand...
There still exist uncertainties in the trend, magnitude and efficiency of carbon sequestration with ...
Soil organic carbon (SOC) content and radiocarbon concentration were measured in three particle-size...
Accelerator mass spectrometry (AMS) radiocarbon measurements were used to investigate the heterogene...
Fine roots are the most dynamic portion of a plant's root system and a major source of soil organic ...
We collected soil samples from depths between 0 and 12–21 m at 33 sites across the Chinese Loe...
Intensive soil tillage is a significant factor in soil organic matter decline in cultivated soils. B...