emission effects. Most of the previous studies on CO
2
emission effects of eroded soil were carried out at watershed and regional scales by model estimation
but not enough attentionwas paid to the CO
2
emission effects induced by gully erosion. According to the carbon pool redistribution model
organic carbon and Cesium-137 content of soil profiles from three gullies were used to estimate the CO
2
flux induced by gully
erosion on the Loess Hilly Region
and the model prediction efficiency and its influencing factors were tested. The results showed that: (1) After long-term erosion
severe erosion occurred in both erosion area and sedimentary area of gullies in the three study areas. The erosion rate in erosion area was between 30.99 and 46.44 mm/a
and that in sedimentary area was between 34.20 and 37.88 mm/a
and the soil loss rate in eroded areas were slightly higher than that in deposition areas. (2) The stronger carbon source existe in both erosion and sedimentary areas. The modeling fluxes in erosion and sedimentary area of gullies ranged from 18.41 to 28.44 g/(m
2
·a)
and from 22.19 to 29.25 g/(m
2
·a)
respectively. (3) Erosion site
soil bulk density
soil organic carbon content
soil erosion amount
average slope of gully
aboveground biomass and underground biomass of vegetation jointly explained the variability of prediction efficiency of the carbon pool redistribution model (R
2
=0.68)
among which erosion site
erosion amount
organic carbon content
soil bulk density
and below-ground vegetation had strong driving effects on prediction efficiency. (4) The neglected parameter of new input organic carbon pool induced by vegetation should be introduced to correct the carbon pool redistribution model and improve the model prediction efficiency. It was clear that the carbon pool redistribution model had a higher prediction efficiency of CO
2
flux in gully erosion area compared with deposition area. In order to further improve the prediction accuracy of the model
the new organic carbon pool induced by vegetation should be considered as a calibration parameter incorporated in to the carbon pool redistribution model.
Responses of Soil CO2 Emission and Soil Factors to Prescribed Fire in Coastal Shelterbelt
Tracing Fine Sediment Sources in the Surface and Subsurface Rivers of a Karst Watershed Using Compound Fingerprinting with 137Cs and Magnetic Susceptibility in Southwest China
Soil Aggregates and Organic Carbon Distribution Characteristics Based on Long-Term Organic Substitution