APPLICATION OF~(137)Cs AS TRACING METHOD TO STUDY SOIL EROSION ON SLOPING LANDS IN THE HILLY RED SOIL AREA ——A CASE STUDY IN FENGCHENG CITY, JIANGXI PROVINVE
PU Li-jie, Zhao Yao-yang
Abstract
PU Li-jie, Zhao Yao-yang
Abstract
Soil erosion is a severe problem in sloping land of hilly red area. Based on (~(137)Cs) tracing technique and by some soil erosion estimating models, the soil erosion rate on the representative sloping lands of Fengcheng City, Jiangxi Province was studied. The results showed that the reference inventory of~(137)Cs in the study area without soil erosion or man -disturbing is 1 992.45±145.63 Bq/m~2 . The annual soil erosion occurring on different parts of slope is evidentily different, with its rate increasing in the order form top of slope, middle of slope and to bottom of slope. Under different land use types, the average soil erosion rates are also different, which decreases in the order from, cultivated sloping land, multi-slope of conversion from farmland for 30 a and 1 a, slope of conversion from farmland for 30 a and barren slope. This result is benefitial for making relative land use, water and soil conservation policy for the ongoing national reducing cultivated land to forestland and grassland project in the study area.
OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Soil erosion is a severe problem in sloping land of hilly red area. Based on (~(137)Cs) tracing technique and by some soil erosion estimating models, the soil erosion rate on the representative sloping lands of Fengcheng City, Jiangxi Province was studied. The results showed that the reference inventory of~(137)Cs in the study area without soil erosion or man -disturbing is 1 992.45±145.63 Bq/m~2 . The annual soil erosion occurring on different parts of slope is evidentily different, with its rate increasing in the order form top of slope, middle of slope and to bottom of slope. Under different land use types, the average soil erosion rates are also different, which decreases in the order from, cultivated sloping land, multi-slope of conversion from farmland for 30 a and 1 a, slope of conversion from farmland for 30 a and barren slope. This result is benefitial for making relative land use, water and soil conservation policy for the ongoing national reducing cultivated land to forestland and grassland project in the study area.
Key concepts: Erosion, Environmental science, Soil conservation, Hydrology (agriculture), Red soil, Grassland, Soil science, Geology