Accordingly, flat lands have developed behind the check dams due to sediment deposition and some of these flat lands are now being cultivated. The crops in the cultivated lands include maize, corns, beans, potato, sunflower, and millet. 84.1% of the croplands have slope gradients greater than 10° (or www.selleckchem.com/products/Cyclopamine.html 15% in steepness), and 56.9% of the watershed area has

slope gradients greater than 25° (or 46.8% in steepness) (Fig. 2). Therefore, more than half of the croplands are beyond the range of slope gradients, 3–18%, of the erosion plots that were used to develop USLE/RUSLE, which necessitates to test the validity of the slope equations used in USLE/RUSLE. To investigate erosion from sloping lands and to evaluate the effectiveness of various soil conservation measures in reducing soil erosion, runoff and soil loss from three sets of erosion plots were measured under natural rainfall in three periods. The first set, short slope plots (SSP), were laid out with a dimension of 2 m in width and 7 m in length at slope angles of 5°, 10°, 15°, 20°, 25°, and 30° (Fig. 3). All the plots were tilled bare soil. The plots were monitored in 7 years out of the period from 1985 to 2003. Storm flows from each plot were collected by an underground brick-built

pool. After each runoff-generating rainfall event, storm water in the pool was first thoroughly stirred and three water samples were then taken from the pool to determine the average sediment concentration for that event in the lab. The total flow discharge for each event was calculated ABT-888 research buy by measuring the volume of storm water in the pool. Flow discharge and sediment concentrations were eventually used to determine the total soil loss not for each event. The second set, long slope plots (LSP), were laid out with a slope length of 20 m and a width ranging from 3 m to 10 m at the same slope angles as the first set of plots (5°, 10°, 15°, 20°, 25°, and 30°). Runoff and soil loss from LSP were measured under natural rainfall by SISWC over 5 years (1957, 1958, 1964, 1965 and 1966). The third set, including five soil conservation plots (SCP) and one cultivated cropland plot,

was also established by SISWC and the characteristics of those plots are summarized in Table 1. The five soil conservation measures are woodland, grasses, alfalfa, contour earth banks, and terraces. Soil and water loss from those plots were monitored by SISWC over a various length of time (6–12 years) out of 1957–1968 (Table 1). The monitoring equipment and sampling methods for the second and third sets of plots are described in detail elsewhere (SISWC, 1982 and Zhu, 2013). All the soil and water loss data collected from the second and third set of plots were compiled by SISWC (SISWC, 1982). The mean annual rainfall over the 17-year of three study periods was 547.4 mm, ranging from 243.3 mm in 1965 and 756.3 mm in 1964. This was about 10% higher than the long-term mean annual precipitation, 496.7 mm, recorded by SISWC.