Understanding the driving factors (precipitation variation, land use
changes and check dams) and mechanisms behind the changes in sediment
load of a Loess watershed, China
Abstract
Soil and water conservation measures, especially reforestation and check
dam construction, have been progressively implemented on the coarse
sandy hilly catchment region of the Yellow River basin for several
decades, and climate conditions are also dynamic. Therefore, it is very
urgent to understand how the precipitation variation, land use changes
and check dams affect soil erosion and sediment yield in a large
watershed. The sediment delivery distributed (SEDD) model was employed
to quantitatively identify the impacts of the three factors on soil
erosion and sediment yield in the Kuye River watershed. Significant land
use changes, with the conversion of arable land and bare land to
vegetation cover and construction land, occurred in the study watershed
from 1987 to 2016. In addition, 306 key dams were built in the
watershed, with a total storage capacity of 316.64 Mm3, according to the
statistical data of 2011. Hot spot analysis showed that the high-risk
regions for soil erosion and sediment yield were mainly concentrated in
the middle reaches of the watershed. The simulation results showed that
the check dams were the dominant factor, reducing total sediment load by
53.77% in 2006. However, from 1987 to 2016, the contribution of these
three factors (precipitation variation, land use changes and check dams)
to sediment reduction was 29.10%, 40.09% and 30.81%, respectively,
which indicated that all of them had significant influence on sediment
load. The results can serve as a reference for watershed management and
policy implementation.