4.7 Article

Temporal variations in soil erodibility indicators of vegetation-restored steep gully slopes on the Loess Plateau of China

Journal

AGRICULTURE ECOSYSTEMS & ENVIRONMENT
Volume 286, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.agee.2019.106661

Keywords

Soil erodibility indicator; Near soil-surface characteristics; Vegetation growth; Temporal variability; Chinese Loess Plateau

Funding

  1. National Key Research and Development Program of China [2017YFC0504702]
  2. State Key Program of National Natural Science of China [41530858]

Ask authors/readers for more resources

Near soil-surface characteristics change considerably with vegetation growth during one growing season, and thus likely induce the temporal variations in soil erodibility indicators. This study was performed to investigate the temporal variations in soil erodibility indicators under different vegetation-restored gully slope lands on the Loess Plateau of China. Soil erodibility indicators included the K factor, mean weight diameter (MWD), mean number of drop impacts (MND), saturated conductivity (K-s), cohesion (Coh), penetration resistance (PR), and one comprehensive soil erodibility index (CSEI). One slope cropland (as the control) and seven vegetation-restored gully slope lands were selected to measure soil erodibility indicators for seven times from April 23 to October 10, 2018. Near soil-surface characteristics were also measured to explain the temporal variations in soil erodibility indicators. The results showed that the temporal variations in soil erodibility indicators of different vegetation lands were similar. The K factor fluctuated considerably, while the MWD, MND, K-s, Coh, and PR gradually increased over time. However, all erodibility indicators of the control cropland fluctuated over time with no distinctive trend. The CSEI of all sites fluctuated significantly over time. Compared to the control cropland, the mean K factors of different vegetation lands decreased by 2%-24%, but the mean values of MWD, MND, K-s, Coh, and PR increased by 108%-217%, 152%-343%, 94%-306%, 73%-175%, and 30%-199%, respectively. Consequently, the mean CSEI of different vegetation lands was reduced by 41% to 86%. The temporal variations in soil erodibility indicators were closely related to the seasonal changes in root mass density. Bothriochloa ischaemum (Linn.) Keng was considered the most effective restoration community to reduce soil erodibility of steep gully slope lands. The results contribute to improving the eco-environment on the Chinese Loess Plateau.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available