4.7 Article

Morphological characteristics and influencing factors of permanent gully and its contribution to regional soil loss based on a field investigation of 393 km2 in Mollisols region of northeast China

期刊

CATENA
卷 217, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2022.106467

关键词

Gully morphology; Land use; Gully erosion intensity; Mollisols; Northeast China

资金

  1. National Key Research and Devel-opment Program of China [2021YFD1500800]
  2. National Natural Science Foundation of China [42107356]
  3. China Postdoctoral Sci-ence Foundation [2021T140663, 2020M681062]
  4. Hei-longjiang Provincial Natural Science Foundation of China [YQ2021C036]

向作者/读者索取更多资源

This study aims to clarify the morphology and factors influencing gully erosion in the Mollisols region of northeast China. The study found that gullies of different types have distinct morphologies and their density and ground lacerative degree vary with slope gradient and length. Gully erosion has significant effects on soil loss in the region, highlighting the urgent need for erosion control measures.
Gully erosion, one of the most damaging forms of land degradation, destroys farmlands and threatens grain and ecological stability. Approximately 295,000 gullies have formed in the Mollisols region of northeast China (NEC), while the actual severity of gully erosion remains unclear. This study aims to clarify gully morphology, factors influencing gully morphology, and contribution of gully erosion to soil loss through a 393 km(2) field investigation in a typical and representative Mollisols region of NEC. There were 1048 gullies observed, with an average length, top width, depth and width-depth ratio of 522.32 m, 15.05 m, 2.77 m and 7.16, respectively. Over 70% of gullies had a length, top width and depth of 100-500 m, 3-20 m and 0.5-3 m, respectively. The three types of gullies, classified based on where the gully head developed (GF, farmland; GR, unpaved road; GW, woodland), had significantly distinct morphologies, with GW being broader and deeper and GF being longer. Notably, 56.2% of gullies are GF, accounted for 74.84% of the total gully area and 67.04% of the total gully volume (V). V of GF, GR and GW could be well explained by a power function of gully area (A). Gully density (gully length per unit area, GD, km km(-2)) and ground lacerative degree (gully area per unit area, GLD, km km-2) increased with slope gradient, and first increased and then decreased with slope length. Gully development was more favorable of sunny slope and a larger angle between gully and ridge orientation. The annual eroded soil from the gully was 1.86 times of that from the hillslope across the region during 2013-2018, contributing 65% of region eroded soil. This clearly identifies the severity of gully erosion and substantiates gully erosion risks to valuable mollisols and therefore food security. An urgent need exists to implement gully erosion control practices in this area.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据