您好，欢迎访问中国农业科学院 机构知识库！

全部

  • 全部
  • 标题
  • 学者
  • 机构
  • 关键词

Effects of lithology and soil horizons on gully morphology in the Mollisol region of China

文献类型： 外文期刊

作者： Wen, Yanru 1 ; Kasielke, Till 2 ; Jiang, Heng 3 ; Zepp, Harald 2 ; Zhang, Bin 4 ;

作者机构： 1.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, State Key Lab Efficient Utilizat Arid & Semiarid A, Beijing 100081, Peoples R China

2.Ruhr Univ Bochum, Inst Geog, Univ Str 150, D-44780 Bochum, Germany

3.Guangdong Acad Sci, Inst Ecoenvironm & Soil Sci, Natl Reg Joint Engn Res Ctr Soil Pollut Control &, Guangdong Key Lab Integrated Agroenvironm Pollut C, Guangzhou 510650, Peoples R China

4.Nanjing Agr Univ, Coll Resources & Environm Sci, Nanjing 210095, Peoples R China

关键词： Gully erosion; Soil horizons; Lithology; Cross-section; Gully morphology

期刊名称：GEODERMA （ 影响因子：6.1； 五年影响因子：7.0 ）

ISSN： 0016-7061

年卷期： 2024 年 446 卷

页码：

收录情况： SCI

摘要： Gully erosion is the most destructive form of land degradation in NE China and many other regions around the globe. It is generally accepted that lithology and topography have an important impact on gully morphology. However, the effects of lithology and slope gradient on gully cross-sectional morphology remain unclear. This study aims to elucidate how the sequence of soil horizons and rock strata influence gully cross-sectional morphology in the Mollisol region of NE China. We measured the gully cross-sectional morphology by a combination of differential GPS, laser range finder, and ruler. Profile samples were collected by core drilling with depths from 1 m to 4 m at 39 sites along the gully thalweg and cross-sections. The physical and geo-chemical properties of 5 cm sub-samples were measured. The sequence of soil horizon and lithology in our study area was as follows (with increasing depth): (1) mollic epipedon (black soil horizon) and (2) subsoil developed in loess, (3) fine to coarse sands, (4) alternating layers of sand and shale debris, and (5) homogeneous shale. We found that the combined effect of soil horizons, lithology, and longitudinal slope gradient of the gully bottom determines gully cross-sectional morphology, which contrasts to simplified generalizations for homogeneous underground material. U-shaped gullies were related to the mollic epipedon, or cohesive sandy loess and fine sands, with an average gentle gully bottom gradient of < 10 degrees. V-shaped gullies were either developed with cohesionless shale, and unconsolidated sediments even at a relatively gentle gradient of < 10 degrees, or cohesive materials at steep gradients ranging from 16 degrees to 27 degrees. Overall, a detailed understanding of underground materials and their proper management are extremely urgent on steep gully slopes, especially in arable land that experienced severe gully erosion. Generalized models of the sequence of gully forms need to be differentiated prior to taking effective countermeasures.

  • 相关文献
作者其他论文 更多>>
置顶
购物车
反馈

© 京ICP备09089781号-29 主办单位：中国农业科学院

学术资源： 中国农业科学院 农业专业知识服务系统 农科联盟资源共建共享平台 中国农业科技文献与信息服务平台 中国农业期刊集成服务平台