龛沟是崩岗早期发育的形态标志

高钰淏; 陈家宙; 邹自强; 刘子轩; 李文凯; 杨雪

doi:10.13870/j.cnki.stbcxb.2022.04.014

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龛沟是崩岗早期发育的形态标志

更新时间：2025-03-12

- 龛沟是崩岗早期发育的形态标志
- Niche-like Ephemeral Gully is A Morphological Symbol of the Early Development of Benggang
- 水土保持学报 2022年36卷第4期页码：105-111
- 作者机构：
  
  1. 华中农业大学资源与环境学院,武汉,430070
  2. 湖北省水利水电规划勘测设计院,武汉,430070
- 作者简介：
  
  [ "高钰淏(1994—),男,博士研究生,主要从事水土保持与坡面土壤侵蚀研究。E-mail:gyh@webmail.hzau.edu.cn" ]
- 基金信息：
  
  国家自然科学基金项目（42177307）
- DOI：10.13870/j.cnki.stbcxb.2022.04.014
  中图分类号： S157.1
- 纸质出版：2022
- 稿件说明：
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高钰淏, 陈家宙, 邹自强, 等. 龛沟是崩岗早期发育的形态标志[J]. 水土保持学报, 2022,36(4):105-111.

GAO Yuhao, CHEN Jiazhou, ZOU Ziqiang, et al. Niche-like Ephemeral Gully is A Morphological Symbol of the Early Development of Benggang[J]. 2022, 36(4): 105-111.
高钰淏, 陈家宙, 邹自强, 等. 龛沟是崩岗早期发育的形态标志[J]. 水土保持学报, 2022,36(4):105-111. DOI： 10.13870/j.cnki.stbcxb.2022.04.014.

GAO Yuhao, CHEN Jiazhou, ZOU Ziqiang, et al. Niche-like Ephemeral Gully is A Morphological Symbol of the Early Development of Benggang[J]. 2022, 36(4): 105-111. DOI： 10.13870/j.cnki.stbcxb.2022.04.014.

摘要

为探究我国南方花岗岩红壤地区崩岗的起始标志和发育阶段。在湖北省通城县和广西岑溪市2个典型崩岗区调查崩岗的发育过程。结果表明，2个调查区都存在一种细沟发育而来的龛状浅沟，将其命名为龛沟。龛沟具有3个特征：上游有明显细沟，沟壁陡峭且具有上窄下宽的宽深梯形形态。龛沟主要发生在砂土层裸露、具有一定汇水面积和局地坡度>30°的裸露坡面。龛沟是一种特殊形态的浅沟，其定义、形态和侵蚀营力都不同于常规浅沟、切沟和Amphitheatershaped canyons等沟蚀地貌。龛沟是沟道侵蚀从水力侵蚀为主变为水力和重力复合侵蚀的过程，是崩岗起始发育的启动标志，其发生原因与花岗岩红壤上红（黏）下砂的土层结构有关。以龛沟出现为标志，将崩岗的发育阶段重新划分为早期准备阶段、初期启动阶段、中期发展阶段和后期成熟阶段。龛沟的特点和研究区的崩岗治理效果表明，削坡开级的治理方式不适合在红土层较薄的花岗岩红壤地区使用。龛沟的发现将推进对崩岗早期发育的研究，并为崩岗的预防和治理提供新的理论依据。

Abstract

In order to explore the initial sign and development stage of Benggang in granite red soil area in South China

field investigations were conducted in two typical Benggang areas in Tongcheng

Hubei and Cenxi

Guangxi to investigated the development process of Benggang. The results showed that there was a special niche shaped ephemeral gully developed from a rill in both survey areas

named niche-like ephemeral gully (NEG). The morphology of the NEG had the following characteristics:a distinct rill in the upstream

steep banks

a narrow upper bank and a wide

deep gully bed. The NEG was formed on slopes without plant cover where sandy soil layers were exposed

with a small contribute area and a slope steeper than 30°. The NEG was a special morphological ephemeral gully

its definition

morphology

erosion forces were different from the ephemeral gully

permanent gully

Amphitheater shaped canyons and so on. The NEG was the process of gully erosion changed from being dominated by hydraulic erosion to being highly coupled by hydraulic and gravity erosion. The NEG is the launching marker for the Benggang. The formation of the NEG is related to the soil configuration of granitic red soil with upper red clay and lower sandy soil layers. Taking the emergence of NEG as a sign

the development stage of Benggang is re-classified into the early preparation stage

initial launching stage

middle development stage and late maturation stage. The characteristics of the NEG and the management effect of the study area show that the terrace is not suitable for the area with a thin red soil layer. The discovery of the NEG will promote the study of the early development of Benggang and provide a new theoretical basis for the prevention and management of the Benggang.

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