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应用生态学报 ›› 2026, Vol. 37 ›› Issue (2): 530-538.doi: 10.13287/j.1001-9332.202602.014

• 研究论文 • 上一篇    下一篇

典型黑土区沟壑密度与小流域沟道网络特征的关系

郭海燕, 张岩*, 李坤衡, 邢慧淼, 李欣梦   

  1. 北京林业大学水土保持学院, 北京 100083
  • 收稿日期:2025-04-03 接受日期:2025-12-27 出版日期:2026-02-18 发布日期:2026-08-18
  • 通讯作者: * E-mail: zhangyan9@bjfu.edu.cn
  • 作者简介:郭海燕, 女, 1999年生, 硕士研究生。主要从事土壤侵蚀与水土保持研究。E-mail: haiyan112599@163.com
  • 基金资助:
    国家重点研发计划项目(2024YFD1501200)

Relationship between gully density and characteristics of watershed channel network in typical black soil region in Northeast China

GUO Haiyan, ZHANG Yan*, LI Kunheng, XING Huimiao, LI Xinmeng   

  1. College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
  • Received:2025-04-03 Accepted:2025-12-27 Online:2026-02-18 Published:2026-08-18

摘要: 在东北典型黑土(土壤亚类)分布区选取64个调查单元,包括完整和区间型小流域各32个,采用高分影像目视解译所有沟道,用Strahler河网分级法对沟道进行分级,计算小流域特征参数、沟壑密度(沟道线密度和面积密度)和沟道网络特征参数,分析沟壑密度与流域特征、沟道网络演化及分维特征的关系,探讨黑土区沟道的活跃程度和发育潜力。结果表明: 调查流域沟道线密度介于0.60~11.45 km·km-2,均值为2.09 km·km-2,35.9%达到中度侵蚀以上;沟道面积密度介于7136~160323 m2·km-2,均值为31752 m2·km-2。小流域沟道最高级别达到8级,1级沟道数量1662条,占比67.8%。网络分维数拟合为良好的线性关系,表明沟道网络存在显著的分形特征。典型黑土分布区的中部和南部支沟发育程度较高,沟道网络复杂程度较高。调查流域均处于沟道发育的幼年期,且处于加速发展阶段。完整型小流域和区间型小流域沟壑密度和沟道网络特征都无显著差异。沟道线密度与流域平均坡度、形状系数、沟道最大级别和网络分维数都呈显著相关,但与调查单元面积无显著相关性。本研究结果有助于明确典型黑土分布区沟壑密度的空间变化和发育潜力,为黑土区沟蚀调查和防治提供理论依据。

关键词: 黑土区, 沟蚀, 沟谷网络, 分维数, 河网分级法

Abstract: We selected sixty-four survey units in the typical black soil (soil sub-class) distribution area of Northeast China, including 32 complete small watersheds and 32 non-closure small watersheds. All gullies were identified through high-resolution image visual interpretation. The Strahler stream order method was used to classify the gullies. We calculated the parameters such as small watershed characteristics, gully density (line and area density of gullies), and gully network characteristics. By analyzing the relationship between gully density and watershed characteristics, gully network evolution, and fractal dimensions, we explored the activity level and developmental potential of gullies in the black soil region. The results showed the line density of gullies in the surveyed watersheds ranged from 0.60 to 11.45 km·km-2, with an average of 2.09 km·km-2, and 35.9% exceeded moderate erosion levels. The area density of gullies ranged from 7136 to 160323 m2·km-2, with an average of 31752 m2·km-2. The highest gully order in small watersheds reached level 8, with 1662 first-order gullies accounting for 67.8%. The fractal dimension fitting curve of the network exhibited linear patterns, indicating significant fractal characteristics in the gully network. The tributary development was higher in the central and southern parts of the typical black soil distribution area, with greater complexity in the gully network. All surveyed watersheds were in the juvenile stage of gully development and were in an accelerated growth phase. There were no significant differences in gully density and gully network characteristics between the two types of small watersheds. Gully line density showed significant correlations with average watershed slope, shape coefficient, maximum gully order, and network fractal dimension, but no significant correlation with survey unit area. These findings would help clarify the spatial variation and deve-lopmental potential of gully density, providing a theoretical basis for gully erosion investigation and prevention in black soil regions.

Key words: black soil region, gully erosion, channel network, fractal dimension, Strahler stream order method