Abstract

Large subsurface streams on steep slopes have stable positions with distinct catchment areas (drainage basins), linear shapes, and lengths of tens and hundreds meters. They form a closed drainage network with a role and scale similar to the primary hydrographic network and serve as specific hydrological objects—drains. Drains are widespread in the medium-height humid mountain zone, where they account for the formation of a considerable portion of slope runoff. The hydrographic and hydrological characteristics of drains have been examined in small river basins of the Sikhote Alin with the use of field studies, hydrometric measurements, and large-scale topographic surveys.

中文翻译：

---

中高山区洪流的线性结构形式：以锡科特岛为例

摘要

陡坡上的大型地下溪流位置稳定，集水区（流域）不同，呈线性形状，长度为数十米至数百米。它们形成了一个封闭的排水网络，其作用和规模与主要的水文地理网络相似，并且充当特定的水文物体（雨水）。排水在中等高度的潮湿山区中很普遍，在这些地区占斜坡径流的很大一部分。通过实地研究，水文测量和大规模地形调查，对锡克特阿林州小河流域的排水沟的水文和水文特征进行了检查。