根据土壤颗粒大小的变化,霍坦河床透率和漏水量从上游到下游的变化
Shuo Wang1,2, Jianghui Zhang3,4, Zheng Fang5
1College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi, 832000, China.
Scientific reports
|March 27, 2025
概括
这项研究量化了霍坦河的河床透情况,揭示了上游透率更高的情况. 调查结果为该地区的可持续水资源管理和生态保护提供了关键数据.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 沉积物学的沉积物学
背景情况:
- 严重的漏对可持续的水资源管理构成重大挑战.
- 在霍坦河流域缺乏泄漏数据,阻碍了有效的资源管理.
研究的目的:
- 为了评估霍坦河床的水透率.
- 评估四种常见的透模型的性能.
- 分析沉积物特性及其与透的关系.
主要方法:
- 使用双环方法来测量水透率.
- 评估了四种透模型 (科斯蒂亚科夫,菲利普,格林-安普特,霍顿).
- 分析了沉积物样本的纹理和碎形尺寸.
主要成果:
- 透率在上游河段最高,向岸边下降.
- 漏量和每单位河长的漏率从上游到下游下降.
- 沉积物碎片尺寸与沙子含量正相关,与粘土和泥含量负相关.
结论:
- 在测试的模型中,科斯蒂亚科夫方程表现出卓越的准确性和适用性.
- 结果为霍坦河流域的水资源管理和生态保护提供了必要的数据.
- 了解透模式和沉积物特征对于解决漏挑战至关重要.
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