基于三维 EBK 模型的采煤扰动对西北地区土壤含水量时空分布的影响

IF 3.2 3区 地球科学 Q1 Environmental Science
Kai Zhang, Mengyuan Chen, Shaokai Feng, Xiangyu Chen, Zhao Yan
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引用次数: 0

摘要

西北地区既是重要的储煤基地,又是生态脆弱区,土壤含水量是制约西北地区生态发展的关键因素。揭示采煤扰动下矿区土壤含水量时空分布变化特征及其影响机制,对保护矿区水资源至关重要。本研究对神东煤炭集团西部某典型采煤沉陷区采后 1 年的土壤含水量(0-1000 cm 深)进行了原位监测,并结合经典统计、二维普通克里金和三维经验贝叶斯克里金空间插值等方法,对土壤含水量的绝对值、变异性和空间分布进行了时序分析。结果表明,浅层 SWC(0 ~ 60 cm)呈水平带状分布,沿西北向东南方向逐渐增大;随着采煤时间的延长,SWC 的绝对值下降了 0.81% ~ 33.58%,变异系数先减小后增大,变异范围为 2.19% ~ 34.49%。深层 SWC(100 ~ 1000 cm)呈垂直分层,并随土壤深度增加而增加,浅层和深层土壤水分在采煤影响下逐渐向中层迁移。此外,本文通过三维 EBK 模型准确刻画了土壤含水量的三维时空分布,进一步揭示了采煤对土壤含水量的影响机理。该研究可为预测和评价采矿活动对水循环的潜在影响提供技术和数据支持,有助于矿区制定水资源管理和保护政策。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Effects of coal mining disturbance on spatial and temporal distribution of soil water content in Northwest China-based on 3D EBK model

Effects of coal mining disturbance on spatial and temporal distribution of soil water content in Northwest China-based on 3D EBK model

Northwest China is both an important coal storage base and an ecologically fragile area, and soil water content (SWC) is a key factor limiting the ecological development of Northwest China. Revealing the characteristics of spatial and temporal distribution changes of soil water content in mining areas under coal mining disturbance and the influencing mechanism is crucial for the protection of water resources in mining areas. In this study, the soil water content (depth 0–1000 cm) of a typical coal mine subsidence area in the western part of Shendong Coal Group was monitored in situ for 1 year after mining, and the absolute value, variability, and spatial distribution of soil water content were temporally analysed by combining classical statistics, 2D Ordinary Kriging and 3D Empirical Bayesian kriging spatial interpolation. sequence analysis. The results showed that the shallow SWC (0 ~ 60 cm) was distributed horizontally in bands, and gradually increased along the direction from northwest to southeast; with the increase of coal mining time, the absolute value of SWC decreased by 0.81% ~ 33.58%, and the coefficient of variation decreased and then increased, with the range of variation from 2.19% ~ 34.49%. The deep SWC (100 ~ 1000 cm) was stratified vertically and increased with soil depth, and the shallow and deeper soil moisture would gradually migrate to the middle layer under the influence of coal mining. In addition, this paper accurately portrays the three-dimensional spatial and temporal distribution of soil water content by the 3D EBK model, which further reveals the mechanism of coal mining's influence on soil water content. This study can provide technical and data support for predicting and evaluating the potential impacts of mining activities on the water cycle, and help mining areas to formulate policies for managing and protecting water resources.

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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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