在干旱地区的绿洲-沙漠生态基质稳定性的量化值水表
Yong Wang1, Xing Li2, Yong Zhao1
1State Key Laboratory of Water Cycle and Water Security, Beijing, 100038, China; China Institute of Water Resources and Hydropower Research, Beijing, 100038, China; Key Laboratory of Water Safety for Beijing-Tianjin-Hebei Region of Ministry of Water Resources, Beijing, 100038, China.
Journal of environmental management
|September 21, 2025
概括
这项研究定义了干旱绿洲-沙漠生态特征的关键地下水深度,对于管理脆弱的过渡区和防止荒漠化至关重要. 这些发现支持干旱地区的生态区划和可持续土地管理.
科学领域:
- 生态水文学 生态水文学
- 干旱土地的生态环境
- 水文地质学 水文地质学
背景情况:
- 干旱和半干旱的景观具有由地下水驱动的区域模式 (绿洲,生态环境,沙漠).
- 绿洲-沙漠生态基质是重要的过渡区,生态脆弱,对地下水深度敏感.
- 了解水流动力学是管理这些干旱环境的关键.
研究的目的:
- 开发一个水生态框架来分析干旱地区的垂直土壤水流动.
- 量化估计水影响区和关键地下水深度.
- 为干旱地区的生态区划和可持续土地管理提供理论支持.
主要方法:
- 开发了一个水生态概念框架,将瓦多斯区分为水和根区.
- 推导出流水分布曲线和估计的流影响区厚度.
- 提出了在生态边界临界地下水深度的理论表达式,并与现场数据进行了验证.
主要成果:
- 在卢灌区的1.29米处估计的水影响区厚度.
- 已确定的临界地下水深度:内部绿洲-生态界限为46米,外部生态界限-沙漠界限为813米.
- 建立了地下水深度和干旱过渡区结构之间的定量关系.
结论:
- 这项研究为界定和管理绿洲-沙漠生态点提供了理论基础.
- 这些发现对于生态恢复,荒漠化控制和干旱内陆河流域的可持续土地利用至关重要.
- 进一步的研究应该涉及跨区域研究和在生态实践中大规模应用.
相关概念视频
Responses to Drought and Flooding
11.9K
Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
11.9K
Adaptations that Reduce Water Loss
27.9K
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
27.9K
Responses to Salt Stress
14.5K
Salt stress—which can be triggered by high salt concentrations in a plant’s environment—can significantly affect plant growth and crop production by influencing photosynthesis and the absorption of water and nutrients.
14.5K
Tonicity in Plants
32.3K
Plant cells maintain appropriate osmotic balance in extreme conditions. For instance, plants in dry environments store water in vacuoles, limit the opening of their stoma, and have thick, waxy cuticles to prevent unnecessary water loss. Some species of plants that live in salty environments store salt in their roots. As a result, water osmosis occurs in the root from the surrounding soil.
Tonicity
Tonicity describes the capacity of a cell to lose or gain water depending on the solute...
Tonicity
Tonicity describes the capacity of a cell to lose or gain water depending on the solute...
32.3K
Tonicity in Plants
59.6K
Tonicity describes the capacity of a cell to lose or gain water. It depends on the quantity of solute that does not penetrate the membrane. Tonicity delimits the magnitude and direction of osmosis and results in three possible scenarios that alter the volume of a cell: hypertonicity, hypotonicity, and isotonicity. Due to differences in structure and physiology, tonicity of plant cells is different from that of animal cells in some scenarios.
59.6K
Design Example: Analyzing Capacity Contours for Flood Risk Assessment
286
Flood risk assessment involves careful planning and analysis to ensure the safety of communities near water retention structures. Capacity contours are a vital tool in this process, as they illustrate the potential spread of water at specific levels in a given area. In the context of building a bund across a small valley, these contours play a critical role in evaluating the safety of nearby residential areas.In this example, the bund is intended to store stormwater in the valley. The engineers...
286


