相关实验视频
Updated: Jul 15, 2025

06:37
Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
Published on: November 13, 2017
9.3K
在中国西南地区的卡斯特地下河流盆地的水文地质运行
Yongli Guo1,2, Fen Huang1,2, Ping'an Sun1,2
1Key Laboratory of Karst Dynamics, MNR and GZAR, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, 541004, China.
Ground water
|September 30, 2023
概括
这项研究揭示了化和降水如何影响中国西南部的地下水流. 了解这些动态对于管理这个重要的水资源至关重要.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 地质化学 地质化学
背景情况:
- 毛孔地下河系统是中国西南部的一个重要地下水源.
- 了解其水文地质结构和流动动力学对于水资源管理至关重要.
研究的目的:
- 评估Maocun地下河系统的水文地质结构和流动动态.
- 为了研究石岩化和降水对地下水流动模式和响应时间的影响.
主要方法:
- 采用了多度追踪器和高分辨率水位监测技术.
- 分析了环境标志物 (EC, δ13CDIC, 222Rn, δ18O) 和它们之间的关系.
- 根据降水场景开发了三种水文地质概念模型.
主要成果:
- 在空间地质结构中观察到高度的异质性.
- 卡斯特化从扩散水增加到管道流动模式.
- 降水量和频率显著影响了子系统响应时间,平均时间从4.08小时到16.42小时不等.
结论:
- 建立了三个不同的水文地质概念模型,将降水水平与地下水流动模式 (缩,混合,扩散) 相关联.
- 卡斯特化程度和空间结构是控制地下水流动动态和响应时间的关键因素.
- 这些发现为卡斯特环境中的可持续地下水管理提供了关键的见解.
相关概念视频
Regulation of Water Output
324
The human body predominantly expels water through the urinary system. On average, an individual generates around 1.5 liters of urine each day. This amount can fluctuate based on how well a person is hydrated, but a critical minimum quantity of urine must be produced to ensure the body's proper functioning. Daily, the kidneys remove 600 to 1200 milliosmoles of dissolved substances, effectively excreting excess minerals and water-soluble toxins such as creatinine, urea, and uric acid from the...
324
Design Example: Design of an Irrigation Channel
124
Trapezoidal channels are widely used in irrigation systems due to their cost-effectiveness and efficiency in conveying water. Trapezoidal channels feature a flat bottom and sloping sides, making them stable and easier to construct compared to other shapes. The bottom width and side slope ratio are determined based on the required flow capacity and site conditions. The side slope is kept gentle for unlined channels to prevent soil erosion.Hydraulic parameters in channel design include the flow...
124
Regulation of Water Intake
545
Osmolality refers to the number of solute particles per kilogram of solvent in a solution. Plasma osmolality specifically indicates the total number of solute particles per kilogram of water in blood plasma. This value reflects the body's hydration status and is tightly regulated through mechanisms controlling water intake and output. While water consumption is a conscious decision, the body has intrinsic regulatory systems to maintain fluid balance. Dehydration, a state of water deficit...
545
Energy Considerations in Open Channel Flow
110
Open channel flow, where a fluid flows with a free surface exposed to the atmosphere, is primarily governed by gravitational and surface effects, distinguishing it from closed conduit or pipe flow. In open channels such as rivers, canals, and artificial channels, energy analysis provides valuable insights into flow behavior and the relationship between depth, velocity, and slope.Specific Energy and Flow DepthIn open channel flow, the specific energy, E, combines the gravitational potential...
110
Underflow Gates
75
Underflow gates are vital for controlling water flow in irrigation canals. The three main types of underflow gates — vertical, radial, and drum gates — serve different purposes while ensuring effective flow management. Vertical gates move up and down, generating a free-flowing water jet; radial gates pivot to regulate the flow; and drum gates rotate for precise adjustments. The flow through these gates is influenced by downstream conditions, resulting in free or drowned outflow.Free and...
75
Gradually Varying Flow
81
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
81

