aquifer water influx

简明释义

1. 水伐进水量; 2. 边水侵入;

英英释义

Aquifer water influx refers to the movement of water from an aquifer into a surface water body, such as a river or lake, or into another geological formation.

含水层水流入是指水从含水层流向地表水体,如河流或湖泊,或流入另一个地质构造的过程。

例句

1.The research indicated that increased aquifer water influx can improve groundwater quality.

研究表明,增加的含水层水流入可以改善地下水质量。

2.Monitoring aquifer water influx is crucial for sustainable water management.

监测含水层水流入对可持续水资源管理至关重要。

3.The study focused on the effects of aquifer water influx on local ecosystems.

这项研究集中于含水层水流入对当地生态系统的影响。

4.Farmers in the region rely heavily on aquifer water influx for irrigation.

该地区的农民在灌溉方面严重依赖含水层水流入

5.Local authorities are concerned about the impact of urban development on aquifer water influx.

当地政府担心城市发展对含水层水流入的影响。

作文

The study of water resources has become increasingly important in the face of climate change and population growth. One critical aspect of this study is understanding the dynamics of groundwater systems, particularly the role of aquifers. An aquifer is a geological formation that can store and transmit water, and it plays a vital role in supplying freshwater to various ecosystems and human activities. One significant process associated with aquifers is the aquifer water influx, which refers to the movement of water into an aquifer from surrounding areas or from precipitation. This process is essential for maintaining the water balance within the aquifer system.Aquifers are often recharged by rainfall, where water seeps through the soil and rock layers, replenishing the groundwater supply. The aquifer water influx not only helps sustain the water levels within the aquifer but also supports the surrounding ecosystems that depend on this water source. For instance, wetlands, rivers, and lakes often rely on the steady flow of groundwater to maintain their health and biodiversity.In many regions, especially arid and semi-arid areas, the aquifer water influx is crucial for agricultural practices. Farmers depend on groundwater for irrigation, and understanding how much water is entering the aquifer helps them manage their water usage effectively. If the influx is insufficient due to prolonged droughts or over-extraction, it can lead to a depletion of the aquifer, resulting in negative consequences for both agriculture and the environment.Moreover, human activities can significantly impact the aquifer water influx. Urbanization, industrialization, and land use changes can alter the natural recharge processes. For example, impervious surfaces such as roads and buildings prevent rainwater from infiltrating the ground, thus reducing the amount of water that can replenish the aquifer. Additionally, pollution from agricultural runoff or industrial discharges can contaminate the groundwater, making it unsafe for consumption and harming aquatic ecosystems.To address these challenges, sustainable water management practices are essential. Monitoring the aquifer water influx and implementing strategies to enhance recharge can help ensure that aquifers remain a viable source of water for future generations. This might include creating green spaces in urban areas to promote infiltration, using rainwater harvesting systems, and protecting natural landscapes that facilitate groundwater recharge.In conclusion, the concept of aquifer water influx is fundamental to understanding groundwater systems and their importance in our ecosystem. As we face increasing pressure on our water resources, recognizing the significance of aquifer recharge will be crucial for sustainable management. By taking steps to protect and enhance the aquifer water influx, we can ensure that these vital water sources continue to support both human and ecological needs for years to come.

水资源的研究在气候变化和人口增长面前变得越来越重要。这个研究的一个关键方面是理解地下水系统的动态,尤其是含水层的作用。含水层是能够储存和传输水的地质构造,它在为各种生态系统和人类活动提供淡水方面发挥着至关重要的作用。与含水层相关的一个重要过程是含水层水流入,它指的是水从周围地区或降水中流入含水层的过程。这个过程对于维持含水层系统内的水量平衡至关重要。含水层通常通过降雨进行补给,水分渗透通过土壤和岩石层,为地下水供应补充。含水层水流入不仅有助于维持含水层内的水位,还支持依赖这一水源的周围生态系统。例如,湿地、河流和湖泊通常依靠地下水的稳定流动来维持其健康和生物多样性。在许多地区,尤其是干旱和半干旱地区,含水层水流入对农业实践至关重要。农民依赖地下水进行灌溉,了解进入含水层的水量有助于他们有效管理水资源。如果由于长期干旱或过度开采,流入不足,可能导致含水层的枯竭,从而对农业和环境产生负面影响。此外,人类活动可以显著影响含水层水流入。城市化、工业化和土地利用变化可以改变自然补给过程。例如,像道路和建筑物这样的不透水表面会阻止雨水渗透到地下,从而减少能够补充含水层的水量。此外,农业径流或工业排放的污染可能会污染地下水,使其不适合饮用并危害水生生态系统。为了解决这些挑战,实施可持续水资源管理实践至关重要。监测含水层水流入并实施增强补给的策略可以帮助确保含水层继续作为未来水源的可行选择。这可能包括在城市地区创建绿色空间以促进渗透、使用雨水收集系统以及保护促进地下水补给的自然景观。总之,含水层水流入的概念对于理解地下水系统及其在我们生态系统中的重要性至关重要。随着我们面临对水资源的日益压力,认识到含水层补给的重要性将对可持续管理至关重要。通过采取措施保护和增强含水层水流入,我们可以确保这些重要的水源在未来几年继续支持人类和生态的需求。

相关单词

influx

influx详解:怎么读、什么意思、用法