annual groundwater recharge

简明释义

地下水年补给量;

英英释义

例句

1.Farmers need to understand annual groundwater recharge (年度地下水补给) to optimize irrigation practices.

农民需要了解年度地下水补给（年度地下水补给）以优化灌溉实践。

2.Rainfall patterns significantly influence the annual groundwater recharge (年度地下水补给) rates.

降雨模式显著影响年度地下水补给（年度地下水补给）率。

3.The local government is investing in projects to enhance annual groundwater recharge (年度地下水补给) in the region.

当地政府正在投资项目，以增强该地区的年度地下水补给（年度地下水补给）。

4.Monitoring annual groundwater recharge (年度地下水补给) helps in sustainable water resource management.

监测年度地下水补给（年度地下水补给）有助于可持续水资源管理。

5.The study focused on the factors affecting annual groundwater recharge (年度地下水补给) in arid regions.

这项研究集中在影响干旱地区的年度地下水补给（年度地下水补给）的因素。

作文

Groundwater is one of the most vital resources for human survival, agriculture, and industry. The process through which water from precipitation and other sources infiltrates into the ground to replenish aquifers is known as annual groundwater recharge. This term refers to the total volume of water that replenishes groundwater supplies over the course of a year. Understanding annual groundwater recharge is essential for sustainable water management, especially in areas where water scarcity is becoming increasingly common due to climate change, urbanization, and over-extraction of water resources.The significance of annual groundwater recharge cannot be overstated. It plays a critical role in maintaining the hydrological balance of ecosystems. Aquifers serve as natural reservoirs that store water for various uses, including drinking water, irrigation, and industrial processes. When the rate of annual groundwater recharge is higher than the rate of extraction, aquifers can sustain their levels, ensuring a continuous supply of fresh water. Conversely, if extraction exceeds recharge, it can lead to depletion of these vital water sources, resulting in adverse environmental and economic impacts.Several factors influence annual groundwater recharge, including rainfall patterns, land use, soil characteristics, and vegetation cover. For instance, regions with heavy rainfall generally experience higher recharge rates compared to arid areas. Additionally, urbanization often leads to increased impervious surfaces, such as roads and buildings, which can reduce the amount of water that infiltrates the ground. Effective land management practices, such as reforestation and the creation of green spaces, can enhance annual groundwater recharge by promoting water infiltration and reducing runoff.Moreover, understanding the seasonal variations in annual groundwater recharge is crucial for water resource planning. In many regions, recharge rates can vary significantly between wet and dry seasons. For example, during the rainy season, the influx of water can lead to a substantial increase in recharge, while in the dry season, the lack of precipitation may cause a decline. Monitoring these fluctuations helps policymakers and water managers develop strategies to optimize groundwater use and ensure long-term sustainability.In conclusion, the concept of annual groundwater recharge is fundamental to understanding groundwater dynamics and managing water resources effectively. As global water demand continues to rise, it is imperative to prioritize the protection and restoration of natural recharge areas, implement sustainable land-use practices, and invest in technologies that enhance recharge. By doing so, we can safeguard this precious resource for future generations, ensuring that both people and ecosystems can thrive. The health of our groundwater supplies depends on our collective efforts to understand and manage annual groundwater recharge wisely.

地下水是人类生存、农业和工业最重要的资源之一。降水和其他来源的水渗入地下以补充含水层的过程被称为年度地下水补给。这个术语指的是在一年内补充地下水供应的总水量。理解年度地下水补给对于可持续水资源管理至关重要，特别是在由于气候变化、城市化和过度开采水资源而日益严重的水资源短缺地区。年度地下水补给的重要性不容小觑。它在维持生态系统的水文平衡中发挥着关键作用。含水层作为自然水库，储存着饮用水、灌溉和工业过程等各种用途的水。当年度地下水补给的速度高于提取速度时，含水层可以维持其水位，确保不断供应新鲜水源。相反，如果提取超过补给，就会导致这些重要水源的枯竭，从而造成不利的环境和经济影响。影响年度地下水补给的因素有很多，包括降雨模式、土地利用、土壤特性和植被覆盖。例如，降雨量较大的地区通常经历更高的补给率，而干旱地区则相对较低。此外，城市化往往导致不透水表面的增加，例如道路和建筑物，这可能减少水渗入地下的数量。有效的土地管理实践，例如重新造林和创建绿地，可以通过促进水的渗透和减少径流来增强年度地下水补给。此外，了解年度地下水补给的季节变化对于水资源规划至关重要。在许多地区，补给率在湿季和干季之间可能会显著变化。例如，在雨季，水的涌入可能导致补给的显著增加，而在干季，降水的缺乏可能导致补给的下降。监测这些波动有助于政策制定者和水资源管理者制定优化地下水使用、确保长期可持续性的策略。总之，年度地下水补给的概念对于理解地下水动态和有效管理水资源至关重要。随着全球水需求的持续上升，必须优先保护和恢复自然补给区，实施可持续的土地利用实践，并投资于增强补给的技术。通过这样做，我们可以为未来几代人保护这一珍贵资源，确保人类和生态系统的繁荣。我们的地下水供应的健康取决于我们共同努力明智地理解和管理年度地下水补给。