artesian water yielding formation

简明释义

1. 自流含水层; 2. 自流出水层; 3. 承压含水层; 4. 承压出水层;

英英释义

例句

1.The city plans to protect its artesian water yielding formation from pollution to ensure clean drinking water.

该市计划保护其自流水出水层免受污染，以确保饮用水的清洁。

2.Farmers rely on the artesian water yielding formation to irrigate their crops during dry seasons.

农民依赖自流水出水层在干旱季节灌溉作物。

3.Geologists study the artesian water yielding formation to understand groundwater movement in the area.

地质学家研究自流水出水层以了解该地区的地下水运动。

4.The region is known for its abundant artesian water yielding formation, which provides a reliable source of fresh water.

该地区以其丰富的自流水出水层而闻名，提供了可靠的淡水来源。

5.Drilling into an artesian water yielding formation can provide water at high pressure without the need for pumping.

钻探到自流水出水层可以在不需要抽水的情况下提供高压水源。

作文

The concept of an artesian water yielding formation is crucial in understanding groundwater systems and their significance in our daily lives. An artesian water yielding formation refers to a geological layer that is capable of producing water under pressure, allowing it to flow naturally to the surface without the need for pumping. This phenomenon occurs when water is trapped between impermeable layers of rock or sediment, creating a pressurized aquifer. When a well is drilled into this formation, the water often rises to the surface due to the pressure, which can be a sustainable source of fresh water for various uses.Understanding the mechanics behind an artesian water yielding formation requires knowledge of geology and hydrology. The formation typically consists of permeable rock or sediment, such as sandstone or limestone, which allows water to flow through it. The impermeable layers above and below the aquifer act as barriers, preventing the water from escaping and maintaining the pressure needed for artesian flow. This unique setup highlights the importance of geological formations in the hydrological cycle and emphasizes the need for responsible water management practices.The benefits of utilizing an artesian water yielding formation are numerous. For one, it provides a reliable source of water for agricultural, industrial, and domestic use, especially in regions where surface water is scarce. Additionally, the water from these formations is often of high quality, as it has been naturally filtered through layers of rock and sediment. This makes it suitable for drinking, irrigation, and other applications without extensive treatment.However, the extraction of water from an artesian water yielding formation must be managed carefully to prevent over-extraction, which can lead to a decline in water levels and potential environmental consequences. Over time, excessive pumping may result in the depletion of the aquifer, causing the pressure to drop and disrupting the natural flow of water. This can lead to land subsidence, reduced water quality, and negative impacts on local ecosystems.To ensure the sustainability of artesian water yielding formations, it is essential to implement effective water management strategies. This includes monitoring water levels, regulating the amount of water extracted, and promoting conservation practices among users. Public awareness campaigns can also play a vital role in educating communities about the importance of these formations and the need to protect them.In conclusion, the artesian water yielding formation is a vital component of our groundwater resources, providing valuable water supplies for various purposes. By understanding its characteristics and implementing sustainable management practices, we can ensure that these natural systems continue to benefit future generations. As we face increasing challenges related to water scarcity and climate change, recognizing the significance of artesian water yielding formations will be key to developing resilient water resource strategies that support both human needs and environmental health.

“自流井水产出层”的概念在理解地下水系统及其在我们日常生活中的重要性方面至关重要。“自流井水产出层”指的是一种地质层，能够在压力下产生水，允许水自然流向地表，而无需抽水。这种现象发生在水被困在不透水的岩石或沉积物之间，从而形成一个加压的含水层。当在这个层中钻井时，水通常会因压力而上升到地表，这可以成为各种用途的可持续淡水来源。理解“自流井水产出层”的机制需要对地质学和水文学有一定的了解。该层通常由可渗透的岩石或沉积物组成，例如砂岩或石灰岩，允许水通过。位于含水层上下方的不透水层作为屏障，防止水逃逸，并维持自流所需的压力。这种独特的设置突显了地质构造在水文循环中的重要性，并强调了负责任的水资源管理实践的必要性。利用“自流井水产出层”的好处是众多的。首先，它为农业、工业和家庭使用提供了可靠的水源，尤其是在地表水稀缺的地区。此外，这些层中的水通常质量较高，因为它经过岩石和沉积物的自然过滤。这使得它在未经广泛处理的情况下适合饮用、灌溉和其他应用。然而，从“自流井水产出层”中提取水必须谨慎管理，以防止过度提取，这可能导致水位下降和潜在的环境后果。随着时间的推移，过量抽水可能导致含水层的枯竭，造成压力下降，扰乱水的自然流动。这可能导致土地沉降、水质下降以及对当地生态系统的负面影响。为了确保“自流井水产出层”的可持续性，实施有效的水资源管理策略至关重要。这包括监测水位、调节抽取水的数量，以及在用户中推广节约用水的做法。公众意识活动也可以在教育社区保护这些层的重要性方面发挥重要作用。总之，“自流井水产出层”是我们地下水资源的重要组成部分，为各种用途提供宝贵的水源。通过理解其特征并实施可持续管理实践，我们可以确保这些自然系统继续惠及未来几代人。随着我们面临与水资源短缺和气候变化相关的日益严峻的挑战，认识到“自流井水产出层”的重要性将是制定支持人类需求和环境健康的韧性水资源战略的关键。