impermeable rock

简明释义

不透水岩石

英英释义

例句

1.Geologists often look for impermeable rock (不透水岩石) when searching for oil reservoirs.

地质学家在寻找油藏时，通常会寻找impermeable rock（不透水岩石）。

2.The water table is protected by layers of impermeable rock (不透水岩石), preventing contamination from surface pollutants.

水位受到一层层的impermeable rock（不透水岩石）保护，防止地表污染物的污染。

3.During the construction of the dam, engineers discovered a layer of impermeable rock (不透水岩石) that would help retain water effectively.

在大坝建设过程中，工程师发现了一层impermeable rock（不透水岩石），这将有助于有效地蓄水。

4.In the study of soil and water conservation, impermeable rock (不透水岩石) layers are crucial for maintaining aquifers.

在土壤和水资源保护研究中，impermeable rock（不透水岩石）层对于维持含水层至关重要。

5.The presence of impermeable rock (不透水岩石) can significantly affect groundwater flow in an area.

在一个地区，impermeable rock（不透水岩石）的存在会显著影响地下水流动。

作文

The study of geology reveals a fascinating aspect of our planet's structure, particularly the role of different types of rocks in the water cycle. Among these rocks, impermeable rock plays a crucial role in determining how water moves through the earth's crust. By definition, impermeable rock refers to a type of rock that does not allow fluids to pass through it. This characteristic makes it an essential component in various geological and environmental processes.One of the most significant functions of impermeable rock is its ability to act as a barrier to groundwater flow. In many regions, layers of impermeable rock can trap water, creating aquifers that are vital for human consumption and agricultural use. When rainwater seeps into the ground, it often encounters these layers, which prevents the water from continuing to move downward. Instead, the water accumulates above the impermeable rock, forming a saturated zone that can be tapped into by wells.In addition to its role in aquifer formation, impermeable rock also influences surface water bodies. For instance, when rivers or lakes are situated above layers of impermeable rock, they tend to retain their water levels more consistently, as there is little to no drainage into the ground below. This can lead to the creation of stable ecosystems that rely on these water sources. Conversely, if impermeable rock is absent, water can quickly drain away, leading to reduced water availability for plants and animals.The presence of impermeable rock can also have significant implications for construction and urban development. Engineers must consider these geological features when planning buildings, roads, and other infrastructure. If a construction site is located above a layer of impermeable rock, it may require special drainage solutions to prevent flooding and water accumulation. Understanding the location and extent of impermeable rock layers can help mitigate risks associated with water management in urban areas.Moreover, impermeable rock can play a role in natural hazards such as landslides and flooding. Areas with steep slopes and impermeable rock layers are more susceptible to landslides, especially during heavy rainfall. The inability of water to permeate through the rock can lead to increased surface runoff, which may destabilize the soil above and trigger a slide. Recognizing these risks is vital for disaster preparedness and land-use planning.In conclusion, the understanding of impermeable rock is essential for various fields, including hydrology, environmental science, and civil engineering. Its unique properties significantly influence groundwater movement, surface water stability, and urban planning. As we continue to explore and manage our natural resources, recognizing the importance of impermeable rock will be crucial for sustainable development and environmental conservation. By integrating geological knowledge into our decision-making processes, we can better protect our water supplies and ensure a balanced ecosystem for future generations.

地质学的研究揭示了我们星球结构的一个迷人方面，特别是不同类型的岩石在水循环中的作用。在这些岩石中，不渗透岩石在决定水如何在地壳中移动方面发挥着关键作用。根据定义，不渗透岩石是指一种不允许流体通过的岩石。这一特性使其成为各种地质和环境过程的基本组成部分。不渗透岩石最重要的功能之一是其作为地下水流动障碍的能力。在许多地区，不渗透岩石的层可以捕获水，形成对人类消费和农业使用至关重要的含水层。当雨水渗入地下时，它通常会遇到这些层，阻止水继续向下移动。相反，水在不渗透岩石之上积累，形成饱和区，可以通过井进行抽取。除了在含水层形成中的作用外，不渗透岩石还会影响地表水体。例如，当河流或湖泊位于不渗透岩石层之上时，它们的水位往往保持得更为稳定，因为几乎没有排水进入下面的土壤。这可以导致稳定生态系统的形成，这些生态系统依赖于这些水源。相反，如果缺乏不渗透岩石，水可能会迅速排出，导致植物和动物的水源减少。不渗透岩石的存在对于建筑和城市发展也有重大影响。工程师在规划建筑、道路和其他基础设施时必须考虑这些地质特征。如果施工现场位于不渗透岩石层之上，可能需要特殊的排水解决方案来防止洪水和水的积聚。理解不渗透岩石层的位置和范围可以帮助减轻与城市地区水管理相关的风险。此外，不渗透岩石还可能在自然灾害如滑坡和洪水中发挥作用。具有陡峭坡度和不渗透岩石层的地区在强降雨期间更容易发生滑坡。水无法渗透岩石可能导致地表径流增加，从而使上方的土壤失去稳定性并引发滑坡。认识到这些风险对于灾害准备和土地使用规划至关重要。总之，理解不渗透岩石对水文学、环境科学和土木工程等多个领域至关重要。其独特的特性显著影响地下水运动、地表水的稳定性以及城市规划。随着我们继续探索和管理自然资源，认识到不渗透岩石的重要性对于可持续发展和环境保护将至关重要。通过将地质知识融入我们的决策过程中，我们可以更好地保护水资源，确保未来世代的生态平衡。