calcium cycle

简明释义

钙循环;

英英释义

The calcium cycle refers to the continuous movement of calcium through various environmental compartments, including the lithosphere (earth), hydrosphere (water), biosphere (living organisms), and atmosphere (air).

钙循环是指钙在不同环境组分之间的持续运动,包括岩石圈(地球)、水圈(水)、生物圈(生物体)和大气圈(空气)。

例句

1.The study of the calcium cycle helps us understand how calcium moves through the environment.

钙循环的研究帮助我们理解钙是如何在环境中循环的。

2.Understanding the calcium cycle can help improve agricultural practices.

理解钙循环可以帮助改善农业实践。

3.In marine ecosystems, the calcium cycle is crucial for coral reef formation.

在海洋生态系统中,钙循环对珊瑚礁的形成至关重要。

4.The calcium cycle plays a significant role in bone health and development.

钙循环在骨骼健康和发育中发挥着重要作用。

5.Farmers need to consider the calcium cycle when managing soil health.

农民在管理土壤健康时需要考虑钙循环

作文

The calcium cycle is a crucial part of the biogeochemical cycles that sustain life on Earth. It describes the movement of calcium through various environmental compartments, including soil, water, and living organisms. Calcium is an essential nutrient for all living organisms, playing a significant role in physiological processes such as muscle contraction, nerve function, and blood coagulation. The calcium cycle ensures that this vital element is available in forms that can be absorbed by plants and animals, thus supporting the entire food web.Calcium primarily enters the calcium cycle through weathering of rocks, particularly limestone, which is rich in calcium carbonate. When rainwater, slightly acidic due to dissolved carbon dioxide, seeps into the ground, it reacts with the calcium carbonate in rocks, breaking it down into soluble calcium ions. These ions then leach into the soil and waterways, making their way into the roots of plants. This process is vital for plant growth, as calcium is necessary for cell wall stability and overall structural integrity.Once absorbed by plants, calcium becomes part of the plant's biological structure. Herbivores consume these plants, incorporating calcium into their own bodies. In this way, the calcium cycle facilitates the transfer of calcium from the soil, through plants, and into animal tissues. When animals die or excrete waste, calcium is returned to the soil or water, where it can again be utilized by plants or microorganisms.Decomposers, such as bacteria and fungi, play a vital role in the calcium cycle. They break down dead organic matter, releasing calcium back into the environment. This process not only recycles nutrients but also enriches the soil, promoting further plant growth. The cycling of calcium is essential for maintaining healthy ecosystems, as it supports plant health, which in turn sustains herbivores and carnivores.In aquatic systems, the calcium cycle operates similarly. Calcium ions are present in water bodies, often originating from the erosion of rocks and soil. Aquatic plants and algae absorb these ions, contributing to their growth and providing food for fish and other marine organisms. The death and decomposition of aquatic life also return calcium to the water, perpetuating the cycle.Human activities have significantly impacted the calcium cycle, particularly through agriculture and urbanization. Excessive use of fertilizers can lead to nutrient runoff, disrupting the natural balance of calcium in ecosystems. Additionally, mining and industrial processes can alter the availability of calcium in the environment, potentially leading to deficiencies in both terrestrial and aquatic systems.In conclusion, the calcium cycle is a vital process that supports life by ensuring the availability of calcium across various ecosystems. Understanding this cycle is essential for managing natural resources sustainably and protecting biodiversity. By recognizing the interconnectedness of calcium within the environment, we can better appreciate the delicate balance of nature and our role in preserving it.

钙循环是维持地球生命的重要生物地球化学循环之一。它描述了钙在土壤、水和生物体等不同环境成分之间的运动。钙是所有生物体所需的基本营养素,在肌肉收缩、神经功能和血液凝固等生理过程中发挥着重要作用。钙循环确保这一重要元素以植物和动物能够吸收的形式存在,从而支持整个食物网。钙主要通过岩石的风化进入钙循环,特别是富含碳酸钙的石灰岩。当雨水因溶解的二氧化碳而略带酸性时,它渗入地下,与岩石中的碳酸钙发生反应,将其分解为可溶的钙离子。这些离子随后渗入土壤和水道,进入植物的根部。这个过程对于植物的生长至关重要,因为钙是细胞壁稳定性和整体结构完整性的必要物质。一旦被植物吸收,钙便成为植物生物结构的一部分。食草动物会食用这些植物,将钙纳入自身的身体中。通过这种方式,钙循环促进了钙从土壤、通过植物,再到动物组织的转移。当动物死亡或排泄废物时,钙会返回土壤或水中,供植物或微生物再次利用。分解者,如细菌和真菌,在钙循环中发挥着至关重要的作用。它们分解死去的有机物质,将钙释放回环境中。这个过程不仅回收了营养物质,还丰富了土壤,促进了进一步的植物生长。钙的循环对于维持健康的生态系统至关重要,因为它支持植物健康,而植物又支撑着食草动物和食肉动物。在水体系统中,钙循环的运作类似。水体中存在钙离子,通常来源于岩石和土壤的侵蚀。水生植物和藻类吸收这些离子,促进它们的生长,并为鱼类和其他海洋生物提供食物。水生生物的死亡和分解也将钙返回水中,延续循环。人类活动对钙循环产生了显著影响,尤其是通过农业和城市化。过度使用肥料可能导致营养物质径流,破坏生态系统中钙的自然平衡。此外,采矿和工业过程可能改变环境中钙的可用性,可能导致陆地和水域系统中的缺乏。总之,钙循环是一个重要的过程,通过确保钙在各种生态系统中的可用性来支持生命。理解这一循环对于可持续管理自然资源和保护生物多样性至关重要。通过认识到钙在环境中的相互联系,我们可以更好地欣赏自然的微妙平衡以及我们在保护它方面的角色。

相关单词

calcium

calcium详解:怎么读、什么意思、用法

cycle

cycle详解:怎么读、什么意思、用法