laterization

简明释义

[ˌlætəraɪˈzeɪʃən][ˌlætərəˈzeɪʃn]

n. 红土化作用

英英释义

Laterization is a geological process characterized by the leaching of soluble minerals from the upper layers of soil and rock, often leading to the accumulation of iron and aluminum oxides.

后期化是一种地质过程,其特征是可溶性矿物从土壤和岩石的上层被浸出,通常导致铁和铝氧化物的积累。

单词用法

the process of laterization

后期化的过程

laterization of soils

土壤的后期化

laterization phenomenon

后期化现象

intense laterization

强烈后期化

laterization rates

后期化速率

laterization processes

后期化过程

同义词

leaching

淋滤

The process of leaching can lead to nutrient loss in the soil.

淋滤过程可能导致土壤中养分的流失。

weathering

风化

Weathering is a key factor in soil formation and landscape evolution.

风化是土壤形成和地貌演变的关键因素。

pedogenesis

土壤形成

Pedogenesis involves various processes including laterization.

土壤形成涉及包括后期化在内的多种过程。

反义词

dehydration

脱水

Dehydration can lead to serious health issues if not addressed promptly.

如果不及时处理,脱水可能会导致严重的健康问题。

desaturation

去饱和

The desaturation of colors in the image gives it a more muted tone.

图像中色彩的去饱和使其呈现出更柔和的色调。

例句

1.Supergenous enrichment of gold during the laterization is also discussed.

最后讨论了红土化过程小金的表生富集作用。

2.Supergenous enrichment of gold during the laterization is also discussed.

最后讨论了红土化过程小金的表生富集作用。

3.Scientists study laterization to understand how minerals are leached from the soil.

科学家研究laterization(后发育化)以了解矿物如何从土壤中被淋洗。

4.In areas where laterization occurs, red and yellow soils are often prevalent.

在发生laterization(后发育化)的地区,红土和黄土通常很常见。

5.Agricultural practices must adapt to the effects of laterization in certain climates.

农业实践必须适应某些气候中laterization(后发育化)的影响。

6.The laterization process leads to the formation of lateritic soils rich in iron and aluminum.

laterization(后发育化)过程导致富含铁和铝的红土形成。

7.The process of laterization can significantly affect soil fertility in tropical regions.

在热带地区,laterization(后发育化)过程会显著影响土壤肥力。

作文

Laterization is a geological process that plays a significant role in soil formation and mineral alteration. This phenomenon occurs primarily in tropical and subtropical regions, where high temperatures and abundant rainfall create ideal conditions for chemical weathering. The term 'laterization' refers to the transformation of rocks and minerals into a layer of laterite, which is rich in iron and aluminum oxides. As rainwater seeps through the soil, it leaches away soluble minerals, leaving behind these oxides and resulting in a distinct red or yellow coloration of the soil. This process not only affects the soil's nutrient content but also influences agricultural practices in these regions.Understanding laterization (土壤后期化) is crucial for farmers and environmental scientists alike. In agricultural contexts, the laterization process can lead to the depletion of essential nutrients such as potassium and magnesium, making it challenging to maintain soil fertility. Farmers must adapt their practices by using fertilizers that can replenish these nutrients or by implementing crop rotation strategies that enhance soil health. Moreover, understanding how laterization affects soil structure can aid in developing sustainable land management practices that prevent erosion and degradation.In addition to agriculture, laterization has implications for ecology and biodiversity. The unique soils formed through this process support specific types of vegetation that are adapted to low nutrient availability. For instance, many tropical rainforests thrive in lateritic soils, as the trees and plants have evolved mechanisms to extract nutrients efficiently. However, deforestation and land-use changes can disrupt these ecosystems, leading to loss of biodiversity and increased carbon emissions.The study of laterization is not limited to its effects on soil and agriculture; it also extends to geology and mining. Areas with significant laterization often become sites for mining operations, particularly for bauxite, which is the primary ore for aluminum production. The economic importance of these resources underscores the need for responsible mining practices that minimize environmental impact. As we extract minerals from lateritic soils, we must also consider the long-term consequences of disrupting these ecosystems.In conclusion, laterization (土壤后期化) is a complex process that significantly influences soil characteristics, agricultural productivity, and ecological balance. By understanding this process, we can develop better land management strategies that promote sustainability and protect our natural resources. As global populations continue to grow, the importance of studying laterization will only increase, highlighting the need for ongoing research and education in this field.

后期化是一个地质过程,在土壤形成和矿物改变中起着重要作用。这一现象主要发生在热带和亚热带地区,在这些地方,高温和丰富的降雨创造了理想的化学风化条件。术语“后期化”指的是岩石和矿物转变为富含铁和铝氧化物的红土层。当雨水渗透土壤时,它会淋洗掉可溶性矿物,留下这些氧化物,从而导致土壤呈现出明显的红色或黄色。这一过程不仅影响土壤的养分含量,还会影响这些地区的农业实践。理解后期化laterization)对农民和环境科学家来说至关重要。在农业背景下,后期化过程可能导致钾和镁等必需营养素的耗竭,使得保持土壤肥力变得具有挑战性。农民必须通过使用能够补充这些营养素的肥料或实施增强土壤健康的轮作策略来调整他们的实践。此外,了解后期化如何影响土壤结构可以帮助开发可持续的土地管理实践,以防止侵蚀和退化。除了农业,后期化还对生态和生物多样性产生影响。通过这一过程形成的独特土壤支持特定类型的植被,这些植被适应低营养可用性。例如,许多热带雨林在红土土壤中繁盛,因为树木和植物已经进化出有效提取养分的机制。然而,森林砍伐和土地利用变化可能会破坏这些生态系统,导致生物多样性的丧失和碳排放的增加。对后期化的研究并不限于其对土壤和农业的影响;它还扩展到地质学和采矿。具有显著后期化特征的地区往往成为采矿作业的地点,尤其是铝土矿,这是铝生产的主要矿石。这些资源的经济重要性凸显了负责任的采矿实践的必要性,以最小化环境影响。当我们从红土土壤中提取矿物时,我们还必须考虑破坏这些生态系统的长期后果。总之,后期化(土壤后期化)是一个复杂的过程,对土壤特性、农业生产力和生态平衡有显著影响。通过理解这一过程,我们可以制定更好的土地管理策略,以促进可持续性并保护我们的自然资源。随着全球人口的不断增长,研究后期化的重要性只会增加,突显了这一领域持续研究和教育的必要性。