Luvisol from the Netherlands. Used in: WRB, other: WRB code: LV: Profile: AhEBtC: Climate: Humid temperate climate: Luvisols are a group of soils, comprising one of the 32 Reference Soil Groups in the international system of soil classification, the World Reference Base for Soil Resources (WRB). [1]

Luvisol, one of the 30 soil groups in the classification system of the Food and Agriculture Organization (FAO). The mixed mineralogy, high nutrient content, and good drainage of these soils make them suitable for a wide range of agriculture, from grains to orchards to vineyards. Luvisols form on

Summary description of Luvisols Connotation: soils in which clay is washed down from the surface soil to an accumulation horizon at some depth; from L. luere, to wash. Parent material: a wide variety of unconsolidated materials including glacial till, and eolian, alluvial and colluvial deposits. Environment: most common in flat or gently sloping land in …

It represents one of the few still active long-term field experiments on sandy soil. The most common soil subtype is Haplic Luvisol (FAO and IUSS, 2015). The experiment includes 21 treatments: five levels of mineral fertilization combined with four levels of organic fertilization and one control treatment.

高活性淋溶土（Luvisol）是1998年公布的土壤学名词，出自《土壤学名词》第二版。

版权所有：中国科学院南京土壤研究所 备案序号：苏icp备05004320号-12 本数据库由“中国科学院十三五信息化专项科学大数据工程项目”提供支持

The concept and theory of lessivage gave birth to the Luvisol, consisting of forest derived humus over a “podzolized” surface mineral soil below which is a clay enriched solum. However, there is still debate as to whether lessivage and podzolization are distinct processes as some illuvial horizons in sandy soils have properties that reflect ...

Brown Luvisol with distinct eluvial horizon between 20 and 45 cm depth and an argic horizon below, having pronounced films of illuviated clay, Ireland (Cutanic Luvisol; ISRIC reference soil IE 007) Contact:

2016年1月1日 · Soil‐pH has a significant influence. At pH values below 5 (measured in water 1:1), there is a sufficiently high concentration of Al 3+ in the soil solution to keep the clay flocculated. Between pH 5.5 and 7.0, the content of exchangeable aluminum is much lower and provided that divalent ions are in low concentration, clay can disperse.

2023年6月25日 · Soil organic matter is a biological system that functions as an integrated whole. These assemblies have different properties, functions, and decomposition times. SOM is one of the main determinants of soil productivity. Our studies were carried out in a temperate deciduous oak forest on Luvisols soil. In the DIRT Project (Detritus Input and Removal Treatments), the following treatments were ...