Assessing capabilities of soil and water resources in drylands 2025

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Dryland soils are classified as Calcisols, Gypsisols, Steppe soils and Leptosols in the World Reference Base for Soil Resources (WRB, IUSS, 2022). Climate, vegetation and parent materials are the primary factors of soil formation in drylands.
Soil moisture plays an important role in agricultural monitoring, drought and flood forecasting, forest fire prediction, water supply management, and other natural resource activities. Soil moisture observations can forewarn of impending drought or flood conditions before other more standard indicators are triggered.
Soil water is a crucial nutrient to plants and is also a media for transporting nutrients for plant growth. It also plays key role in soil forming process, weathering of rocks and process of photosynthesis. Soil water can become blue water or recharge groundwater by gravity.
soil water content - Amount of water a given soil can store, primarily influenced by the soil texture and the soil organic matter content. In general, soils with greater silt and clay-sized particles have greater water- holding capacities. Likewise, soils with more organic matter have greater water-holding capacities.
In drylands, land degradation is known as dedocHubcation. It is estimated that 25-35% of drylands are already degraded, with over 250 million people directly affected and about one billion people in over one hundred countries at risk.
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They have several characteristics that make them unique : Rainfall scarcity. High temperatures. Evapotranspiration and low humidity.

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