eChapter Name: Improving Water Retention and Nutrient Uptake
9789358879018
eBook Name: REGENERATIVE AGRICULTURE
by Vivek Kamble, Princy Thakur, Meraj Ahmed
Introduction
Water retention is an important soil hydraulic property that affects how soil operates in an ecosystem and how it is managed. Hydrology, agronomy, meteorology, ecology, environmental protection, and many other soil-related professions employ soil water retention data. Some soil survey programs measure water retention. A soil survey can estimate water retention from other soil properties. However, these measurements are problematic during project design and in large-scale implementations (Rawls et al., 1991; Wo sten et al., 2001) since agricultural land needs rise periodically. Agriculture is using dry land. Food self-sufficiency and becoming a world food barn by 2045 necessitate agricultural land expansion (Mulyani and Agus, 2017). Water concerns afflict farming in this agroecosystem (Syam et al., 1996; Mulyani and Agus, 2017). Because of soil composition, much water stays in the earth. Tang et al. (2022).
For plant growth, soil water retention variables indicate how well the soil holds water. The dirt provides most of the plant’s water. Water in root layer dirt pores is absorbed by plants. Thus, soil water retention is the key factor affecting plant development and productivity. Plants can take in the soil pores’ water between the field capacity and the point where they always wilt. Field capacity occurs when the matrix potential and gravitational potential match. The most significant component for plant growth is soil water (Tang et al., 2022, Deng et al., 2016, Su et al., 2020). The soil’s physical features determine plant water availability. The amount of water available depends on clay minerals, organic matter, absorbed cations, soil texture and structure, and water availability. Thus, to prevent plants from experiencing water or groundwater stress, soil physical attributes must be investigated to determine groundwater availability (Kirkham 2023). Infiltration is crucial to groundwater availability. The amount of water that can penetrate the soil depends on its physical features, such as soil texture, organic matter, bulk density, porosity, aggregate stability/stability, and water content. Thus, soil water availability depends on its physical qualities, particularly its ability to absorb and transfer water. The physical properties of saturated soil affect how water travels through it, which affects runoff and infiltration (Sauer and Logsdon 2002).