Compactness with the free space of the soil differs the water that it can hold.
For example: in Sand, it has free space but there is no compactness so it just does not get stored in the sandy soil but in a Clay, it has compactness but no good free space so, it takes time to intake water while Lacustrine and other loamy soil can absorb the water and store it very fast manner with compactness to hold the water as well as the free space for the water to be placed.
3 abiotic factors that affect a coniferous forest is the soil, the amount of rainfall, and the amount of sunlight that reaches the plants and animals. hi lillie
Crops hold the soil together with their roots, therefor preventing soil erosion.
Factors that affect evaporation include temperature, humidity, wind velocity, exposed surface area, porosity of soil, grain size of soil particles, soil water content, matric potential, and sun intensity.
Deforestation
Because depends on how the soil is
the answer to this question is that Soil with smaller particles can hold more water when Soil with larger rock particles can hold less water.....
Yes because diffrent types of soil have diffrent amounts of density
soil texture deterimines how much water soil can hold
It may seem that dry soil can hold more water but that's not the case. If it is the same soil used in two different tests, then wet or dry, the soil will hold the same amount of water. The water soaked soil would appear to hold less water because it is already absorbing it's capacity (or closer to it), whereas the dry soil will hold just as much but will take more water to reach it's "soaked" point since it is dry and void of moisture.
Water holding capacity of soil is just that, the specific ability of a particular type of soil to hold water against the force of gravity. Different types of soils have difference capacities, for example a sand soil had a lower capacity to hold water when compared to a clay soil. The nature of the soil, composition of the soil, amount of organic component and size of the soil particles determine its ability to retain water. Water molecules are held closely to the individual soil particles by forces of cohesion. The maximum amount of water a soil can hold before it is saturated and starts to loose water by gravity is known as "field capacity"
In order for soil to increase its ability to hold water it must have a higher amount of clay present in it. The more clay present in the soil, the more water it will hold. The opposite to this is how sandy or grainy the soil is, if it is too sandy then it will not hold water very well.
Water retention in soil refers to the ability of soil to hold onto water. It affects plant growth and nutrient availability by influencing the amount of water and nutrients available to plants. Soil with poor water retention can lead to water stress in plants, affecting their growth and nutrient uptake. Conversely, soil with good water retention can provide a consistent supply of water and nutrients to plants, promoting healthy growth and nutrient availability.
The amount of soil can affect plant growth by providing nutrients and support to the roots. A larger amount of soil allows for more root growth, increasing the plant's ability to absorb water and nutrients. Conversely, plants may struggle to thrive in limited soil volume due to restricted root development.
poor soil means no. of voids more and soil does not hold nuritent the seepage loose more.it also affect crop yield
soil
Yes, topsoil can hold water. Topsoil is the upper layer of soil that is rich in organic matter and nutrients, making it capable of retaining water. The ability of topsoil to hold water is important for supporting plant growth and providing moisture for roots.
Yes, organic material can increase the absorbency of water in soil by improving soil structure and increasing the soil's ability to hold onto water. Organic matter acts like a sponge, holding onto water and keeping it available for plant roots.