It become more by the help of the earthworm.
Soil can become more liquid when it absorbs excess water, causing a decrease in viscosity and turning it into mud or slurry. This can happen when there is heavy rainfall, snowmelt, or over-irrigation, leading to saturated soil conditions.
When there is no more grass, the soil can become more prone to erosion due to lack of root systems holding it together. Soil quality may decline as there are no longer plants helping to cycle nutrients. Additionally, without grass to provide organic matter, the soil may become less fertile over time.
When you add water to soil, the density typically decreases as the water fills in the pore spaces between soil particles. This can cause the soil to become more compacted and settle, leading to a reduction in overall density compared to dry soil.
Soil turns into mud when it absorbs water, causing the soil particles to separate and the mixture to become more liquid-like. This is due to the water filling the spaces between the soil particles, reducing friction and allowing the particles to move more freely, creating a muddy consistency.
Clay soil is generally more porous than sandy soil because clay particles are smaller and have more surface area for water retention. However, clay soil can become waterlogged more easily due to its fine particle size, which can restrict water drainage compared to sandy soil.
Soil can become more liquid when it absorbs excess water, causing a decrease in viscosity and turning it into mud or slurry. This can happen when there is heavy rainfall, snowmelt, or over-irrigation, leading to saturated soil conditions.
When there is no more grass, the soil can become more prone to erosion due to lack of root systems holding it together. Soil quality may decline as there are no longer plants helping to cycle nutrients. Additionally, without grass to provide organic matter, the soil may become less fertile over time.
because it turns into soil using the power of magic
When you add water to soil, the density typically decreases as the water fills in the pore spaces between soil particles. This can cause the soil to become more compacted and settle, leading to a reduction in overall density compared to dry soil.
Fields become muddy when there is an excessive amount of water or rain that saturates the soil, making it unable to absorb any more water. This causes the top layer of soil to become waterlogged and turn into mud. Heavy foot traffic or livestock can further churn up the soil, exacerbating the muddy conditions.
Soil turns into mud when it absorbs water, causing the soil particles to separate and the mixture to become more liquid-like. This is due to the water filling the spaces between the soil particles, reducing friction and allowing the particles to move more freely, creating a muddy consistency.
Clay soil is generally more porous than sandy soil because clay particles are smaller and have more surface area for water retention. However, clay soil can become waterlogged more easily due to its fine particle size, which can restrict water drainage compared to sandy soil.
Compacted soil absorbs less water when wet, as the pores in the soil become filled with water and limit additional water flow into the soil. When the soil is dry, the pores are more open, allowing for better water absorption.
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Nitrogen in soil can become limited if there is an imbalance in the nitrogen cycle, where plants remove more nitrogen than is being replenished through processes like nitrogen fixation. Factors such as over-fertilization, leaching, erosion, and poor crop rotation can also contribute to nitrogen depletion in soil.
A soil is acidic because there are compounds within it which dissolve in water to form an acid. An acid is defined as a substance which readily gives out protons to oter molecules. An alkali is the converse, in that it is a proton acceptor and readily takes on protons. Treating an acidic soil with an alkali would neutralise the soil, and so the soil would become less acidic. If enough alkali is added, the soil will become neutral, and it will become alkaline if even more alkali is added.
As in all acid-base (alkali) reactions, it will reduce the acidity of the soil and, if there is an excess of base to acid, it can make the soil become alkaline. The soil will be less acidic if base is less than acidity, become neutral (if base = acidity), or become alkaline if base is greater than acidity.