roots
Soil compaction can reduce pore space in the soil, limiting water infiltration and drainage which can lead to water logging and decreased oxygen levels in the soil. This can hinder root growth and nutrient uptake by plants. Compacted soil also limits microbial activity, which is crucial for nutrient cycling in the soil.
Sandy soil is typically nutrient-poor but drains well, whereas clay soil is nutrient-rich but often retains water. A soil that holds water poorly but has many nutrients may be loamy soil, which is a mix of sand, silt, and clay and offers good drainage while being nutrient-rich. Organic matter can also improve water retention in nutrient-rich soils.
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.
Land development can disrupt nutrient cycles in soil by removing vegetation that replenishes nutrients, disrupting soil organisms that aid in nutrient recycling, and altering the water flow that transports nutrients through the soil. This can lead to nutrient depletion in the soil and affect plant growth and ecosystem health.
Water that soaks into the ground and collects in pores in soil and rock becomes groundwater. Groundwater is water that has infiltrated the soil and rocks below the Earth's surface, filling the spaces between particles or within cracks and cavities. It is an important water source for wells and springs.
The roots, of course.
Soil compaction can reduce pore space in the soil, limiting water infiltration and drainage which can lead to water logging and decreased oxygen levels in the soil. This can hinder root growth and nutrient uptake by plants. Compacted soil also limits microbial activity, which is crucial for nutrient cycling in the soil.
Sandy soil is typically nutrient-poor but drains well, whereas clay soil is nutrient-rich but often retains water. A soil that holds water poorly but has many nutrients may be loamy soil, which is a mix of sand, silt, and clay and offers good drainage while being nutrient-rich. Organic matter can also improve water retention in nutrient-rich soils.
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.
No it collects nutrients and water from the soil
Land development can disrupt nutrient cycles in soil by removing vegetation that replenishes nutrients, disrupting soil organisms that aid in nutrient recycling, and altering the water flow that transports nutrients through the soil. This can lead to nutrient depletion in the soil and affect plant growth and ecosystem health.
Water that soaks into the ground and collects in pores in soil and rock becomes groundwater. Groundwater is water that has infiltrated the soil and rocks below the Earth's surface, filling the spaces between particles or within cracks and cavities. It is an important water source for wells and springs.
an underground layer of rock that can hold water is an aquifer.
Air, moisture and nutrient content are ways to compare compost and soil. Soil can be nutrient- and water-deficient in the case of sand and nutrient- and water-retentive in terms of clay and loam. Dark-colored, fresh-smelling, nutrient-rich compost may be added to correct air, moisture and nutrient deficiencies or excesses through amending, fertilizing or mulching actions.
This is known as pore water. If the soil or rock is in-situ (in other words in the ground) it may also be known as ground water.
Nutrient fertilizer gets to the roots when you water it, it goes down and it gets in threw the soil
Nutrient rich soil, water, and sun.