Groundwater.
percolation rate (mL/min) = amount of water (mL)/percolation time (min) For example, suppose that for a certain sample, it took 20 minutes for 200 mL to percolate. So, rate of percolation =200 ml/20 min=10 ml/min. Weight of soil = 50g Initial volume of water in the measuring cylinder = U mL Final volume of water in the measuring cylinder = V mL Volume of water absorbed by the soil = (U Weight of water absorbed by the soil = (U (1 mL of water has weight equal to 1 g) percentage of water absorbed=(U-V)*100/50
The plants absorb minerals from the soil, since it is wet. When the soil is dry, there is no way for plants to absorb anything. That's what rain do, by making the soil wet, so that plants can absorb minerals through their roots.
absorbed
soil is not dissolve in water because plants grow in soil and water them
water
soil
Water is absorbed by plants through the soil. When water is poured into the soil, the roots of the plant soak in the moisture from the soil, which allows the nutrients and vitamins to thrive.
52 liters
Water that is absorbed through the soil surface is called seepage. This is water that soaks into the ground, usually in a low spot of the area.
Rivers & oceans.
percolation
From the roots
It is called Condensation
Watershed
As you know that water is a universal solvent, so it dissolves almost every thing. So, as the water is absorbed by soil, automatically plant nutrients are also absorbed by the soil.
It is absorbed from the soil. There are no phosphates in water, though water can help phosphates and other nutrients enter the roots of plants.
The soil is at "field capacity". In other words the capillary spaces are already full of water to the surface, hence no more water can be absorbed.