Detailed Notes on Water Infiltration and Soil Chemistry
Water in the Subsurface
Infiltration: The process where water enters the soil layer.
Soil Water: Water that has infiltrated into the soil; can be classified into two main components:
Gravity Water:
Defined as water that drains through soil to the saturated zone due to gravity.
Movement process: Percolation.
Limited utility for plant uptake as it quickly drains away.
Capillary Water:
Water that is retained in the soil due to electrical forces, primarily in soils with negative charge (like clay).
Water Molecule Polarity
Structure of Water Molecule (H₂O):
Composition: 2 Hydrogen (H) atoms and 1 Oxygen (O) atom.
Geometry: Not symmetrical; resembles Mickey Mouse where H atoms are on one side and O on the other.
Charge Distribution:
Oxygen atom (8 protons) attracts electrons more than hydrogen (1 proton).
Result:
Negative pole on the oxygen side (due to higher electron density).
Positive pole on the hydrogen side.
Polarity: Water molecules are polar, resulting in unique properties:
Universal Solvent: Water can dissolve many substances due to its polar nature.
Surface Tension: Polar interactions create a "skin" effect that supports light objects on the water's surface.
Capillary Action and Soil Interaction
Capillary Action: The ability of water to move against gravity through small spaces, important for water transport in plants.
Clay Humus Complex:
Composed of negatively charged clay and humus.
These components electrically hold onto capillary water against gravitational pull.
Capillary Water Definition:
Water that's held electrically in the soil by the clay humus complex, making it available for plant absorption.
Comparison with Gravity Water:
Capillary water is crucial for plants as it is within reach of roots, unlike gravity water that drains away to deeper layers.
Groundwater Formation
Result of Infiltrated Water: Precipitation infiltrates the surface, leading to:
Soil Water: Water held in the soil (both gravity and capillary water).
Groundwater: Water that percolates down to the saturated zone, not retained by soil structures.
Importance of Groundwater: It is a vital resource often supplied by surface water infiltration rather than magical processes.