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www.reference.com/article/definition-water-holding-capacity-79787e1edc5e417d

Water-holding capacity is defined as the water retained between field capacity and wilting point. Field capacity is the saturated state of water in the soil that can drain freely due to the force of gravity. Wilting point is the soil water level after its absorption by ...

www.reference.com/article/water-high-heat-capacity-7937c9c620e6f610

Water has a high heat capacity because a lot of heat energy is required to break the hydrogen bonds found in a molecule of water. Because the majority of heat energy is concentrated on breaking the hydrogen bonds, the water molecule itself heats up after the bonds are b...

www.reference.com/article/buffering-capacity-water-594ab855585ffc9d

Pure or distilled water has relatively no buffering capacity. The buffering capacity of water can vary somewhat if the water comes from an impure source such as a river or pond.

www.reference.com/article/lives-soil-1e1659392566b783

Soil is home to thousands of living organisms, including moles, earthworms, centipedes, millipedes and grubs. Snails, beetles, ants, mushrooms and fungi also live in soil. Most of these organisms play a fundamental role breaking down remains of plants and animals, trans...

www.reference.com/article/capacity-water-heater-3f9c0b458a44c6e0

Manufacturers list the water heater capacity on the ratings plate. With tank-style water heaters, the capacity is in gallons. This plate includes other important information, including the manufacturer, model, serial number, wattage of the heating elements and length of...

www.reference.com/article/soil-formed-73d78ec1767f77ac

Soil is formed when organic matter accrues and colloids are washed downward to deposit substances like clay, humus, carbonate, gypsum and iron oxide, which form a separate layer called the B horizon. This formation results from the effects of biological, chemical and ph...

www.reference.com/article/soil-affect-ph-water-c9a6164fc90dfbad

Depending on the chemicals in the soil, the pH of water passing through it increases, decreases or remain the same. In areas where water passes through soil containing limestone, dissolving the calcium carbonate in water creates a buffer solution, tying up the hydrogen ...