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Science of Life Explorations: What`s in Soil?
Science of Life Explorations: What`s in Soil?

... never alive - such as a rock - then it is inorganic. This is a good discussion point. Is a wooden fence organic? a book? a leather glove? Trees were alive, but what about leather? Remind students that leather is a by product of animals, and because leather is part of something that was once living, ...
Eons, Eras, Periods and Epochs Dating by radioactive isotopes
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Richmond Lake Water Quality Project: Septic Systems on Shoreline
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Verrucated Mountains
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coloring book - Soil Science Society of America
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... 1. Lakes and reservoirs are often stratified into layers with little vertical mixing, and they also have very little flow occurring. It may take from 1–100 years to flush and change water in lakes and reservoirs. 2. Lakes and reservoirs are much more vulnerable to runoff contamination of all kinds o ...
Basic Organic Gardening - Richmond Grows Seed Lending Library
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... enough water to make 1-1/2 quart (6 cups) total Use hot water to remove molasses from cup, then thoroughly mix up all the ingredients. Cut a 2-inch diameter hole just below the shoulder of a 1 gallon plastic jug (milk, water) and add mixture. Leave the cap on the jug. Hang the jug in the tree using ...
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... • The TDR technique is relatively insensitive to salinity as long as the salinity level is low enough that a useful wave form is returned • As salinity levels increase, the signal reflection from the ends of the rods in the TDR probe is lost (amplitude is less). • This occurs because of conduction o ...
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... water retention capacity~> is distributed on the coastal area of Hokkaido along the Sea of Okhotsk. 'fhe so-called heavy clay soils are classified into several soi l types; mainly Pseudogley soil and Brown Forest soil, and others. They are distributed on the coastal terrace, reflecting differences o ...
Chapter 14 – Weathering and Erosion
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... • Acid Precipitation - (Acid Rain) – natural rainwater is slightly acidic, but when it combines with nitrogen oxides and sulfur dioxides found in the air (due to burning fossil fuels), nitrous acid or sulfuric acid is formed in the rainwater. When this acid rain falls to the ground, it weathers ...
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Soil security, a new important concept Christos Tsadilas* Hellenic

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... so they can wedge apart crystals through freeze-thaw cycles or by evaporation-precipitation; water, for example, expands about 9% when it freezes; need water, temperature changes above and below the freezing point and pre-existing cracks. = Frost wedging 2. rapid heating (as in fires) 3. Wedging by ...
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Surface runoff



Surface runoff (also known as overland flow) is the flow of water that occurs when excess stormwater, meltwater, or other sources flows over the earth's surface. This might occur because soil is saturated to full capacity, because rain arrives more quickly than soil can absorb it, or because impervious areas (roofs and pavement) send their runoff to surrounding soil that cannot absorb all of it. Surface runoff is a major component of the water cycle. It is the primary agent in soil erosion by water.Runoff that occurs on the ground surface before reaching a channel is also called a nonpoint source. If a nonpoint source contains man-made contaminants, or natural forms of pollution (such as rotting leaves) the runoff is called nonpoint source pollution. A land area which produces runoff that drains to a common point is called a drainage basin. When runoff flows along the ground, it can pick up soil contaminants including, but not limited to petroleum, pesticides, or fertilizers that become discharge or nonpoint source pollution.In addition to causing water erosion and pollution, surface runoff in urban areas is a primary cause of urban flooding which can result in property damage, damp and mold in basements, and street flooding.
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