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Markville CGC 1D1
Markville CGC 1D1

... Read page 90 in Encounter Canada and define the following terms in your own words. Provide examples for each of your definitions and sketches where appropriate. Biome: Boreal: Coniferous: Deciduous: GROUP B: VEGETATION REGIONS OF CANADA Define the term natural vegetation and provide an example. Then ...
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... Saturated hydraulic conductivity (old term-permeability) is the ease with which pores of a saturated soil transmit water. Formally, it is the proportionality coefficient that expresses the relationship of the rate of water movement to hydraulic gradient in Darcy's Law (a law that describes the rate ...
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... Saltpeter, white, translucent, lustrous mineral composed of potassium nitrate, KNO3. It crystallizes in the orthorhombic system in prismatic crystals, which have a hardness of 2 and a specific gravity of 2.1, and these crystals exhibit perfect domal cleavage. The mineral, which is also called niter ...
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Soil microbiology

Soil microbiology is the study of organisms in soil, their functions, and how they affect soil properties. It is believed that between two and four billion years ago, the first ancient bacteria and microorganisms came about in Earth's oceans. These bacteria could fix nitrogen, in time multiplied and as a result released oxygen into the atmosphere. This led to more advanced microorganisms. Microorganisms in soil are important because they affect soil structure and fertility. Soil microorganisms can be classified as bacteria, actinomycetes, fungi, algae and protozoa. Each of these groups has characteristics that define them and their functions in soil.Up to 10 billion bacterial cells inhabit each gram of soil in and around plant roots, a region known as the rhizosphere. In 2011, a team detected more than 33,000 bacterial and archaeal species on sugar beet roots.The composition of the rhizobiome can change rapidly in response to changes in the surrounding environment.
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