what is the most abundant element in the eart
Nitrogen occupies 78% of air and oxygen occupies 21% of...
Texture refers to the size of the particles that make up the soil. The terms sand, silt, and clay refer to relative sizes of the soil particles. … The combined portions of sand, silt, and clay in a soil determine its textural classification.
Soil is the thin layer of material covering the earth’s surface and is formed from the weathering of rocks. … Weathering of rocks takes place. Rock is broken down into small particles. These small particles mix with humus (organic matter) and form soil.
Algae are scarcely populated in soil and their presence in soil and its activities is smaller when compared to that of either bacteria or fungi. Algal population in soil usually ranges from 100 to 10,000 numbers per gram of soil.
Microbes can make nutrients and minerals in the soil available to plants, produce hormones that spur growth, stimulate the plant immune system and trigger or dampen stress responses. In general a more diverse soil microbiome results in fewer plant diseases and higher yield.
Psychrophiles – active in temperatures less than 68 degrees. Mesophiles – Active in temperatures between 77 degrees and 95 degrees. This makes up the largest group of soil microbes and the range most activity charts are based on. Thermopholes – Active in temperatures from 115degrees to 150 degrees.
Four basic processes occur in soils— additions, losses, transformations (changes), and translocation (movement).
THE FIRST STEP IN SOIL FORMATION IS THE WEATHERING. THE RATE OF WEATHERING DEPENDS ON THE STRUCTURE OF THE ROCK AND MINERALS THAT MAKE UP THE ROCK.
The whole soil, from the surface to its lowest depths, develops naturally as a result of these five factors. The five factors are: 1) parent material, 2) relief or topography, 3) organisms (including humans), 4) climate, and 5) time.
UNIT OVERVIEW Earth is made up various living and nonliving materials. In the Minerals, Rocks, and Soil unit, students learn about the properties, classification, and uses for many nonliving Earth materials. Elements form minerals, and minerals form rocks.
The Sun heated up the rocks and the rain cooled them. This heating and cooling over thousands of years broke down the big rocks into smaller rocks. The smaller rocks continued to break down and formed tiny pieces of soil.
Sedimentary rocks are formed from deposits of pre-existing rocks or pieces of once-living organism that accumulate on the Earth’s surface. If sediment is buried deeply, it becomes compacted and cemented, forming sedimentary rock.
Soil formation involves two major processes: (1) slow chemical alteration by water seeping through the weathered rock material after rains and (2) mixing of the rock material with organic debris produced by the decay of plants.
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