|The oxygen and carbon dioxide content in the soil air and ordinary air is normally equal in areas with dense population of plants. A young soil can provide plants with sufficient amount of nutrients throughout its stages of growth. The parent materials of organic soil are rocks and minerals. Precipitation and temperature are components of climate that cannot affect the forces of weathering and soil development. The particle density provides information about how soil is affected with compaction from tillage operation. Soil color is a chemical property that can be used in the field to locate soil horizon in a soil profile. Parent materials provide information to what kind of soil will be formed in a particular locality. Time of soil formation and development is not that much longer as it happens like overnight. Properties of horizon A is not dominant in a transition AB horizon. Soil texture is a property that cannot be linked to soil's water holding сарacity Soil dominated with macropores is able to hold water for a long period of time. _Micropores in soil are the reason for the water to infiltrate at higher rate. Properties of horizon A is dominant over horizon B in a transition BA horizon. Minerals with high surface area are much easier to disintegrate compared to minerals with low surface area. Chemical structure of mineral is maintained even disintegrated

Human Anatomy & Physiology (11th Edition)

11th Edition

ISBN:9780134580999

Author:Elaine N. Marieb, Katja N. Hoehn

Publisher:Elaine N. Marieb, Katja N. Hoehn

Chapter1: The Human Body: An Orientation

Section: Chapter Questions

Problem 1RQ: The correct sequence of levels forming the structural hierarchy is A. (a) organ, organ system,...

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Transcribed Image Text:The oxygen and carbon dioxide content in the soil air and ordinary air is normally equal in areas with dense population of plants. A young soil can provide plants with sufficient amount of nutrients throughout its stages of growth. The parent materials of organic soil are rocks and minerals. Precipitation and temperature are components of climate that cannot affect the forces of weathering and s oil development. The particle density provides information about how soil is affected with compaction from tillage operation. Šoil color is a chemical property that can be used in the field to locate soil horizon in a soil profile. Parent materials provide infomation to what kind of soil will be formed in a particular locality. Time of soil formation and development is not that much longer as it happens like overnight. Properties of horizon A is not dominant in a transition AB horizon. Soil texture is a property that cannot be linked to soil's water holding сарacity Soil dominated with macropores is able to hold water for a long period of time. Micropores in soil are the reason for the water to infiltrate at higher rate. Properties of horizon A is dominant over horizon B in a transition BA horizon. Minerals with high surface area are much easier to disintegrate compared to minerals with low surface area. Chemical structure of mineral is maintained even disintegrated chemically.

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