Soil Science and the concept of soil

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50 Terms

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Soil

Derived from the latin word “SOLUM” means floor/ground

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Soil

True soil

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Soil

Non-renewable

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Inorganic matter

Sand, Silt & clay

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Organic matter

5% is the ideal OM

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Decomposition

Releases Oxygen and carbon dioxide

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VV Dokuchaiev (1900)

Father of Soil Science

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Whitney, 1892

Says that Soil a nutrient bin which supplies the nutrients necessary for plant growth.

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VV Dokuchaiev

Soil is natural body composed of mineral and organic matter

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Joffe, 1936

Soil is a dynamic natural body of mineral and organic matter that is spatially differentiated into different unconsolidated horizons of varialble depths

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Brady, 1969

Says that it is a natural body that is a varialble mixture of inorganic matter derived from the weatherin and disintregation of rocks and minerals and organic matter derived from the actively and fully decomposed organic matter.

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Jenny, 1941

Soil is equal to a combined influence of Climate and Organisms, modified by Relief/Topography, acting upon the Parent Material ove Significat period of Time (S=CL,O,R,PT)

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Soil

A natural body with thickness and width with distinct and indistict horizontal boundaries

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Components of Soil

Soil Solids 50%

Pores Spaces 50%

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Soil Solids

Mineral Water (45%)

Organic Matter (5%)

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Pore Spaces

Air (20-30%)

Water (20-30%)

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Mineral Matter

Derived from the decomposition and disintegration of rocks and minerals; “Soil Particles”; source of most nutrients present in the soil except nitrogen, oxygen and carbon

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Organic Matter

Derived from the decomposed living organisms; major source of nitrogen in the soil, thus, an indicative of N level in the soil

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Air 20-30%

Primarily composed of nitrogen, oxygen and carbon dioxide; soil air is the major source of oxygen for plants; has a humdity of 100%

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Carbon dioxide in soil air

Higher than atmospheric carbon dioxide with 78% N, 20% O, 0.5% CO2

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Water 20-30%

Transport nutrients to the roots; causes weathering of rocks and minerals Resulting to nutrient supply; also known as the soil solution; carries and moves dissolved nutrients

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Ped

A natural aggregates which continue persist when wetted and dried

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Pedon

A hexagonal column

<p>A <mark data-color="yellow" style="background-color: yellow; color: inherit">hexagonal</mark> column</p>
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Basic unit of soil

  • Ped

  • Clod

  • Pedon

  • Polypedon

  • Pedosphere

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Clod

An artificial structural unit formed by cultivation

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Pedon

Basic sampling unit in soil survey

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Pedon

Typically used to classify soil

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Polypedon

Typically used to map soil

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Polypedon

Multiple pedons that has distinct characteristics that differentiate it from surrounding polypedons or within a defined limit of single soil series

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Pedosphere

  • the soil mantle of the Earth

  • A zone of activity in which mineral, water, air and biological components come together to form soils

<ul><li><p><strong>the soil mantle of the Earth</strong></p></li><li><p><strong>A zone of activity in which mineral, water, air and biological components come together to form soils</strong></p></li></ul>
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Air and Water content

Is depending in the moisture condition of the soil 20-30% is the ideal level

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A saturated soil

Means that the pore spaces are fully occupied by water

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Field of soil science

  • Pedalogical

  • Edaphology

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Soil Science

The science that deals with soil as a natural body/resource, its pedology (classification and genesis), physical, chemical, biological and fertility characteristics in ultimate relation to crop management and production

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Pedological

  • Deals with the genesis, survey, classification and study of soils as a natural body. “Pedon”= Soil earth

  • Science concerned with the formation, nature, ecology, classification of soil

  • Study of soil's characteristics and its variations and does not focus on its immediate practical use or application

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Edaphology

  • Deals with the study of soils in relation to higher plants. “Edaphos”= Soil or ground

  • Science concerned with the study of how soil influences human's overall use of the land and also the effect of the soil to plants

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Difference of Pedalogical and Edaphology

Pedology is the study of nature or classification of soil while the edaphology is the study of soil influences human and plants

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Branches of Soil Science

  • Soil fertility

  • Soil physics

  • Soil Chemistry

  • Soil Biology and ecology

  • Soil Conservation and management

  • Soil Survey

  • Soil Genesis, Morphology and classification

  • Land-Use Plannin and Classification

  • Soil Mineralogy

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Essential Functions of Soil

  • Soil support plant growth

  • Soils regulate water supply

  • Soil functions as nature's recycling system

  • Soils are alive and home to various and diverse organisms

  • Soils influence the composition and physical condition of the atmosphere

  • Foundation and structural support of engineering structure

  • Preservation of earth's ecosystem

  • Soils serve sas an engineering medium

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Soil Fertility

  • Deals with the study of the properties of the soil which enables it to provide essential chemical elements in quantities and proportions for the growth of specific plants

  • Quality of sioils to provide optimum level of nutrients for plant growth

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Sol physics

  • Deals characteristics, properties, or interaction of soil which is caused by physical forces

  • Deals with the properties and interactionof the three soil phases (soild, liquid &gas)

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Soil Chemistry

  • Study the various chemical reactions in the soil solution, considering that the soil is an open system

  • Interaction between solid, liquid and gaseous phases of the soil

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Soil Biology & Ecology

  • Living organisms in the soil (bacteria, fungi, earthworms, nematodes).

  • Nutrient cycling, decomposition, soil health, and ecosystem services.

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Soil Conservation & Management

  • Protecting soil from erosion, degradation, and pollution.

  • Sustainable agriculture, watershed management, and climate adaptation.

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Soil Survey

  • Systematic study, description, and mapping of soils.

  • Provides data for agriculture, engineering, land-use planning.

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Soil Genesis, Morphology & Classification

Genesis: Soil formation processes.

Morphology: Physical appearance and profile properties.

Classification: Grouping soils based on characteristics (like USDA Soil Taxonomy, FAO, WRB).

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Land-Use Planning & Classification

  • Evaluating soil suitability for agriculture, forestry, urbanization, and engineering projects.

  • Guides proper land utilization while preventing degradation.

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Soil Mineralogy

  • Minerals in soils (clays, silicates, oxides).

  • Controls soil fertility, nutrient availability, and engineering properties.

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two main umbrellas

Pedology-Soil Survey, Genesis, Morphology, Classification, Mineralogy.

Edaphology-Soil Biology & Ecology, Soil Conservation & Management, Land-use planning.

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