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31. soil science By Allah Dad Khan

Mr.Allah Dad Khan
Mr.Allah Dad Khan
Mr.Allah Dad KhanPeshawar at Consultany Natural Resource Management Specialist IUCN PAkistan

31. soil science By Allah Dad Khan

31. soil science By Allah Dad Khan

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31. soil science By Allah Dad Khan
Soil Science By Allah
Dad Khan
Soil
Dirt is simply misplaced soil!
SOIL: A RENEWABLE
RESOURCE
• Soil is a slowly renewed resource
that provides most of the nutrients
needed for plant growth and also
helps purify water.
– Soil formation begins when bedrock is
broken down by physical, chemical
and biological processes called
weathering.
• Mature soils have developed
over a long time are arranged in a
series of horizontal layers,soil
Fig. 15-8, p. 343
Erosion
Transportation
Weathering
Deposition
Igneous rock
Granite,
pumice,
basalt
Sedimentary
rock
Sandstone,
limestone
Heat, pressure
Cooling
Heat, pressure,
stress
Magma
(molten rock)
Melting
Metamorphic rock
Slate, marble,
gneiss, quartzite
Layers in Mature Soils
• Infiltration: the downward
movement of water through soil.
• Leaching: dissolving of minerals
and organic matter in upper layers
carrying them to lower layers.
• The soil type determines the
degree of infiltration and leaching.

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31. soil science By Allah Dad Khan

  • 2. Soil Science By Allah Dad Khan
  • 3. Soil Dirt is simply misplaced soil!
  • 4. SOIL: A RENEWABLE RESOURCE • Soil is a slowly renewed resource that provides most of the nutrients needed for plant growth and also helps purify water. – Soil formation begins when bedrock is broken down by physical, chemical and biological processes called weathering. • Mature soils have developed over a long time are arranged in a series of horizontal layers,soil
  • 5. Fig. 15-8, p. 343 Erosion Transportation Weathering Deposition Igneous rock Granite, pumice, basalt Sedimentary rock Sandstone, limestone Heat, pressure Cooling Heat, pressure, stress Magma (molten rock) Melting Metamorphic rock Slate, marble, gneiss, quartzite
  • 6. Layers in Mature Soils • Infiltration: the downward movement of water through soil. • Leaching: dissolving of minerals and organic matter in upper layers carrying them to lower layers. • The soil type determines the degree of infiltration and leaching.
  • 9. Soil Horizons • O horizon: leaf litter • A horizon: top soil • E horizon: eluviation zone; – eluviation is the lateral or downward movement of dissolved or suspended material within soil when rainfall exceeds evaporation, a.k.a. infiltration. – A & E horizons comprise the “zone of leaching” • B horizon: subsoil • C horizon: parent material • Bedrock
  • 10. Soil Profiles of the Principal Terrestrial Soil Types Figure 3-24Figure 3-24
  • 11. Fig. 3-24a, p. 69 Mosaic of closely packed pebbles, boulders Weak humus- mineral mixture Dry, brown to reddish-brown with variable accumulations of clay, calcium and carbonate, and soluble salts Alkaline, dark, and rich in humus Desert Soil (hot, dry climate) Grassland Soil semiarid climate) Clay, calcium compounds
  • 12. Fig. 3-24b, p. 69 Tropical Rain Forest Soil (humid, tropical climate) Acidic light-colored humus Iron and aluminum compounds mixed with clay
  • 13. Fig. 3-24b, p. 69 Deciduous Forest Soil (humid, mild climate) Forest litter leaf mold Humus-mineral mixture Light, grayish- brown, silt loam Dark brown firm clay
  • 14. Fig. 3-24b, p. 69 Coniferous Forest Soil (humid, cold climate) Light-colored and acidic Acid litter and humus Humus and iron and aluminum compounds
  • 16. All Soil is Brown, Right? • Wrong! Soils vary in color depending on material make-up and location. • The Munsell System of Color Notation is a color catalog. – Soil scientists compare the soil next to the color chips to find a visual match and assign the corresponding Munsell notation with the soil. • The wide use and acceptance of the Munsell System allows for direct comparison of soils anywhere in the world.
  • 17. The Munsell system The system categorizes by three components: hue, value, and chroma. •Hue: the specific color •Value: the lightness or darkness of color •Chroma: the light intensity •Written: Hue Value/Chroma •10 YR 3/2
  • 22. Soil Color Factors • Parent Material: Minerals relate to color • Age/Time: Older soil is often more red • Climate: May leach, remove coatings, or even enhance red • Topography: Uplands are more brown and red; low lands are more grey. • Vegetation : Conifers are more acid, more leaching, less color and Grasslands are more organic, darker colors
  • 23. Diversity of Color • All soil in a specific area is not all the same color. • Soil within the same soil profile can have strong color variation.
  • 24. What do the colors indicate? • Reddish, yellowish, or brownish: Iron oxides (variation from amount of:moisture) – Hematite – red – Goethite – yellowish brown – Ferrihydrite – reddish brown • White: Carbonates, gypsum, other salts, or very leached • Black/very dark brown: Organic matter • Purple/black: Manganese oxides
  • 26. Soil Color Variation A horizon: organic coatings B horizon: Iron coatings C horizon: little coating
  • 28. Colorful Soils •Red Soil in Southern U.S.
  • 29. Red Sands in Arizona
  • 31. •Green Soils & Sands in Maryland, New Jersey, & Hawaii Colorful Soils
  • 32. •White Sands in New Mexico
  • 33. Dark surface soils in the Great Plains & the Corn Belt are from rich organic matter. Hwang Ho River in China carries yellow sediment creating a yellow river bed.
  • 35. Surface Soil Rich in Organic Matter
  • 37. Particle Size Distribution (Texture) • Important for determining suitability for various uses • Considered a basic property because it doesn’t change
  • 38. Properties Related to Texture –Porosity –Permeability –Infiltration –Shrink-swell –Water holding Capacity –Erodibility
  • 39. Soil Separates • Most soils have a combination of soil particles sizes   – Sand – Silt – Clay
  • 40. Soil Particles • Soils vary in the size of the particles they contain, the amount of space between these particles, and how rapidly water flows through them. Figure 3-25Figure 3-25
  • 41. Sand • Gritty feel • Can be seen with the naked eye • Hand sampling: – No residue left on hand
  • 42. Silt • Dry: Powdery smooth feel, flour- like • Wet: Creamy slick, slippery feel • No sticky or plastic feel • Can be seen with a hand lens or microscope • Hand sampling: – Coats hand, able to brush off
  • 43. Clay • Dry: Hard feel • Wet: Sticky, plastic feel • Can be seen with an electron microscope • Hand Sampling: – Sticks to fingers
  • 44. Particle Sizes – Clay: less than 0.002 mm – Silt: 0.002-0.05 mm – Sand: 0.05-2 mm • 0.05-0.24 mm fine • 0.25-0.49 mm medium • 0.5-0.99 mm coarse • 1- 2 mm very coarse – Gravels: 2-75 mm – Cobbles:75-250 mm – Stones: 250-600 mm – Boulders: >600 mm
  • 46. Fine Textured Soil • Large amounts of silt and clay, making it "muddy" when wet  • Pore spaces are small, but numerous and hold more water • As clay soils begin to dry, they may still hold large quantities of water, but adhesive and cohesive properties of water make it unavailable for root uptake
  • 48. Coarse Textured Soil – Large pore spaces and allows water to easily run through it beyond the reach of roots – Drought-prone – Little surface area for the particle volume, reducing fertility
  • 50. Loamy Soil • A mix of sand, silt, and clay that optimizes agricultural productivity
  • 51. Sand + Silt + Clay = 100% Texture = CLAY LOAM 34 % Sand 33 % Silt 33 % Clay
  • 52. General Influence of Soil Separates on Properties and Behaviors of Soils Property/Behavior Sand Silt Clay Water holding Low Med-high high Aeration Good Med Poor OM decomposition Fast Med Slow Water erosion pot. Low High Low Compact-ability Low Med High Sealing (ponds) Poor Poor Good Nutrient supplying Poor Med-high High Pollutant leaching High Med Low
  • 53. Soil Texture and Surface Area • As particle size decreases, surface area increases – Clay has about 10,000 times as much surface area as sand • Surface area has a big effect on: – Water holding capacity – Chemical reactions – Soil cohesion – Ability to support microorganisms
  • 54. Influences of Soil Properties • Organic Matter is derived from decomposing plant and animal remains • Humus is the dark, moist layer found on the top of a soil profile. This is because it is made up of dead and decaying matter. It is fairly fertile in that the decay process adds nutrients to the soil
  • 55. Influences of Soil Properties • Parent Material: – Rock or original source of soil particles – Effects soil quality – Glacial outwash sands tend to be infertile, or hold few minerals and nutrients important for growth  – Soils derived from other sources may be relatively rich in minerals and nutrients – Usually a combination of weathered parent materials and organic matter make a soil
  • 56. Sources of Parent Material • Weathering or erosive actions: – heating/cooling – freezing/thawing – glaciers – water – wind – chemistry – plants & animals
  • 57. Other Uses of Soil • Native North American cultures used earth colors as body paints. • Modern American culture uses colored earth in cosmetics and ceramics and as pigments for paints.
  • 59. Porosity • A measure of the amount of pore space between grains; the ratio of the volume of openings (voids) to the total volume of material. Porosity represents the storage capacity of geologic material
  • 60. Permeability • A measure of the ability for fluid to pass through the pores.
  • 61. Wetlands- rich in humus and nutrients -Hydrology, Soil type, Species composition
  • 62. Pond Littoral zone has soil where rooted plants live (water lillies, cattails) Aides in reducing erosion
  • 64. Nutrients in Soil • Nutrients are chemical elements and compounds found in the environment that plants and animals need to grow and survive. – Nitrate (NO3-), – nitrite (NO2-), – ammonia (NH3), – organic nitrogen (in the form of plant material or other organic compounds), and – phosphates (PO4 3 -)(orthophosphate and
  • 65. MATTER CYCLING IN ECOSYSTEMS • Nutrient Cycles: Global Recycling – Global Cycles recycle nutrients through the earth’s air, land, water, and living organisms. – Nutrients are the elements and compounds that organisms need to live, grow, and reproduce. – Biogeochemical cycles move these substances through air, water, soil, rock and living organisms.
  • 66. The Big 13 • The 13 mineral nutrients, which come from the soil, are dissolved in water and absorbed through a plant's roots. There are not always enough of these nutrients in the soil for a plant to grow healthy. This is why many farmers and gardeners use fertilizers to add the nutrients to the soil. 
  • 67. Macronutrients: Primary Nutrients • Macronutrients are those elements and compounds needed in large quantities for a plant to grow. • The primary nutrients are nitrogen (N), phosphorus (P), and potassium (K). • These major nutrients usually are lacking from the soil first because plants use large amounts for their growth and survival. 
  • 68. Macronutrients: Secondary Nutrients • The secondary nutrients are calcium (Ca), magnesium (Mg), and sulfur (S). There are usually enough of these nutrients in the soil so fertilization is not always needed. – Large amounts of Ca and Mg are added when lime is applied to soils. – Sulfur is usually found in sufficient amounts from the decomposition of
  • 69. Micronutrients • Micronutrients are those elements essential for plant growth which are needed in only very small (micro) quantities and are sometimes called minor elements or trace elements. • Micronutrients include boron (B), copper (Cu), iron (Fe), chloride (Cl), manganese (Mn), molybdenum (Mo) and zinc (Zn).
  • 70. Soil pH is a factor • Soil pH (a measure of the acidity or alkalinity of the soil)  • Soil pH is one of the most important soil properties that affects the availability of nutrients.  – Macronutrients tend to be less available in soils with low pH. – Micronutrients tend to be less available in soils with high pH.
  • 71. The pH can be changed • Lime can be added to the soil to make it less acidic and also supplies calcium and magnesium for plants to use. – Lime also raises the pH to the desired range of 6.0 to 6.5.  In this pH range, nutrients are more readily available to plants, and microbial populations in the soil increase.
  • 72. Nitrogen • Nitrogen is a part of all living cells and is a necessary part of all proteins, enzymes and metabolic processes involved in the synthesis and transfer of energy. • Nitrogen is a part of chlorophyll, the green pigment of the plant that is responsible for photosynthesis.  • Nitrogen is usable in the forms of NO3 - , NO2 - , and NH3
  • 73. Where does N come from • Helps plants with rapid growth, increasing seed and fruit production and improving the quality of leaf and forage crops.  • Nitrogen often comes from fertilizer application whether it is industrial fertilizer or animal waste. • Bacteria can fix Nitrogen from the atmosphere (N2) into a more usable form. • Decomposition of organic matter puts nitrogen back into the soil.
  • 74. Phosphorus • Like nitrogen, phosphorus (P) is an essential part of the process of photosynthesis.  • Involved in the formation of all oils, sugars, starches, etc. • Helps with the transformation of solar energy into chemical energy; proper plant maturation; effects rapid growth; and, encourages blooming and root growth.
  • 75. Sources of Phosphorus • Phosphorus often comes from fertilizer, bone meal, and from rock. • Phosphorus is found in rock and is therefore a function of the rock cycle. – P is in limited supply and is often a limiting factor because the rock cycle is so slow! • Phosphorus also comes from bird guano.
  • 76. Potassium • Potassium is absorbed by plants in larger amounts than any other mineral element except nitrogen and, in some cases, calcium.  • Helps in the building of protein, photosynthesis, fruit quality and reduction of diseases. • Potassium is supplied to plants by soil minerals, organic materials, and fertilizer.
  • 77. Calcium • Calcium, an essential part of plant cell wall structure, provides for normal transport and retention of other elements as well as strength in the plant. It is also thought to counteract the effect of alkali salts and organic acids within a plant.  • Sources of calcium are dolomitic lime and gypsum
  • 78. Magnesium • Magnesium is part of the chlorophyll in all green plants and essential for photosynthesis. It also helps activate many plant enzymes needed for growth. • Soil minerals, organic material, fertilizers, and dolomitic limestone are sources of magnesium for plants.
  • 79. Sulfur • Sulfur is essential plant food for production of protein. It promotes activity and development of enzymes and vitamins; helps in chlorophyll formation; improves root growth and seed production; helps with vigorous plant growth and resistance to cold.
  • 80. Sulfur • Sulfur may be supplied to the soil from rainwater. It is also added in some fertilizers as an impurity, especially the lower grade fertilizers. The use of gypsum also increases soil sulfur levels. • The decomposition of organisms can add sulfur to the soil.  • Sulfur is used by plants in the form of sulfates (SO4 2- ) and sulfites (SO3 2- )
  • 81. Micronutrients Boron (B) • Helps in the use of nutrients and regulates other nutrients.  • Aids production of sugar and carbohydrates.  • Essential for seed and fruit development.  • Sources of boron are organic matter and borax Copper (Cu) • Important for reproductive growth. • Aids in root metabolism and helps in the utilization of proteins. 
  • 82. Chloride (Cl) • Aids plant metabolism.  • Chloride is found in the soil.  Iron (Fe)  • Essential for formation of chlorophyll. • Sources of iron are the soil, iron sulfate, iron chelate.  Manganese (Mn)  • Functions with enzyme systems involved in breakdown of carbohydrates, and nitrogen metabolism.  • Soil is a source of manganese.
  • 83. Other Tests • Percolation (permeability) • Organic matter • Salinity • Ion Exchange • Heavy and Trace Metals
  • 84. Soil Degradation The breakdown of our most important resource.
  • 85. Soil: The Final Frontier • Soil is a vital part of the natural environment. It influences the distribution of plant species and provides a habitat for a wide range of organisms. • It controls the flow of water and chemical substances between the atmosphere and the earth, and acts as both a source and store for gases (like oxygen and carbon dioxide) in the atmosphere.
  • 86. Soil: The Final Frontier • Soils not only reflect natural processes but also record human activities both at present and in the past. – They are therefore part of our cultural heritage. – The modification of soils for agriculture and the burial of archaeological remains are good examples of this.
  • 87. Without it, what would we do? • Soil helps to provide much of the food that humans consume. – Only 25% of the Earth’s surface is made up of soil and only 10% of that soil can be used to grow food. • I.E., without soil, we cannot support primary producers. – By the way, they are the base of the trophic levels!
  • 88. Major Causes of Soil Degradation • Overgrazing 35% • Deforestation 30% • Other Agricultural Activities 27% • Other Causes 8%
  • 89. Soil Exhaustion • Agricultural systems disrupt natural mineral cycling. – The soil may become mineral deficient and lose fertility. – Plants need minerals to grow and thrive such as nitrates, phosphates and sulfates.
  • 90. Soil Erosion • The removal of trees that stabilize slopes result in erosion. – Erosion is the removal of the top soil by physical means. – Deforestation is one of the major causes of soil erosion.
  • 91. Erosion from flooding • Floodplains and tropical rain forests are areas where there is a lot of erosion. – most concerns about erosion are related to accelerated erosion, where the natural rate has been significantly increased mostly by human activity
  • 92. Chemical Emissions • Industrial processes and vehicles release toxic substances which are heavier than air and settle on the soil. – PCB’s, Heavy metals
  • 93. Pesticides • Pesticides that are applied to fields can also destroy beneficial organisms in the soil. – Bacteria that fix nitrogen, organisms that break down soil (worms) – Bioaccumulation causes the concentrations of these pesticides to increase up the food chain. – In the United States, farmers rely heavily on pesticides to maximize crop output.
  • 94. Toxic Seepage and Chemical Contamination • Chemicals released into the environment from industrial discharges or improperly disposed chemicals seep into the soil and migrate or leach. – These chemicals can impact the aquifer as well as the soil.
  • 95. Brownfields • A Brownfield is underused or abandoned industrial site that is available for re-use that may or may not be contaminated – Contamination would be mostly in the soil and due to the previous industrial process • Heavy metals, organic by-products, acidic soil, etc.
  • 96. Salinization • Salinization is an increase in salt (ionic compounds) in soil. Irrigation in areas where the bedrock contains high salt levels will cause these aqueous salts to be brought to the surface. – This problem is compounded by clearing native vegetation. – Irrigation of farmland and deforestation has in Western and South Eastern Australia has caused widespread salinization.
  • 97. Desertificaion • Desertification is the expansion of dry lands due to poor agricultural practices, improper soil moisture management, salinization and erosion, forest removal, and climate change. – Overuse of agricultural lands is the cause. – 10% of the world’s land has been desertified. – 25% is at risk. – In Mali, the Sahara desert has expanded more than 650 km in less than 20 years.
  • 98. Desalination • Desalination is used to remove ions from water. – The Middle East has the least amount of freshwater than any other area on the planet and desalination is used to provide freshwater for agricultural and household purposes. This prevents salinization of the soil through agriculture.
  • 100. Contaminated Soil Cleanup• Site cleanup depends upon the pollutant – Acid = neutralization – Heavy metals = chelation, de- toxification – Organic solvents = incineration – Other = secure landfill – Electrokinetic separation removes metals and organic contaminants from low permeability soil, mud, sludge, and marine dredging
  • 101. Remediation • Biological organisms can be used to clean up – Phytoremediation uses plants to remove pollutants from the soil; as the soil takes up water through the root systems, it takes up the pollution and incorporates it into the plant tissue. – Bioventing introduces air into the soil which promotes biodegradation
  • 102. Conservation • What is soil conservation? – The protection of soil against erosion or deterioration • How can we do that?
  • 103. The Laws • The U.S. Soil Conservation Act of 1935 established the Soil Conservation Service.  – This agency deals with soil erosion problems and was enacted following the Dust Bowl. • Soil & Water Resources Conservation Act of 1977 – This Act provides for a continuing appraisal of U.S. soil, water and related resources, including fish and wildlife habitats, and a soil and water conservation program to assist landowners and land users in furthering soil and water conservation
  • 104. Agricultural Methods • No-till or minimum tillage methods protect the top soil • Shaping of the land decreases runoff • Windbreaks prevent erosion from wind • Crop rotation prevents nutrient depletion
  • 105. Aquatic Protection • Protection along riparian zone – Riprap • Lake zones with emergent plants protect sediment (littoral zone) • Wetlands are characterized by the type of soil present, the hydrology and the species of flora and fauna
  • 106. Alternative Irrigation • Drip irrigation methods deliver water directly to the plant which – Reduces water loss through evaporation – Increases crop yield and efficiency – Reduces erosion potential – Protects the top soil
  • 107. What have we done at JF? • Rain gardens and fast growing plants to secure the top soil and prevent erosion into the James River