Meaning of conservationList the ways nutrients are lost in the soil 2. Enumerate factors that determine the degree of nutrient losses 3. Explain the meaning of erosion and describe the types of erosion 4. Outline the various preventive and control measures of erosion. 5. List the ways through which soil water is lost. 6. Enumerate the ways through which soil water loss can be prevented.
Meaning of conservation Conservation is regarded as planned use of any natural resources In avoid exploitation, neglect and destruction. Soil conservation is the use of soil without waste so as to sustain higher crop production M yield. It is aimed at preventing waste of the soil and depletion of its
SOIL AND WATER CONSERVATION
The students should be able to 1. List the ways nutrients are lost in the soil 2. Enumerate factors that determine the degree of nutrient losses 3. Explain the meaning of erosion and describe the types of erosion 4. Outline the various preventive and control measures of erosion. 5. List the ways through which soil water is lost. 6. Enumerate the ways through which soil water loss can be prevented.
Meaning of conservation Conservation is regarded as planned use of any natural resources In order to avoid exploitation, neglect and destruction ofc soil. Soil conservation is the use of soil without wasting it so as to sustain higher crop production yield. in reality conservation is aimed at preventing waste of the soil and depletion of its nutrients. Soil conservation is important because plants .depend on nutrients in the soil. Animals indirectly depend on the soil for their feed. It is the soil that provides the medium for plant growth development and hence the sustenance of life.
5. Oxidation and reduction
These are used by man for food and other purposes. The nutrients taken up by plants are lost completely from the soil. This is because the harvested parts of crops are not returned to the soil through decay.
(c) burning: The burning of vegetation reduces soil fertility. This is because it exposes the surface of the soil to the agents of erosion such as water and wind. Soil micro-organisms of agricultural importance are killed during burning. There is also break down of volatile nutrients like sulphur and nitrogen.
(d) effect of soil erosion to conservation of land and nutrient
The factors are:
The roots of plants help to bind soil particles. The temperature of the soil is also regulated as a result of the cover. Above all, the dead vegetative cover crop adds organic matter to the soil, which is a major source of plant food. Where the soil lacks vegetative cover, it is exposed to wind and water that can carry away soil particles and nutrients. Micro-organisms in the soil are reduced because of lack of organic matter. The soil is subjected to wide temperature fluctuation.
(d) Cultivation practices: Continuous cropping leads to exhaustion of soil nutrients while over tillage exposes the soil to easy erosion hy water and wind. 3.2 Soil erosion Erosion is the removal or wearing away of the surface soil by different agents. These agents are: 1. Water 4. Ice 2. Wind 5. Man. 3. Animals However, water is the major agent of erosion in Nigeria. The process of erosion involves three stages. These detachment of soil particles, transportation and deposition.
Types of soil erosion
There are four types of soil erosion depending on how they occurs. These are: 1. Splash or raindrop erosion. 2. Sheet erosion. 3. Rill erosion. 4. Gully erosion. (a) Splash or raindrop erosion: This is the first stage of the erosion caused by rainfall. It is the removal of soil particles by llu lime til raindrops. The soil particles scattered by raindrops block the soil pores. This will make it difficult for the rain water to the soil. The result is that the water will begin to flow gradually on the surface of the soil. (b) Sheet erosion: Sheet erosion follows splash. It occurs when lamdrops cause soil particles to block soil pores. Rain water then flows slowly over the soil surface. The soil particles are then removed or carried away evenly. This can also be caused by wind. The wind blowing over the soil that is exposed can carry away soil particles uniformly and deposit them somewhere else": (c) Rill erosion: Sheet erosion develops into rill erosion. This occurs when raindrops on the soil surface cause gradual removal of soil particles in suspension along narrow channels. The channels may be existing before^They could be caused by the rain water itself. The size of the "channels, or rills becomes larger because of downward cutting. This eventually leads to gully erosion. (d) Gully erosion: Channels that cannot be smoothened out by ordinary cultivation are referred to as gullies. Gully erosion takes place when rain water does not sink into the soil, it therefore runs off over the land.
The soil panicles being carried by the rain water help to cut deeper and deeper into the soil. Sudden drop in slope or channel increases the cutting power of the water. Where the land is very sloppy and the soil loose, large gullies are easily formed. 2. Prevention and control of erosion Prevention and control of erosion can be achieved through the following practices: (a) Covering the land with vegetation: Covering the soil with plants prevent the soil from being exposed to agents of erosion such as water and wind. The planting of cover crops is to maintain adequate ground cover. Soil fertility is also increased because of leaf fall. Water infiltration is encourage and run-off is reduced because of the vegetative cover. (a) Crop rotation: A well designed crop rotation ensures that the land is always protected against erosion. Where legumes are included in the rotation, they help to control erosion because they Mirad over the soil surface.
(c) Application of organic and inorganic manures: The addition of compost and farm yard manures make the soil cohesive and absorb water.' They also add plant nutrients to the soil. The addition of lime fertilizers such as calcium triococarbonate (IV) to the soil causes loose soil particles to be bound together. This improves the structure of the soil and the soil cannot be carried a|way easily whether by water or wind. (d) Mulching: This involves covering the soil with mulch materials such as papers, grasses and stones. It prevents direct contact between the soil and raindrops. Mulching increases water infiltration and reduces sheet erosion. Where mulching is done with plant materials, organic is added to the soil. This helps to bind loose soil particles together.
(e) Preventing bush burning: Setting the bush on fire destroys fertility of the soil. During bush burning, organic matter and many agriculturally important living organisms are destroyed. The soil is therefore exposed to agents of erosion. Where bush burning is avoided, the organic matter and micro-organisms present help to improve the soil structure and control erosion. (f) Preventing overgrazing: Overgrazing of pasture or field could occur if animals are allowed to remain for a long time on the same land.
Almost every vegetation in such a place is eaten up stud will not have time to grow again. Such land is exposed to piosion agents. The feet of animals also destroy soil structure and cause the formation of hard layers or hard pans below the soil surface. This makes infiltration difficult and increases surface run-off. Overgrazing by farm animals should therefore be avoided. (g) Establishment of wind breaks: The planting of trees prevents pitision by acting as wind breaks.
This is a good erosion pirvciitive measure especially in the Savannah regions and where the soil is sandy. (h) Contour strip cropping: This involves the growing of close ginning plants such as grasses and row crops such as maize in alternate strips across the slope of the land. This ensure adequate cover for the land. It therefore reduces the speed of moving water and its load. DIAGRAM Figure 2.3.1: Contour Strip Cropping (i) Terracing: These are embankments constructed across the slope at regular interval to conduct water from the land in such a way as to keep erosion under control. They reduce the length of slope thaT may aid erosion. Terraces are built in form of steps along the contour of the land or across the slope. DIAGRAM Figure 2.3.2: Level Bench Terrace (j) Ridging: The construction of ridges during land preparation cross or tied ridges helps to control soil erosion. Ridges enhance water absorption by the soil and this reduces the speed of run-off. (k) Construction of contour bunds: The construction of ridges called bunds across the slope prevents soil elusion. Tliccorrtor bunds prevent water run-off down the slopes. (l) Errection of barriers: Barriers can he created at intervals in gullies to reduce the speed of water run-off. Dams of earth blocks, concrete or stones can be used to fill gullies already created. These help to trap sediments which eventually fill the gullies. Wire netting can also be stretched across gullies. This helps lo trap grasses, soil and debris which graduallyblock the gullies. 3. Problems created by soil (a) Erosion reduces the nutrient content of the soil. As soil particles are detached and earned away by the agents of erosion, the nutrients are dissolved and washed away by water. This renders the soil infertile, resulting in poor crop yield. (b) Erosion washes away crops. Crops planted in farms are at times uprooted and carried away by agents such as water. This is very MM ions where the farmland is slopy. (c) Erosion leads to soil destruction. Frosion involves the ilHachment and transportation of soil particles from one area to another. The top soil which supports crops is gradually removed. The subsoil left can also be broken into gullies making the land useless. (d) The soil particles detached by erosion are deposited in rivers, reservoirs and dams. This results in water pollution and shortages. The soil particles can also be deposited on crops. (e) The farmer spends time, labour and money to control erosion once it has occurred. This increases his cost of production, thus lowering his marginal profit. (f) The water responsible for the erosion is lost. The water is no longer available for crop use. . 4. Loss of soil water Water is lost in the soil through many ways. These include:
(a) Transpiration: This is the loss of water vapour through the leaves of plants. The water is absorbed by the roots of plants and is then transported through the stem to the leaves. High temperature and wind increase the rale of water loss through inspiration. (b) Transportation: This is the process whereby water leaves the soil surface into the atmosphere in form of vapour. As a result of heat. water changes form into vapour. The amount of water loss through evaporation depends on the temperature, wind, humidity and vegetative cover of the environment.
(c) Crop removal: The roots of crops absorb water from the soil. The water is used by the crops for development and production. the water taken up by crops from the soil is lost for ever as it is never returned to it again.
(d) Seepage or percolation: This is the-down-ward movement of water through the soil. Soil water moves by infiltration from one layer to another. The water gradually goes into wells and under¬ground water.
(e) Run-off: The soil at times finds it difficult to absorb excess water. The excess water is removed from the soil when it flows over the land into streams, rivers and other natural water ways. The water is lo»t from the soil for ever.
(f) Burning: Setting the farmland on fire to remove trashes contributes to soil water loss. Fire dries up moisture-from the dipper layer of the soil as a^result of the heat generated. The 'water cannot return to the soil again. Preventing loss of soil water Soil water loss can be prevented or minimized by carrying out the following practices:
(a) Maintaining vegetatiVe cover. 'Covering the land with plants presents excessive drying of the soil. It also prevents direct evaporation of soil water.
(b) Good cultivation methods: This involves tillage.
Tillage encourages the soil to absorb water and prevents run-off Contour ridging or ridging across slopes helps to reduce water movement down the slope and thereby encourages infiltration.
(c) Use of organic manure: This refers to the addition of farm yard, compost or green manures to the soil. These provide cover for the soil. Organic manures bind soil particles together and enable the soil to hold water.
(d) Controlled burning practice: The burning of the farm during land preparation should be done when no other way of disposing off farm trashes is available. This should be limited to areas where burning is very necessary.
(e) Mulching: The use of mulch materials to cover heaps, beds and ridges helps in conserving soil water, evaporation and excessive drying by the sun.
(f) Terracing: This helps to reduce the length of slopes and decreases run-off. Water infiltration is thn encouraged.
(g) Use of wind break” The planting of trees protects the soil against excessive drying by the sun and strong wind. The trees produce cooling effect on the soil.
(h) Regular weeding: The removal of weeds from the farm reduces unnecessary transpiration. Enough water is therefore conserved for crop use.
(i) Breeding drought resistant crops: The development of crops that use little water will enable the soil to retain most of its water.
(j) Strip cropping: This involves the growing in alternate strips of different crops in the same field. It ensures that the entire land area is not empty at the same time.
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HERE YOU WILL FIND EVERY AVAILABLE TOPICS ABOUT AGRICULTURAL SCIENCE AND BIOLOGY. AND THE LINKS TO THEIR VARIOUS SOURCES.
1. DEVELOPMENT OF AGRICULTURE
2. IMPORTANCE OF AGRICULTURE
3. SUBSISTENCE AGRICULTURE
4. COMMERCIAL AGRICULTURE
5. PROBLEM OF AGRICULTURAL DEVELOPMENT
6. SOLUTIONS TO POOR AGRICULTURAL DEVELOPMENT
7. AGRICULTURAL LAWS AND REFORMS
8. ROLES OF GOVERNMENT IN AGRICULTURAL DEVELOPMENT
9. AGRICULTURAL POLICIES
10. PROGRAM PLANNING IN AGRICULTURE
35. WILDLIFE CONSERVATION
36. FACTORS AFFECTING LAND AVAILABILITY
39. BIOLOGICAL FACTORS
40. SOCIAL-ECONOMIC FACTORS
41. ENVIRONMENTAL FACTORS AFFECTING AGRICULTURAL PRODUCTION
42. CLIMATIC FACTORS AFFECTING AGRICULTURAL PRODUCTION
47. SOLAR RADIATION
48. BIOTIC FACTOR AND AGRICULTURAL PRODUCTION
52. SOIL MICRO-ORGANISMS
53. SOIL PH
54. ROCK FORMATION
55. IGNEOUS ROCK
56. SEDIMENTARY ROCKS
58. SOIL AND ITS FORMATION
59. FACTORS OF SOIL FORMATION
60. LIVING ORGANISM
61. PARENT MATERIALS
62. SOIL FORMATION TOPOGRAPHY
63. PROCESS OF SOIL FORMATION
65. PHYSICAL WEATHERING
66. CHEMICAL WEATHERING
73. BIOLOGICAL WEATHERING
74. CHEMICAL AND BIOLOGICAL COMPOSITION OF THE SOIL
75. SOIL WATER
76. MICRO AND MACRO NUTRIENTS
77. SOIL MICRO ORGANISM
78. PROPERTIES OF SOIL
79. SOIL STRUCTURE
80. SANDY SOIL
81. CLAY SOIL
82. LOAMY SOIL
83. SOIL TEXTURE
84. IDENTIFICATION OF SOIL TYPES THROUGH EXPERIMENTS
85. RETENTION OF WATER BY VARIOUS SOIL TYPES
86. DETERMINATION OF SOIL PH REACTION
87. COLORIMETRIC DETERMINATION OF SOIL PH LEVELMeaning of conservation
88. PH SOIL TEST
89. PLANT NUTRIENTS
90. MACRO NUTRIENTS IN GENERAL
112. THE MAINTENANCE OF SOIL FERTILITY
113. CROP ROTATION
114. APPLICATION OF ORGANIC MANURES
115. FARM YARD MANURE
116. APPLICATION OF INORGANIC MANURE
118. FARMING PRACTICES
119. BUSH BURNING
121. FERTILIZER APPLICATION
122. ORGANIC MANURING
123. FARM YARD MANURE
126. CROP ROTATION
133. FARM POWER AND MACHINERY
134. SOURCES OF FARM POWER
135. HUMAN SOURCE
142. FIELD MACHINES
164. SIMPLE FARM TOOLS
165. AGRICULTURAL MECHANIZATION
166. THE CONCEPT OF MECHANIZATION