LAND DEGRADATION AND THEIR RESTORATION TECHNOLOGY.pptx

LAND DEGRADATION AND THEIR RESTORATION TECHNOLOGY.pptx

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  LAND DEGRADATION AND THEIR RESTORATION TECHNOLOGY PRESENTEDBY: Sai Suman Bhuyan(2241901046) Submitted to: Dr. Suchismita Mohapatra (DEPT. SOIL SCIENCE AND AGRICULTURE CHEMISTRY)
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  CONTENT: ▪ Land degradation ▪Indian scenario ▪ Types of land degradation ▪ Methodologies of land degradation ▪ Procedure ,Assessment ,Classification , Factors ▪ Land restoration ▪ Methods used in land restoration and revegetation ▪ Explanatory video of land degradation scenario ▪ Conclusion ▪ References
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  LAND DEGRADATION ▪ Landdegradation can be considered in terms of the loss of actual or potential productivity or utility as a result of natural or anthropic factors; it is the decline in land quality or reduction in its productivity. ▪ In the context of productivity, land degradation results from a mismatch between land quality and land use (Beinroth et al., 1994). ▪ Mechanisms that initiate land degradation include: 1. Physical processes 2. Chemical processes 3. Biological processes (Lal, 1994). SOURCE-https://www.sciencedirect.com/topics/agricultural-and-biological.../land- degradation
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  ▪ Physical processesare a decline in soil structure leading to crusting, compaction, erosion, desertification, anaerobism, environmental pollution, and unsustainable use of natural resources. ▪ Chemical processes include acidification, leaching, salinization, decrease in cation retention capacity, and fertility depletion salinizatio n crustin g
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  LAND DEGRADATION population and one-quarterof the world's land, and salinization affects some 20 million hectares of irrigated land. ▪ India losing 5334 million tonnes annually .(THE HINDU 2010) SOURCE-https://www.researchgate.net/figure/Information-needs-of-farmers-through-the- Continent Total area Degraded area † % degraded Africa 14.326 10.458 73 Asia 18.814 13.417 71 Australia and the Pacific 7.012 3.759 54 Europe 1.456 0.943 65 North America 5.782 4.286 74 South America 4.207 3.058 73 Total 51.597 35.922 70
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  Indian Scenario ofland degradation: Types of land degradationArea in million hectares Water eroded 111.26 Wind eroded 38.74 Water logged 6 Alkali soils 2.50 Saline soil 2.50 Ravine and gullies 3.97 Shifting cultivation 4.36 Riverine 2.73 Total problem area 175.06 Total geographical area 347.12 Source –forest survey of
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  IMAGE SOURCE-BHU
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  Source-icar webpage/https://icar.org.in/node/8099
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  Methodology of Land Degradation ▪Land information system should consist of RS, GIS and modeling, which can be expressed as following formula: ▪ Spatial data + Statistical data + Attribute data + Modeling Source-FAO. 1976. A Framework For Land Evaluation. FAO Soil Bulletin No. 32. ILRI Publication
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  Procedure of Assessmentof Land Degradation: 1. Comprehensive Land Type Mapping, Land Cover and Vegetation Index Study 2. Land Characteristics Data Base Construction based on Land Type Mapping Units. 3. Land Information System (LIS) Construction: Maps are digitized within ARC/INFO,ILWIS or other environment 4. Set up an applied Land Information System: Land Type Units, integrated with land cover and vegetation index, are compared with land degradation classification systems. 5. Reinterpretation of Land Type Map into Land Degradation Map: Extraction, Integration and Conversion of the Spatial (polygon etc.) data e.g. for the Land Degradation Map Reproduction. 6. Conversion and Reconstruction of Statistic data. 7. As the map and land inventory are produced, then sustainable land use planning can be carried on. SOURCE-FAO. 2004. A Framework For Land Evaluation. FAO Soil Bulletin
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  Land Degradation Classification Systems: ▪Land degradation classification system must include : 1. Degradation Types 2. Degrees within each type 3. Degradation units
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  1.Degradation Types ▪ Thereare four kinds of land degradation recognized: 1. Desertification (D), 2. Soil Erosion (E), 3. Secondary Salinization (S) and 4. Wasted Land (W). ▪ (There must also be some transition areas influenced by two or three factors that is remarked with two Letters such as DE) Source-Beek, K J. 1980. From soil survey interpretation to land evaluation. ILRI Reprint No. 15. Reprinted from Land Reclamation and Water Management , Publication no. 27, ILRI, Wageningen, The Netherlands
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  2.Degradation Classes ▪ Theclasses are numbered in Arabic numbers, with increasing degrees of degradation within the type, for example, D1, D2, E1, ...,E5 etc. ▪ Class 1 ▪ Class 2 ▪ Class 3 ▪ Class 4 ▪ Class 5 potential degradation, but no evidence or improved. light degradation, mainly vegetation quality degraded so that its utilization value is reduced. moderate degradation, vegetation, and /or soils are influenced. severe degradation, vegetation, soils and landform are strongly influenced so that land use had to be changed from former practice. very severe degradation, land lost its productivity and is very difficult to reclaim. 3.Degradation Units ▪ They are indicated as land type units, e.g. D1A22, E3H24.
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  Land Degradation Factors: 1. Soilerodibility (e) 2. Slope degree(p) 3. Farming land use (f) 4. vegetation type and vegetation coverage (v)
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  Types of landdegradation Assessed: Land degradation have been grouped into six classes: ▪ 1.Water erosion ▪ Water erosion covers all forms of soil erosion by water, including sheet and rill erosion and gullying. Human-induced intensification of land sliding, caused by vegetation clearance, road construction, etc., is also included. ▪ 2.Wind erosion ▪ It refers to loss of soil by wind, occurring primarily in dry regions.
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  ▪ 3.Soil fertilitydecline ▪ Decline in fertility is indeed a major effect of erosion, the term is used here of cover effects of processes other than erosion. The main processes involved are: i. Lowering of soil organic master, with associated decline in soil biological activity; ii. degradation of soil physical properties (structure, aeration, water holding capacity), as brought about by reduced organic master; iii. adverse changes in soil nutrient resources, including reduction in availability of the major nutrients (nitrogen, phosphorus, potassium), onset of micronutrient deficiencies, and development of nutrient imbalances. iv. buildup of toxicities, primarily acidification through incorrect fertilizer
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  ▪ 4.Waterlogging ▪ ItIs the lowering in land productivity through the rise in groundwater close to the soil surface. Also included under this heading is the severe form, termed ponding, where the water table rises above the surface. ▪ 5.Salinization ▪ It is used in its broad sense, to refer to all types of soil degradation brought about by the increase of salts in the soil. ▪ 6.Lowering of the water table ▪ It is a self-explanatory form of land degradation, brought about through tube well pumping of groundwater for irrigation exceeding the natural recharge capacity. This occurs in areas of non-saline ('sweet') groundwater. Pumping for urban and industrial use is a further cause.
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  Other types ofdegradation included Further classes are recognized as types of land degradation:- ▪ Forest degradation :-This is the reduction of biotic resources and lowering of productive capacity of forests through human activities. ▪ Rangeland degradation:- This is the lowering of the productive capacity of rangelands.. ▪ Acid sulphate formation: a serious but localized form of degradation, which may occur on drainage of coastal swamps ▪ Soil pollution, from industrial or mining effluents:- to the atmosphere, rivers or groundwater. This is an important concern in the region, but is strongly
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  LAND RESTORATION: ▪ Landrestoration is the process of ecological restoration of a site to a natural landscape and habitat, safe for humans, wildlife, and plant communities. ▪ Land restoration is not the same as land reclamation, where existing ecosystems are altered or destroyed to give way for cultivation or construction. ▪ Land restoration can enhance the supplyof valuable ecosystem services that benefit people.
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  RESTORATION TECHNOLOGY 1. Improvementin soil organic carbon pool ▪ Crop yields can be increased by 20–70 kg ha−1 for wheat, 10– 50 kg ha−1 for rice, and 30–300 kg ha−1 for maize with every 1 Mg ha−1 increase in soil organic carbon pool in the root zone. ▪ Adoption of recommended management practices on agricultural lands and degraded soils would enhance soil quality including the available water holding capacity, cation exchange capacity, soil aggregation, and susceptibility to crusting and erosion. Increase in soil organic carbon pool by 1 Mg ha−1 y−1 can increase food grain production by 32 million Mg y−1 in developing countries. Source-
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  PEATLAND RESTORATION: ▪ Organicor peaty soils accumulated large quantities of carbon due to anaerobic decomposition of the organic matter. Anaerobic decomposition, or decomposition under absence of oxygen, occurs due to the flooded conditions of peatlands. ▪ When converted to agricultural lands the soils are drained, which removes the anaerobic conditions as it introduces oxygen into the soil. ▪ This process favours aerobic decomposition (decomposition with oxygen) which results in high CO2 and N20 fluxes (IPCC, 2007).
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  METHODS USED INLAND RESTORATION AND REVEGETATION ▪ a) On cultivated land: 1. Agro-silvicultural methods ▪ These are practiced to restore the soil fertility. The traditional system under rainfed conditions, is to restore the lost fertility through bush fallow system. Vegetation, mainly bushes, colonise the area naturally. Example: Acacia senegal
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  ▪ 2. Shelterbelts ▪These are used to protect both irrigated and rainfed farms. Their main function, at present, is to protect valuable agricultural land and irrigation canals from creeping sands. ▪ Shelterbelts reduce wind velocity, improve the microclimate and increase yields. ▪ Field investigations in dry areas show that crop production may be increased by as much as 300% while the increase in average years is often 30 to 50%. ▪ Mostly Eucalyptus, Casuarina sp., populus and prosop is. Seedlings are used for establishment.
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  ▪ 3. Plantationson seriously degraded irrigated or rainfed crop land ▪ Salinization is of common occurrence in irrigated lands, plantations of eucalyptus were established in some of these degraded lands to bring them back to production. ▪ The product is to be used to establish wood-based industries. ▪ Eucalyptus, microtheca plantations are established on such sites.
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  ▪ C) OnBare land: sand and sand-dune fixation: ▪ When erosion reaches an acute level, and where sand starts to move and threatens habitations, establishments, roads and agricultural land, sand-dune fixation is carried out. ▪ This occurs along the coasts of seas and oceans or in continental areas. ▪ The conventional method used is the establishment of hedges of stalks of dry grass and/or bushes to restrain temporarily sand movement until the dunes are planted with trees, shrubs and grasses. ▪ Eucalypts, pines, and acacias are used.
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  ▪ (ii) Activeintervention methods: ▪ These require the actions of man to restore the degraded land and vegetation. ▪ a. Sand and sand-dune fixation through artificial sowing of plants including tree, shrub and grass species. ▪ b. Establishment of shelterbelts on irrigated and rainfed cultivated land, and for protection of habitations and infrastructures. ▪ c. Establishment of plantations on degraded lands, especially on irrigated degraded lands (salinity and waterlogging). These offer a great potential for generation of wood-based industries in dry lands. ▪ d. Establishment of tree, shrub and grass plantations of value to restore the fertility of degraded lands where soil fertirainfed cultivation is practiced (use of Acacia and leguminous plants to restore lity).
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  ▪ Use oforganic farming techniques: Organic farming techniques that help restore the soil include use of green manure (uprooted or sown crop parts incorporated or left on topsoil), cover crops, crop rotation and organic compost. A)Green manure and cover crops: ▪ Green manures and cover crops serve as mulch to the soil preventing the soil from wind/water erosion and moisture loss. ▪ They also increase the soil organic matter content as they decompose in the soil. ▪ Green manure and cover crops that are legumes (plants which produce seeds in pods) have nitrogen fixing ability. The nitrogen fixing bacteria in their root nodules help capture nitrogen from the atmosphere. ▪ Green manure and cover crops suppress weed growth.
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  B) Organic compost: Compostis a mixture of decomposed plant parts and animal waste. ▪ The key benefit of composting is that it increases soil organic matter content. ▪ Organic matter improves the soil fertility, the soil structure and its water holding capacity. ▪ It also sequesters carbon in the soil. C) Crop rotation: This is a farming practice which involves growing different types of crops in one location sequentially. This practice reduces soil erosion, increases the soil fertility and subsequently crop yield.
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  D)Soil remediation: Soil remediation involvesthe removal of harmful contaminants such as, heavy metals, sewage sludge, coal tar, carcinogenic hydrocarbons, liquors and petroleum from soils. Soil remediation can be achieved using biological techniques. This method is called bioremediation. Some examples of bioremediation techniques include: ▪ • Phytoremediation: The use of plants to remove contaminants from soils or to degrade contaminants to a lesser toxic form. Some plants have the ability to extract contaminants from soils. This process is called phytoextraction. ▪ The willow (Salix viminalis) is a shrub credited for its ability to extract cadmium from soils. ▪ . Phyto-extraction is one technique in phytoremediation. Some other techniques are phyto-stabilization, phyto-transformation and phyto- stimulation.
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  ▪ • Bioaugmentation: ▪This is the introduction of genetically modified micro organisms into contaminated soils with the aim of degrading contaminants. ▪ The efficiency of this technique depends on a number of factors, some of which are the physico-chemical properties of the soil and the ability of the introduced micro organisms to compete successfully with the indigenous soil microflora ▪ Land-based treatments: ▪ This includes techniques like land farming and composting. In land farming, contaminated soils are taken to land farming sites and continuously overturned and tilled to allow aeration. In composting, micro organisms present in organic material are used to biodegrade soil contaminants.
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  ▪ Desalinization: ▪ Soilsalinization occurs when high levels of soluble salts accumulate in the root zone. Saline soils frustrate crop growth and reduce crop yield. Soil salinization is encouraged by • Formation from parent materials with high salt content • Low rainfall in arid regions where there is insufficient water to leach salts • Poor soil drainage system • Excessive exposure of soil to salty irrigation water or chemicals Some methods used to restore saline soils are: ▪ • Installing drainage systems to wash salts down the soil profile (this method is expensive and complicated). ▪ • Leaching out saline soils by applying water to contaminated soils to wash salts beyond the root zone.
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  ▪ • Useof salt tolerant plants (halophytes) as bio- remediants:- ▪ Halophytes accumulate salts in their shoots and other aerial plant parts. Examples include 1.Allenrolfea occidentalis (iodine bush), 2.Salicornia bigelovii (dwarf saltwort), 3.Panicum virgatum (switch grass),4. Sesuvium portulacastrum (sea purslane). • Application of gypsum (calcium sulphate dehydrate) to sodic soils. Sodic soils have high content of sodium chloride. Gypsum mixed into the layers of sodic soils replaces sodium with calcium, reducing the sodium level
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  CONCLUSION ▪ 1. Morethan 6-7 million hectare of land are degraded annually and increasing per year due to improper management and ever increasing demand and increasing population which should be controlled with proper restoration technology and creating awareness towards land use planning. ▪ 2.Traditional methods of restoration can be used for small area to restore land . ▪ 3. Large effected degraded land are hard to restore and are much more expensive. FINAL REMARK-ITS BETTER TO TAKE CARE OF SOIL AND LAND BEFORE ITS GET LATE TO RECOVER.
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  ▪ Ayyad, M.A.Soil - vegetation - atmosphere interactions. In arid-land (1981) ecosystems Vol. 2, pp. 9-31, Cambridge University Press. Cambridge, U.R. ▪ Ben Salem, 8. and Eren T.M. Forestry in A Sandy World. (1982) Unasylva, Vol. 34 No. 135, pp. 8-12, FAO, Rome. ▪ Grainger, A. Desertification. Earthscan - International Institute for (1984) Environment and Development - IIED, London. Second edition. ▪ Image source:- ▪ Icar/bhu/google webpage ▪ Video source :–