Lecture no. 5 Drought and its management
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The document discusses various types of drought, their definitions, and impacts on Indian agriculture, emphasizing the reliance on monsoon rains for crop irrigation. It categorizes drought based on duration, relevance to users, occurrence time, and other terms, while detailing the physiological and morphological effects of drought on plants. Additionally, strategies for crop adaptation, mitigation practices, and specific drought-resistant varieties and agronomic approaches are outlined to combat the adverse effects of water scarcity on agriculture.
Lecture no. 5 Drought and its management
- 1. Drought: types, effect of water deficit on physio-morphological characteristics of the plants, Crop adaptation and mitigation to drought Prepared by: Dr Pooja Goswami Assistant Professor (Agronomy) College of Agriculture Balaghat(M.P.)
- 2. Drought Definition of drought There is no universally accepted definition for drought. a) Early workers defined drought as prolonged period without rainfall. b) According to Ramdas (1960) drought is a situation when the actual seasonal rainfall is deficient by more than twice the mean deviation. c) American Meteorological Society defined drought as a period of abnormally dry weather sufficiently prolonged for lack of water to cause a severe hydrological imbalance in the area affected.
- 3. DROUGHTS IN INDIA Drought in India has resulted in tens of millions of deaths over the course of the 18th, 19th, and 20th centuries. Indian agriculture is heavily dependent on the climate of India: a favorable southwest summer monsoon is critical in securing water for irrigating Indian crops. In some parts of India, the failure of the monsoons result in water shortages, resulting in below-average crop yields. This is particularly true of major drought-prone regions such as southern and eastern Maharashtra, Karnataka, Haryana , Gujarat, and Rajasthan. In the past, droughts have periodically led to major Indian famines, including the Bengal famine of 1770, in which up to one third of the population in affected areas died; the 1876–1877 famine, in which over five million people died; and the 1899 famine, in which over 4.5 million died.
- 5. Classification of drought: Drought can be classified based on duration, nature of users, time of occurrence and using some specific terms. 1. Based on duration a. Permanent drought: This is characteristic of the desert climate where sparse vegetation growing is adapted to drought and agriculture is possible only by irrigation during entire crop season. b. Seasonal drought: This is found in climates with well- defined rainy and dry seasons. Most of the arid and semiarid zones fall in this category. Duration of the crop varieties and planting dates should be such that the growing season should fall within rainy season.
- 6. Continued…. c. Contingent drought: This involves an abnormal failure of rainfall. It may occur almost anywhere especially in most parts of humid or sub humid climates. It is usually brief, irregular and generally affects only a small area. d. Invisible drought: This can occur even when there is frequent rain in an area. When rainfall is inadequate to meet the evapo-transpiration losses, the result is borderline water deficiency in soil resulting in less than optimum yield. This occurs usually in humid regions.
- 7. 2. Based on relevance to the users (National Commission on Agriculture, 1976) a) Meteorological drought: It is defined as a condition, where the annual precipitation is less than the normal over an area for prolonged period (month, season or year). b) Atmospheric drought: It is due to low air humidity, frequently accompanied by hot dry winds. It may occur even under conditions of adequate available soil moisture. It refers to a condition when plants show wilting symptoms during the hot part of the day when transpiration exceeds absorption temporarily for a short period. When absorption keeps pace with transpiration the plants revive. (Mid day wilt).
- 8. Continued… c) Hydrological drought: Meteorological drought, when prolonged results in hydrological drought with depletion of surface water and consequent drying of reservoirs, tanks etc. It results in deficiency of water for all sectors using water. This is based on water balance and how it affects irrigation as a whole for bringing crops to maturity. d) Agricultural drought (soil drought): It is the result of soil moisture stress due to imbalance between available soil moisture and evapotranspiration of a crop. It is usually gradual and progressive. Plants can therefore, adjust at least partly, to the increased soil moisture stress. This situation arises as a consequence of scanty precipitation or its uneven distribution both in space and time.
- 10. 3. Based on time of occurrence a) Early season drought: It occurs due to delay in onset of monsoon or due to long dry spells after early sowing b) Mid season drought: Occurs due to long gaps between two successive rains andmstored moisture becoming insufficient during the long dry spell. c) Late season drought: Occurs due to early cessation of rainfall and crop water stress at maturity stage.
- 11. 4. Other terms to describe drought a) Relative drought: The drought for one crop may not be a drought situation for another crop. This is due to mismatch between soil moisture condition and crop selection. Eg. A condition may be a drought situation for growing rice, but the same situation may not be a drought for growing groundnut. b) b) Physiological drought: Refers to a condition where crops are unable to absorb water from soil even when water is available, due to the high osmotic pressure of soil solution due to increased soil concentration, as in saline and alkaline soils. It is not due to deficit of water supply.
- 12. Important causes for agricultural drought are Inadequate precipitation Erratic distribution Long dry spells in the monsoon Late onset of monsoon Early withdrawal of monsoon Lack of proper soil and crop management
- 13. Effect of drought on crop production a) Water relations: Alters the water status by its influence on absorption, translocation and transpiration. The lag in absorption behind transpiration results in loss of turgor as a result of increase in the atmospheric dryness. b) b) Photosynthesis: Photosynthesis is reduced by moisture stress due to reduction in Photosynthetic rate, chlorophyll content, leaf area and increase in assimilates saturation in leaves (due to lack of translocation). c) c) Respiration: Increase with mild drought but more serve drought lowers water content and respiration.
- 14. Continued… d) Anatomical changes: Decrease in size of the cells and inter cellular spaces, thicker cell wall , greater development of mechanical tissue. Stomata per unit leaf tend to increase. e) Metabolic reaction: All most all metabolic reactions are affected by water deficits. f) Hormonal Relationships: The activity of growth promoting hormones like cytokinin, gibberlic acid and indole acetic acid decreases and growth regulating hormone like abscisic acid, ethylene, etc., increases. g) Nutrition: The fixation, uptake and assimilation of nitrogen is affected. Since dry matter production is considerably reduced the uptake of NPK is reduced.
- 15. Continued… h) Growth and Development: Decrease in growth of leaves, stems and fruits. Maturity is delayed if drought occurs before flowering while it advances if drought occurs after flowering. i) Reproduction and grain growth: Drought at flowering and grain development determines the number of fruits and individual grain weight, respectively. Panicle initiation in cereals is critical while drought at anthesis may lead to drying of pollen. Drought at grain development reduces yield while vegetative and grain filling stages are less sensitive to moisture stress. j) Yield: The effect on yield depends hugely on what proportion of the total dry matter is considered as useful material to be harvested. If it is aerial and underground parts, effect of drought is as sensitive as total growth. When the yield consists of seeds as in cereals, moisture stress at flowering is detrimental.
- 16. Crop Adaptation and Mitigation to Drought Crop Adaptation: The ability of crop to grow satisfactorily under water stress is called drought adaptation. Adaptation is structural or functional modification in plants to survive and reproduce in a particular environment. Crops survive and grow under moisture stress conditions mainly by two ways: (i) Escaping drought and (ii) drought resistance
- 17. Crop Adaptation and Mitigation to Drought
- 18. 1. Escaping Drought Ephemerals:- Many desert plants, the so called ephemerals, germinate at the beginning of the rainy season and have an extremely short life period (5 to 6 weeks) which is confined to the rainy period. These plants have no mechanism for overcoming moisture stress and are, therefore, not drought resistant. Germination inhibitors serve as safety mechanism. In cultivated crops, the ability of a cultivar to mature before the soil dries is the main adaptation to growth in dry regions. Certain varieties of pearl millet mature within 60 days after sowing. Short duration pulses like cowpea, green gram, and black gram can be included in this category. Verbeena
- 19. 2. Drought/Stress Resistance : Plants can adopt to drought either by avoiding stress or by tolerating stress due to different mechanisms. These mechanisms provide drought resistance.
- 20. Avoiding Stress Stress avoidance is the ability to maintain a favourable water balance, and turgidity even when exposed to drought conditions, thereby avoiding stress and its consequences. Stress avoidance is usually achieved through morphological changes in the plant : Reduced stomatal conductance Decreased leaf area Development of extensive root systems Increased root/shoot ratios
- 21. I. DROUGHT STRESS Drought : Moisture scarcity which restricts the full expression of genetic yield potential of a plant. Mechanisms of drought resistance: a) Drought escape: Mature early (Ephemerals) b) Drought avoidance: Maintain water balance c) Drought tolerance: Higher yield even under low water potential
- 22. Effects of drought at cellular level Structures of membrane and organelles Structures of macromolecules like proteins and nucleic acids Amounts of specific mRNA Rate of translation Pressure differential across the membrane- cell wall complex; in turn affects cell expansion. A combination of the above.
- 23. Morphological features providing drought resistance Earliness Reduced tillering Leaf rolling, folding, shedding, leaf reflectance Reduced leaf area; narrow leaf, change in leaf angle • Hairiness Color of leaves Wax coating Root systems
- 24. Physiological response to drought Photosynthetic efficiency is reduced due to chloroplast damage Reduced transpiration and reduced respiration losses Stomatal behavior Biochemical response to drought Accumulation of compatible solutes Increase in ABA & Ethylene Protein synthesis Nitrate reductase activity
- 25. Sources of drought resistance Cultivated varieties Land races Wild relatives: e.g. Wheat: A.variabilis, A,speltoides, A.squarrosa Sugar cane: S. spontaneum Transgenes : Rab (Responsive to abscisic acid) in rice
- 26. Mitigation Strategies to Drought
- 27. Mitigation by crop management practices Selection of crops/varieties Seed hardening Sowing of crops
- 28. Selection of crops/varieties Short duration Early vigour Deep root system Dwarf plant with erect leaves and stems Moderate tillering Lesser period between flowering and maturity Moderate dormancy Wider adoptability
- 29. Relative drought tolerant crops RABI • Oats • Barley • Triticale KHARIF • Sorghum • Pearl millet • Kodo millet • Green gram • Black gram • Niger LEGUMES •Soybean •Groundnut •Chickpea •Cowpea •Pigeon pea
- 30. Relative Drought tolerance crop variety Pearl millet: CZIC 923,HHB 67,HHB 68,GHB 183, GHB 1399,etc • Cluster bean: Maru guar, FS 277,HG 75, HG 182,I- IGS 365,RGC 936, PLG119, PLG 85, Suvidha, Navcen,etc • Mung bean: Asha,K 851,RMG 131,etc • Moth bean: RMO 40,Marp moth,Jadia, Jawala,PCMO 880,T 88, CAZRI moth-l,etc. Relatively drought tolerant crop varieties Source-CAZRI,2000 .Strategy to combat drought and famine in the Indian arid zone
- 31. Seed hardening It is done to induce drought tolerance in emerging seedlings. It is the process of soaking seeds in chemical solution and drying to induce tolerance to drought. Seed hardening enables seedlings to survive this early moisture stress. Seeds are soaked for specified time in chemical solutions of prescribed concentration. Soaked seeds are then dried in shade back to original moisture content. During soaking, seeds imbibe water and germination process is started but not completed. The hardened seeds are thus in a ready state for germination. When sown in moist soils, seeds germinate immediately. Such early germination helps in seedling emergence before surface soil dries up.
- 32. Sowing at optimum soil moisture An effective rainfall of 20-25 mm which can wet a depth of 10-15 cm is needed for sowing. Moisture stress at or immediately after sowing adversely affects germination and establishment of seedlings. To ensure adequate soil moisture at sowing, sowing has to be done as early as possible after soaking rainfall is received.
- 33. Time of sowing Optimum time of sowing is indicated by adequate rainfall to wet seeding depth and continuity of rainfall after sowing. The probable sowing time in a rainfed area is the week which has a rainfall of not less than 20 mm with coefficient of variability less than 100% and the probability of a wet week following wet week. Timely sowing ensures optimal yield besides it may also help pest avoidance.
- 34. Optimum depth of sowing When seeds are sown on surface or at very shallow depth, germination and seedling growth are affected when surface soil moisture dries up. Sowing at a depth where soil moisture availability is adequate, ensure early and uniform germination and seedling establishment. Optimum depth of' sowing varies with crop, especially seed size and penetration power of plumule. Crop Depth of sowing (cm) Sesamum 1-2 cm Pearl millet and minor millets 2-3 cm Pulses, sorghum, sunflower 3-5 cm Cotton, maize 5 cm
- 35. Method of sowing: In dry lands, it is important to sow the seeds in moist soil layer at correct depth, neither on the surface nor too deep ensure proper germination. The density, geometry, and depth of sowing are dependent on method of sowing. The sowing methods usually adopted in dry lands include broadcasting, sowing behind plough and sowing by seed drills. Dibbling of seeds and planting of seedlings are also adopted for some crops (Cotton, tobacco, chillies).
- 36. Other Agronomical Strategies for drought management 1. Adjusting the plant population: The plant population should be lesser in dryland conditions than under irrigated conditions. The rectangular type of planting pattern should always be followed under dryland conditions. Under dryland conditions whenever moisture stress occurs due to prolonged dry spells, under limited moisture supply the adjustment of plant population can be done by :
- 37. Continued… a) Increasing the inter row distance: By adjusting more number of plants within the row and increasing the distance between the rows reduces the competition during any part of the growing period of the crop. Hence it is more suitable for limited moisture supply conditions. b) Increasing the intra row distance: Here the distance between plants is increased by which plants grow luxuriantly from the beginning. There will be competition for moisture during the reproductive period of the crop. Hence it is less advantageous as compared to above under limited moisture supply.
- 38. 2)Mid season corrections: The contingent management practices done in the standing crop to overcome the unfavourable soil moisture conditions due to prolonged dry spells are known as mid season conditions. a) Thinning: This ca be done by removing every alternate row or every third row which will save the crop from failure by reducing the competition b) Spraying: In crops like groundnut, castor, redgram, etc., during prolonged dry spells the crop can saved by spraying water at weekly intervals or 2 per cent urea at week to 10 days interval. c) Ratooning: In crops like sorghum and bajra, ratooning can practiced as mid season correction measure after break of dry spell.
- 39. 3. Mulching: It is a practice of spreading any covering material on soil surface to reduce evaporation losses. The mulches will prolong the moisture availability in the soil and save the crop during drought conditions.
- 40. 4. Weed control: Weeds compete with crop for different growth resources are seriously under dryland conditions. The water requirement of most of the weeds is more than the crop plants. Hence they compete more for soil moisture. Therefore the weed control especially during early stages of crop growth reduce the impact of dry spell by soil moisture conservation. 5. Water harvesting and life saving irrigation: 6. Use of wind breaks and shelterbelts