Micronutrient does not mean that they are less important to plants than other nutrients. Plant growth and devel- opment may be retarded if any of these elements is lacking in the soil or is not adequately balanced with other nutrients. Inorganic micronutrients occur naturally in soil minerals. The parent material from which the soil de- veloped and soil forming processes determines what the micronutrient content of the soil will be. As minerals break down during soil formation, micronutrients are gradually released in a form that is available to plants. Two sources of readily available micronutrients exist in soil: nutrients that are adsorbed onto soil colloids (very small soil particles) and nutrients that are in the form of salts dissolved in the soil solution [1] . Organic matter is an important secondary source of some micronutrients. Most micronutrients are held tightly in complex organic compounds and may not be readily available to plants. However, they can be an important source of micronu- trients when they are slowly released into a plant available form as organic matter decomposes.

Micronutrient deficiencies are widespread. 50% of world cereal soils are deficient in zinc and 30% of cultivated soils globally are deficient in iron. Steady growth of crop yields during recent decades (in particular through the green revolution) compounded the problem by progressively depleting soil micronutrient pools. In general, farmers only apply micronutrients when crops show deficiency symptoms, while micronutrient deficiencies de- crease yields before symptoms appear [1] . Some common farming practices (such as liming acid soils) contrib- ute to widespread occurrence of micronutrient deficiencies in crops by decreasing the availability of the micro- nutrients present in the soil. Major problems in alleviating micronutrient deficiencies include difficulty in the identification of field crop symptoms, variation in soil micronutrient status, soil pH, and intensity, and seasonal fluctuations in the levels and temperature regimes in the region, inadequate facilities and field tests to validate soil and plant micronutrients in the region [2] . Assessment of micronutrient deficiency can be made through visual leaf symptoms and soil and plant analyses. Response of crops to the application of micronutrients not only confirms the deficiencies but also helps in determining nutrient needs.

Various agronomic approaches can be used to correct micronutrient disorders. Once a deficiency is reliably identified, it can generally be corrected by chemical amendments that suit the plant demand and farmer options. The amount, form, mode and timing are critical, especially if multiple nutrient stresses and antagonisms among nutrients are present. Toxicities are more difficult to handle than nutrient deficiencies [2] . Direct toxicities occur when excess element is absorbed and retards physiological functions or becomes lethal to the plant. Indirect toxicity may occur through interactions; excess uptake of one nutrient may hamper the uptake, transport and uti- lization of another nutrient and may result in its deficiency.

It is the most common micronutrient disorders in wet-land rice (often combined with P deficiency). Due to in- crease availability of Ca, Mg, Cu, Fe, Mn and P under prolonged submergence Zn availability and uptake ham- pered by the crops. Zinc (Zn) deficiency is the most widespread micronutrient disorder in rice, but efforts to de- velop cultivars with improved tolerance have been hampered by insufficient understanding of genetic factors contributing to tolerance [1] . Zinc is essential for several biochemical processes such as cytochrome and nucleo- tide synthesis, enzyme activation, chlorophyll production, maintenance of membrane activity, increase rate of seed and stalk maturation. Zinc deficiencies mainly occur when soil pH is, high organic matter in soil, calca- reous soils with high bicarbonate content, intensively cropped soils. Paddy soil under prolonged submerged condition cause zinc deficiency. Symptoms are common on younger or middle aged leaves [2] [3] . Deficiency symptoms causes brown to dusty brown spots on younger leaves (2 - 4 weeks after transplanting) in red soils, yellowing of leaves/midrib bleaching. Symptoms are prolonged during early growth stages due to immobilization of zinc. Symptoms of zinc deficiency sometimes resemble Fe/Mn deficiencies. Zinc deficiency in rice soil is commonly known as khaira. The main symptom of khaira in rice is usually in nursery; chlorotic/yellow patches at leaf base on both sides of the midrib; restricted root growth and usually main roots turn brown. Zinc deficiency has also been associated with high bicarbonate content, a Mg:Ca ratio in soils >1, the use of high level of fertilizers, intensive cropping, use of high yielding cultivars, and irrigation with alkaline water [4] . The most preventing measures for zinc deficiency is selection of Zn efficient variety that is tolerant to high level of bicarbonate as well as low zinc in soil. Beside these applications of ZnSO₄ in nursery beds, drain the field, seedling root dipping in 2% - 4% ZnO suspension, mid season correction by spraying 0.5% ZnSO₄ thrice at weekly intervals between 3 - 6 WAT etc. But curative measure for correcting are application of 20 - 25 kg/ha ZnSO₄ in acid soil, 22 kg Zn/ha initially followed by 5 - 10 kg Zn in the later years or 50% gypsum + 10 t GM + 22 kg Zn once in 2 - 3 years in sodic soils, 1.0 - 1.5 kg/ha Zn as foliar spray at tillering stage and 2 times latter is very helpful for correct this deficiency. Plant Zn uptake from low Zn soils can be increased by Zn mobilizing chemical rhizosphere processes.

The iron content in soil varies from 1% to 20%, averaging 3.2%, but its normal concentration in plants is only 0.005%. Iron deficiency is common in upland, high pH and aerobic soil and toxicity is one of the major con- straints to lowland rice production. It disrupts the rice plant physiology in several respects. The critical iron toxi- city concentration in plant tissue depends partly on the overall nutritional status of the plant. Iron helps in the formation of chlorophyll. A deficiency of iron causes chlorosis between the veins of leaves and the deficiency symptom show first in the young leaves of plants [5] . It does not appear to be translocated from older tissues to the tip meristem and as a result growth ceases. Iron is also a structural component of nonheame molecules like ferrodoxins (stable Fe-S proteins). Ferrodoxin is the first stable redox compound of the photosynthetic electron transport chain [2] . The main important deficiency symptoms are interveinal yellowing and chlorosis of emerg- ing leaves, less dry matter production, reduced sugar metabolism enzymes, plants become stunted with narrow leaves. Iron deficiency causes chlorosis symptoms in rice plant due to relative immobility of iron in rive plants, interveinal chlorosis on surface of the leaf showing a fine reticulate network of green setting off chlorotic areas. The main reason for iron deficiency are low concentration of iron in upland soil, coarse textured soil, low land soil with very low organic matter content, increased rhizosphere pH etc. Though it is the most difficult and costly micronutrient deficiency to correct it can be controlled by application of FeSO₄ 25 kg/ha in between rows, application of iron containing fertilizers or foliar spary of FeSO₄ 1% - 3% solution. Iron toxicity is caused by toxic effects of excessive Fe uptake due to large concentration of Fe in soil solution [4] [6] . The main important toxicity symptoms of iron are tiny brown spots on lower leaves starting from tip and spread towards the leaf, base or whole leaf coloured orange-yellow to brown. Spots combine on leaf inter-veins and leaves turn orange- brown and die. Leaves appear purple-brown if Fe toxicity is severe stunted growth, extremely limited tillering. Iron toxicity can be controlled by seed treatment with Ca peroxide at 50% - 100% seed wt., intermittent irriga- tion at tillering stage and by balanced fertilization.

Boron is concerned with precipitating excess cations, buffer action, regulatory effect on other nutrient elements etc., development of new cells in meristematic tissue, treanslocation of sugars, starches, phosphorus etc., essen- tial for cell wall formation. Boron deficiency occurs under moister stress and dry condition which cause reduced plant height [5] . Plants fail to produce panicles if they are affected by B deficiency at the panicle formation stage. The tips of emerging leaves are white and rolled. Soil application of B (1 - 2 kg/ha) is superior to foliar sprays. For hidden deficienct, spary 0.2% boric acid or borax at pre flowering or flower head formation stages. Excess of boron appears to inhibit the formation of starch from sugars or results in the formation of B-carbohydrate complexes, resulting in retarded grain formation [6] . The symptoms of boron toxicity are brownish leaf tips and dark brown elliptical spots on leaves, necrotic spot at panicle initiation stage. Use of boron rich ground water, excessive application of boron and high temperature are the main cause of boron toxicity. Boron toxicity can be controlled by B tolerant variety, use of irrigation water having low boron content, deep ploughing etc. Some- times dark green leaf and brown root also occur when B is absent in soil as well as in plant.

The role of manganese is regarded as being closely associated with that of iron. Manganese also supports the movement of iron in the plant. It influences auxin levels in plants and high concentrations of Mn favour the breakdown of Indole Acetic Acid (IAA), takes part in electron transport in photosystem II [2] . Manganese defi- ciency is very common in upland rice, degraded paddy soil high in Fe content, accumulation of H2S, acid sandy or acid sulphate soil, excessive liming in acid soil etc. manganese deficiency can be corrected by application of farmyard manure, acid forming fertilizer (do not use urea), MnSO₄ or MnO at 2 - 5 kg/ha as multiple application [6] . Chelates should be avoided as Fe and Cu displaces Mn. Manganese toxicity shows brown spots on the veins of the leaf blade and the leaf sheath in lower leaves. Plant growth are stunted and ultimately cause less number of tillering.

Silicon is considered a plant nutrient “anomaly” because it is presumably not essential for plant growth and de- velopment. The beneficial effects of silicon have been attributed to correction of soil toxicities arising from high levels of available Mn, Fe²⁺ and active aluminium. Silicon also provides greater stalk strength and resistance to lodging, increased availability of phosphorus, reduced transpiration etc. Silicon tends to maintain erectness of rice leaves, increases photosynthesis because of better light interception. The oxidizing power of rice roots and accompanying tolerance to high levels of iron and manganese were found to be very dependent on silicon nutri- tion. The major deficiency symptoms of Si in rice are soft droopy leaves and culms, lodging of plant, severe pest-disease attack [7] . Deficiency generally occurs due to small mineral reserves in organic soil, old paddy soils of subtropical and temperate climates. Silicon deficiency can be correct by irrigation of water rich in Si, avoid excessive application of N fertilizers, recycling rice hulls or hull ash, apply granular silicate fertilizers like Ca silicate: 120 - 200 kg/ha; K silicate: 40 - 60 kg/ha for rapid correction. Foliar spray of Si at 0.1% - 0.2% with sodium silicate improve Si nutrition.

Copper helps in the utilization of iron during chlorophyll synthesis. Lack of copper causes iron to accumulate in the nodes of plants. It has an unique involvement in enzyme systems of plants like oxidase enzymes, terminal oxidation by cytochrome oxidase, photosynthetic electron transport mediated by plastocyanin etc. It also acts as “electron carrier” in enzymes which bring about oxidation-reduction reactions in plants. Sandy, calcareous, late- ritic soil, high in organic matter induce Cu deficiency in soil. The main important deficiency symptoms of cop- per are chlorotic leaves, bluish green leaves, new leaves don’t unroll and leaf tips give needle like appearance, reduced tillering, less pollen viability. Excessive liming in acid soil sometimes causes Cu deficiency in soil [8] . It can be control by seeding root dipping in 1% CuSO₄ suspension, apply Cu at 5 - 10 kg/ha once in 5 years in the form of CuO or CuSO₄. Foliar application can be done during tillering to panicle initiation stage. Soil appli- cation can also be done with CuSO₄ as broadcasting or band placement.

Molybdenum is an essential component of the major enzyme nitrate reductase in plants. Its requirement of plants is influenced by the form of inorganic nitrogen supplied to plants, with either nitrite () or ammonium () effectively lowering its need [3] . It is also reported to have an essential role in iron absorption and translocation in plants. Deficiency symptoms of Mo in rice resembles to nitrogen deficiency (older leaves be- come chlorotic). Necrotic spots are seen at leaf margins because of NO₃ accumulation. Molybdenum deficiency can be correct by liming of acid soils to pH 6.5 (not preferable if pH change is not desirable for other purposes). Beside these dusting with Na/NH₄ at 100 - 500 g/ha is very much beneficial. Foliar spay of Na/NH₄ molybdate at 0.1% is also beneficial [9] .

Boron and molybdenum are generally fixed in rice soil. In case of boron main reaction occur when acid soils are limed. Lime is able to replace Al³⁺ by Ca²⁺ and produce insoluble precipitation of aluminium hydroxide/iron hydroxide. This precipitate adsorbs large quantities of boron. Soil high in organic matter also has high Boron. Molybdenum adsorbed strongly by iron/aluminium oxides. Soils high in non crystalline iron on clay surfeces, tend to be low in available molybdenum due to fixation [7] -[9] .

• Low levels of N, S & Mg exhibited high Mn and low Fe uptake

• P induced Zn deficiency: High level of available P

o ZnSO₄ application at 15 - 20 kg/ha

• Application of K decrease Mn & Fe content in rice plant

• Increase in pH by lime application reduce Zn availability to plants

• Application of Zn depress extractable Fe but increase Mn in submerged rice soil

• Application of Cu decrease Fe & Mn in submerged rice soil

• High Fe in soil suppress Cu absorption by rice

• Fe plays an antagonistic role in relation to Zn in rice plant & waterlogged rice plant

• Mn inhibit Zn absorption by rice root, but favored Zn translocation within plants

• Mn interferes with translocation of Fe from root to shoot

• Calcareous soil + high pH: Iron chlorosis due to iron remaining in ferric (oxidized state)

o inundation for 2 - 3 days or foliar application of iron

• Iron toxicity: Acidic soil (liming is best way)

o Zinc deficiency: Normal & saline-sodic soils-ZnSO₄ application at 40 kg/ha

More information on the transformation and availability of micronutrients for different soils and the effect of manipulating the soil physical environment and its moisture regimes on plant available micronutrients need to be generated. Continuous use of farmyard manure or of other organic sources arrests the depletion of available mi- cronutrient pools from soils. Development of integrated micronutrient technology using available organic mate- rials is needed not only to increase micronutrient use efficiency but also to decrease the pressure on the use of costly inorganic micronutrient carriers. Field experiments have proved the superiority of zinc sulfate as a zinc carrier. Increasing costs coupled with a shortfall in supply of zinc sulfate have necessitated investigations on evaluating sparingly soluble zinc sources or ores combined with zinc mobilizers. The residual availability of various sources of micronutrients for a cropping system needs to be worked out.