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Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 International Journal of Current Microbiology and Applied Sciences ISSN: 2319-7706 Volume 6 Number 9 (2017) pp. 4585-4590 Journal homepage: http://www.ijcmas.com Original Research Article https://doi.org/10.20546/ijcmas.2017.607.479 Studies on Secondary and Micro Nutrient Properties of Soil Profiles in Village Baragaon Nandur, Taluka Rahuri, Maharashtra, India Vaddepally Pavan*, M. R. Chauhan and A. G. Durgude Department of Soil Science and Agriculture Chemistry, Mahatma Phule KrishiVidyapeeth, Rahuri-413722, Maharashtra, India *Corresponding author ABSTRACT Keywords Entisols, inceptisols, vertisols, Ca, Mg, Fe, Mn, Zn, Cu Article Info Accepted: 28 June 2017 Available Online: 10 July 2017 Soil profile studies was conducted in Baragaon Nandur Village, four soil orders viz two entisols, one inceptisols, vertisols were analyzed for chemical properties which are derived from basalt, basaltic alluviam and slightly conditioned by topography. Calcium was ranged from 22.30, 19.70 to 23.78, 18.20 to 26.51, 17.5 to 25.5 cmole (p+) kg -1 in Entisols (A), Entisols (B,) Inceptisols, and Vertisols, soils respectively. In case of magnesium it wasranged from 14.75, 8.86 to 13.58, 8.75 to 16.47, and 9.23 to 13.33 cmole (p+) kg -1. in Entisols (A), Entisols (B), Inceptisols, Vertisols, soil pedons respectively.Available sulphur in the soil was 10.75 mg kg-1in Entisols (A), and it was ranged from 7.54 mg kg-1 to 15.75 mg kg-1 In Entisols (B). While in Inceptisols it was ranged from 10.37 to 14.12 mg kg-1 and inVertisols this range was 6.37 to 24.5 mg kg-1.The value of DTPA extractable Fe ranged from 2.04 to 3.07 mg kg-1 in Entisols (B), 4.10 to 4.25 mg kg-1 in Inceptisols, 2.07 to 5.81 mg kg-1 in Vertisols and 4.33 mg kg-1 in Entisols (A). DTPA extractable Mn content of Entisols (A) was 4.42 mg kg-1.Entisols (B) was ranged from 2.29 to 3.50 mg kg1 . Manganese content in Inceptisols ranged from 3.19 to 4.98 mg kg -1. in Vertisols it was ranged from 2.30 to 4.90 mg kg-1.Zinc content was 0.49 mg kg-1 in Entisols (A) and it was ranged from 0.24 to 0.32 mg kg-1, 0.28 to 0.53 mg kg-1, and 0.38 to 0.45 mg kg-1, in Entisols (B), Inceptisols and Vertisols respectively. Copper content in Entisols (A), Entisols (B), Inceptisols, and Vertisols, ranged from 1.18, 0.44 to 0.92 mg kg-1, 1.73 to 2.46 mg kg-1, and 1.56 to 2.07 mg kg-1respectively.The present investigation was undertaken to generate comprehensive information about the characteristics of soil for evolving proper soil and water management strategies so as to maximize and sustain agriculture production. Introduction Soils are considered as the integral part of the landscape and their characteristics are largely governed by the landforms in which they are developed. Topographic maps, aerial photographs and remote sensing data provide useful tools for geomorphic analysis of the region and help in the soil survey and mapping (Pandey and Pofali, 1982). The life supporting systems of a country and socioeconomic development of its people depends on the soils. More than ever before, a renewed attention is being given to soils due to rapidly declining land area for agriculture, declining in soil fertility and increasing soil 4585 Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 degradation, land use policies and irrational and imbalanced use of inputs (Kanwar, 2004). All the above factors call for a paradigm shift in research away from the maximum crop production to the sustainability of the crop production system without degradation of soil health and environmental quality. Systematic study of morphology and taxonomy of soils provides information on nature and type of soil, their constraints, potential, capabilities and their suitability for various uses (Sehgal, 1996). farms the unit of study in pedagogical investigation. It also helps in soil classification and forms the basis for practical studies of soils. A study of soil profile is important from crop husbandry point of view, since it reveals the surface and subsurface characteristics and qualities, namely depth, texture, structure, drainage conditions and soil-moisture relationships, which directly affect plant growth. It helps to classify the soils and to understand soil-moisture-plant relationships. Study Area Soils of Maharashtra State have been broadly classified as 1) The laterites and lateritic soils 2) The costal saline and costal alluvium soils 3) Shallow medium and deep black soil 4) Gray and red soils of mixed parent materials and 5) Saline, saline-alkaline and non-salinealkaline soils (Raychaudhari and Chakravarty, 1943). Soil is a vital natural resource and should be used judiciously according to its potential to meet the increasing demands of ever growing population. To ensure optimum agricultural production, it is imperative to know best fact about our soils and their management to achieve sustainable production. The quality of soil needs to be looked into because presently the natural resources are being over exploited. Soils of Maharashtra State are categorized as poor in fertility and vary widely in genetic, morphological, physical, chemical and biological characteristics (Challa et al., 1995). The nutrient deficiencies started appearing in different areas due to introduction of intensive production systems after green revolution period. It is due to net removal rates of micronutrients by crops being higher under intensive productivity regimes (Kanwar, 2004). The nutrient deficiencies situation was further increased by the discontinuous and diversified use of organic manures and chemical fertilizers. A soil profile is a historic record of all the soil farming processes and The Village Baragaon Nanduris boundary between region located in between 19° - 21’N latitude and 74°- 35’ E longitude and covers total geographical area of 3845 ha. The elevation is 500m above mean sea level. The Village Baragaon Nandur, is situated about 38 km away from Ahmednagar city.Soils of Village Baragaon Nanduris derived from the igneous rocks viz. Basalt (Deccan trap) which is basic in nature containing mainly feldspars, augite and small amount of titaniferrous magnetite mineral. In the vesicular rocks the any of daloidal cavities are filled with mineral like zeolite and quartz. The soils of Village Baragaon Nandurare under the cultivation of Jowar, Bajara, Wheat, Gram, Pigeon Pea, Soybean, Black Gram, Safflower, Sugarcane and Cotton crops. The natural vegetation grown comprises of dry deciduous tree species and some grasses. The climate is usually hot and potential evapo-transpiration (PET) is far excess of the precipitation and is classified as semi-aired tropical. Village Baragaon Nandur, Taluka Rahuri, DistAhmednagar experience a hot spell from the month of March and May, with rains from June to September. The mean annual maximum and minimum temperatures were ranged from 32.90C and 18.80C, respectively. The Village Baragaon Nandur has annual precipitation of 517.8 mm. The rainfall is torrential, erratic, scanty and ill distributed. 4586 Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 Materials and Methods The survey and sampling was carried out in Village Baragaon Nandur, Taluka Rahuri, Dist- Ahmednagar. Four soil profile site were selected by using GPS (Global Position System) for study after travelling through the area where inceptisols, entisols, vertisols are present. Recorded of surveyed fields, latitude, longitude and altitude was maintained. Profile were dug at selected sites and detailed morphological examination was carried out as per procedure laid down in USDA soil survey manual. Soil sample were collected horizon wise. The soil samples from selected site were collected by using stainless steel auger to avoid iron contamination. Total 12 samples collected from the different horizons of two Entisols, one Inceptisol, and one Vertisol. Soil samples were brought to the laboratory and air dried under shade avoiding contamination with foreign materials and then crushed with a wooden pestle. The sample is then screened through a 2mm sieve and the pebbles, stones and roots were rejected. About 0.5 to 1kg of air dried crushed soil sample was put in the plastic sample bottle, labeled and stacked on the open sample racks for analysis. Each soil sample was analysed for following physical, chemical properties of soil. Results and Discussion The soil profile study was conducted on four soil orders of Village Baragaon Nandur such as two Entisol, one Inceptisol, and one Vertisols. The result of the investigation is described under following heading. Exchangeable Magnesium) cations (Calcium and Among the Exchangeable cations calcium is dominant followed by magnesium in all the soil pedons indicating calcium bearing minerals in parent rock. Similar result was reported by Maji et al., (2005). Calcium was ranged from 22.30, 19.70 to 23.78, 18.20 to 26.51, 17.5 to 25.5 cmole (p+) kg-1 in Entisols (A), Entisols (B,) Inceptisols, and Vertisols, soils respectively. Vertisols having more exchangeable calcium followed by Inceptisols, Entisols. In case of magnesium it wasranged from 14.75, 8.86 to 13.58, 8.75 to 16.47, and 9.23 to 13.33 cmole (p+) kg-1. in Entisols (A), Entisols (B), Inceptisols, Vertisols, soil pedons respectively. Exchangeable calcium decreased with depth and magnesium in most of horizon increased with depth which might be due higher solubility of magnesium salts in their leaching down the profile. (Krishanamoorthy and Govindarajan, 1977). Available Sulphur Availability and distribution of sulphur are controlled by amount and type of clay, organic matter content and management practices. Available sulphur in the soil was 10.75 mg kg-1in Entisols (A), and it was ranged from 7.54 mg kg-1 to 15.75 mg kg-1 In Entisols (B). While in Inceptisols it was ranged from 10.37 to 14.12 mg kg-1 and inVertisols this range was to 6.37 24.5 mg kg-1. Most of all the soils of Village Baragaon Nandur were sufficient in sulphur as per the critical limit 10 mg kg-1 except Entisols (A). Available sulphur showed significant correlation with organic carbon, considering critical limit. (Bandopadhyay and Chattopadhyay, 2001, Shrinivasarao et al., 2005). 4587 Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 Table.1 Standard analytical methods used for chemical analysis of soil samples Sr. No. Soil analysis 1. 2. 3. Parameters Method used Available (Fe,Mn,Zn and Cu) Exchangeable Ca2+, Mg2+ Available S Atomic Absorption Spectrophotometer Versenate titration 0.15% CaCl2 extractable Reference Lindsay and Norvell (1978) Page (1982) Williams and Steinbergs(1969) Table.2 Chemical properties of Representative Pedons of Village Baragaon Nandur Exchangeable (cmol (P+) Kg1) Available nutrients (mg Kg -1) Ca Mg S Fe Mn Zn Cu Pedon 1 Entisols(A) P1-0-22 22.30 14.75 10.75 4.33 4.42 0.49 1.18 Pedon 2 Inceptisols P2-0-26 26.51 16.47 14.12 4.25 4.98 0.53 2.46 26-58 19.74 8.75 12.25 4.21 3.42 0.25 1.58 58-75 18.20 11.35 10.37 4.10 3.19 0.28 1.73 Pedon 3 Vertisols P3-0-28 25.50 11.02 24.5 5.81 4.90 0.45 2.07 28-66 20.80 9.23 15.37 4.05 2.78 0.39 2.03 66-90 17.50 12.18 10.87 3.83 2.43 0.39 1.80 90-120 20.7 13.33 6.37 2.07 2.30 0.38 1.56 Pedon 4 Entisols (B) P4- 0-30 23.78 12.79 15.75 3.07 3.50 0.32 0.92 30-68 21.92 8.86 11.62 2.22 2.68 0.29 0.68 68-100 22.21 10.43 9.25 2.93 2.29 0.24 0.56 100-150 19.70 13.58 7.54 2.04 2.38 0.29 0.44 Pedonno. Available micronutrients (Fe, Mn, Zn and Cu) Every micro-nutrient element plays an important role in plant processes. Their significance in physiological processes and plant metabolism is equally important. The data on available micro-nutrient given in table 2. The value of DTPA extractable Fe ranged from 2.04 to 3.07 mg kg-1 in Entisols (B), 4.10 to 4.25 mg kg-1 in Inceptisols, 2.07 to 5.81 mg kg-1 in Vertisols and 4.33 mg kg-1 in Entisols (A). All the soil pedons are deficient in Fe content except the surface horizon of the Veritisols. Surface layer of Vertisols had sufficient in Fe content and it decreases with depth. (Pharande et al., 1996) DTPA extractable Mn content of Entisols (A) was 4.42 mg kg-1.Entisols (B) was ranged from 2.29 to 3.50 mg kg-1. Entisols are sufficient in Mn content. Manganese content in Inceptisols ranged from 3.19 to 4.98 mg kg1 . Status of Mn is good in Vertisols it ranged from 2.30 to 4.90 mg kg-1. All the soils 4588 Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 contain Higher Mn might be due to parent material i.e. ferromagnesium minerals. Zinc content was 0.49 mg kg-1 in Entisols (A) and it was ranged from 0.24 to 0.32 mg kg-1, 0.28 to 0.53 mg kg-1, and 0.38 to 0.45 mg kg1 , inEntisols (B), Inceptisols and Vertisols respectively. All the soil pedons are deficient in Zn conternt as considering critical limit for zinc is 0.6.Similar results reported by (Sharma et al., 1996). Depth wise decrease in zinc with depth was noticed because of low organic matter and variable clay content. Copper content in Entisols (A), Entisols (B), Inceptisols, and Vertisols, ranged from 1.18, 0.44 to 0.92 mg kg-1, 1.73 to 2.46 mg kg-1, and 1.56 to 2.07 mg kg-1respectively. Depthwise decrease in copper content in Vertisols and Entisols was noticed. (Pharande et al., 1996). References Bandyopadhyay, P.K., and Chattopadhyay, G.N. 2001. 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Sharma, B.L., Bhadoria, A.K.S Rathore, G.S. and Bapat, P.N. 1996. Evaluation of extractant for available Zinc and its form in Verttsols of Madyapradesh.Journal of the Indian Society of Soil Science44, 701-704. Shrinivasrao Ch. Ganeshmurthy, A.N. Singh, R.N. and Masood Ali 2005. Status and 4589 Int.J.Curr.Microbiol.App.Sci (2017) 6(9): 4585-4590 distribution of Sulphur vis-a-vis Taxanomic class wise distribution of sulphur in selected soil series of Inceptisol in West Bengal.Journal of the Indian Society of Soil Science54, 368371. Williams, C.H., and Steinberg, A. 1969. Soil sulphur fraction as chemical indices of available sulphur in some Australian soil Australian Journal of Agricultural. Resources 10, 340-352. How to cite this article: Vaddepally Pavan, M. R. Chauhan and Durgude A. G. 2017. Studies on Secondary and Micro Nutrient Properties of Soil Profiles in Village Baragaon Nandur, Taluka Rahuri, Maharashtra, India. Int.J.Curr.Microbiol.App.Sci. 6(9): 4585-4590. doi: https://doi.org/10.20546/ijcmas.2017.607.479 4590