Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/478532
Title: Assessment of Soil Quality and Organic Carbon Stocks under Different Land use Systems in Sub Humid Southern Plains of Rajasthan
Researcher: MEENA, RAM BHAWAN
Guide(s): Meena, S. C.
Keywords: Ecology and Environment
Life Sciences
Soil Science
University: Maharana Pratap University of Agriculture and Technology
Completed Date: 2022
Abstract: newlineResearch database information regarding soil quality, organic carbon, and nitrogen stocks, and soil properties under different land-use systems (LUSs) is essential for the sustainable utilization of existing soil resources. The main objective of this study was to examine the variation in measurable soils properties with carbon and nitrogen storage patterns and soil quality indices (SQIs) under different prevailing land-use systems in the Sub Humid Southern Plains of Rajasthan. Preliminary survey and group interaction with the farmers about land-use, cropping history were used to select the six LUSs, namely barren land (BL), agricultural (AG), agri-horticulture (AH), horticultural (HL), grassland (GL), and natural forest (NF) land-use. A total of 120 composite soil samples [6- land-use systems, 4- soil depths (0-20, 20-40, 40-60, and 60-80 cm), and 5-replication for each LUS] were randomly collected from the selected LUSs for laboratory analysis. The study area was dominated by sandy clay loam soil texture. Soil pH ranged from 7.74 to 8.27 showed slightly alkaline soil conditions under all the LUSs. The EC was not a limiting factor for plant growth and productivity of field crops in the study area. The lowest and highest soil bulk density was observed under natural forest (1.51 Mg m-3), and barren land-use (1.62 Mg m-3), respectively. The maximum total soil porosity, water holding capacity, moisture content at different water potentials, and plant available water recorded under natural forest land-use soil, while barren land-use soil was least in all these soil parameters. The calcium carbonate (CaCO3) varied from 3.12 to 3.30 per cent under different land-use systems with a non-significant difference. However, a significant increasing trend was recorded with soil depth which might be associated with the precipitation of dissolved carbonates in lower soil depths. The CEC, available N, P, K, DTPA extractable soil micronutrients (Zn, Cu, Fe, Mn) and soil organic carbon contents were higher in natural fo
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URI: http://hdl.handle.net/10603/478532
Appears in Departments:Soil Science & Agricultural Chemistry

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01_title.pdfAttached File155.51 kBAdobe PDFView/Open
02_prelim.pdf438.65 kBAdobe PDFView/Open
03_list of content.pdf475.77 kBAdobe PDFView/Open
04_abstract.pdf758.65 kBAdobe PDFView/Open
05_introduction.pdf223.61 kBAdobe PDFView/Open
06_review of literature.pdf584.38 kBAdobe PDFView/Open
07_materials and methods.pdf594.42 kBAdobe PDFView/Open
08_experimental results & discussion.pdf2.76 MBAdobe PDFView/Open
09_summary & conclusion.pdf275.1 kBAdobe PDFView/Open
10_annexures.pdf1.57 MBAdobe PDFView/Open
80_recommendation.pdf588.95 kBAdobe PDFView/Open
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