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首页> 外文期刊>Journal of the Indian Society of Soil Science >Characterization, Classification and Evaluation of Soils of Karanji Watershed, Yavatmal District of Maharashtra for Land Resource Management using Geospatial Technologies
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Characterization, Classification and Evaluation of Soils of Karanji Watershed, Yavatmal District of Maharashtra for Land Resource Management using Geospatial Technologies

机译:马哈拉施特拉邦亚瓦特马尔地区卡兰吉流域土壤的表征,分类和评估,用于利用地理空间技术进行土地资源管理

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摘要

Soils representing major physiographic units comprising plateau top, escarpment, isolated hillock, foot slopes, undulating land, alluvial plain and valley developed from basalt and basaltic alluvium under varying land use and slope were characterizedusing remote sensing data and digital elevation model (DEM), classified, mapped and assessed for their sustainable use. Soils developed on plateau top, escarpments, isolated hillocks and foot slopes were very shallow to shallow, loamy to clayey, well-drained and moderately to severely eroded, while soils developed on undulating lands, alluvial plain and valley were deep to very deep, fine to very fine in texture, moderately well drained and slightly eroded. The soil colour, in general, is l0YR in hue and at places (plateau top and foot slope) exhibited SYR with chroma 1 to 3 and value 3 to 5. The pH of the surface soils is neutral to slightly alkaline. However, higher pH and exchangeable sodium percentage (ESP) in sub-soils of Dhama (P12) and Kongara (P14) in alluvial plain indicated the development of sub-soil sodicity with concomitant decrease in hydraulic conductivity. At sub-group level, the soils were classified as Lithic Ustorthents (PI, P3 and P4) and Typic Ustorthents (P2, P5, P6 and PIO), Typic Haplustepts (P17), Vertic Haplustepts (P7, P8, P9, P11, P13, P15 and P16) and Sodic Haplusterts (P12 and P14) based on soil profile development and diagnostic characterisfics. Seventeen soil series were identified and mapped as association of soil series in different physiography-land use units. The soils were found extremely poor to poor at upper elevations but it is good in soil productivity at lower elevations of the watershed. Based on assessed soil constraints and site characteristics, the landcapability, land irrigability and soil suitability for major crops were evaluated and a suitable land use plan has been suggested for land resource management and development.
机译:利用遥感数据和数字高程模型(DEM)表征了代表主要生理单位的土壤,包括高原顶,陡坡,孤立的岗地,山坡,起伏的土地,玄武岩和玄武冲积物在不同土地利用和坡度下发育的冲积平原和山谷。 ,对它们的可持续利用作图和评估。在高原顶,陡坡,孤立的丘陵和山脚斜坡上发育的土壤非常浅至浅,从壤土到黏土,排水良好,中等至严重侵蚀,而在起伏的土地,冲积平原和山谷上发育的土壤深至非常深,细密质地非常细腻,排水适度,略有腐蚀。通常,土壤颜色在色调上为10YR,在某些地方(高原顶坡和山麓坡)表现出SYR,色度为1至3,值为3至5。表层土壤的pH为中性至弱碱性。然而,冲积平原中的Dhama(P12)和Kongara(P14)的次土壤中较高的pH值和可交换钠百分比(ESP)表示次土壤苏打水的发展,同时水力传导率随之降低。在亚组级别上,土壤分为以下类别:岩石Ustorthents(PI,P3和P4)和Typic Ustorthents(P2,P5,P6和PIO),Typic Haplustepts(P17),Vertic Haplustepts(P7,P8,P9,P11, P13,P15和P16)和Sodic Haplusterts(P12和P14)基于土壤剖面的发展和诊断特征。确定了十七个土壤系列,并将其映射为不同生理土地利用单位中土壤系列的关联。人们发现高海拔地区的土壤极为贫瘠,但流域低海拔地区的土壤生产力却很好。根据评估的土壤限制条件和场地特征,对主要农作物的土地利用能力,土地灌溉能力和土壤适应性进行了评估,并提出了适合土地资源管理和开发的土地利用计划。

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