首页> 外文期刊>Journal of the Indian Society of Soil Science >Particle Size Distribution, Soil Organic Carbon Stock and Water Retention Properties of Some Upland Use System of Odisha and Assessing their Interrelationship
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Particle Size Distribution, Soil Organic Carbon Stock and Water Retention Properties of Some Upland Use System of Odisha and Assessing their Interrelationship

机译:Otisha的一些高地使用系统的粒度分布,土壤有机碳储备和水保留特性,评估它们的相互关系

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Analyzed particle size distribution, soil water retention properties and organic carbon (SOC) stock of some upland cropping/land use systems of a watershed of Odisha (Kadalipal watershed, Dhenkanal, Odisha) viz., forest grazing land, maize, rice, groundnut, cucumber, okra, cowpea, cashew nut plantation and barren land and assessed their interrelationship. An overview of soil texture of the samples revealed that sandy clay loam texture constituted about 60% of all samples in different cropping systemsand at different depths. Clay loam, sandy loam and loamy texture represented 20, 15 and 5%, respectively. Bulk density (BD) of surface layer ranged from 1.39 Mg m~3 in C7 (cashew plantations) to 1.48 Mg m3 in forest grazing land (C0). The average clay content in the soil profile ranged from 23.8% in C0 (grazing land) to 32.6% in C6 (cowpea). The SOC at surface (0-0.15 and 0.15-0.30 m) layers were higher in forest grazing land (9.6 to 10.8 g kg1) and inside cashew plantation (12.3 to 13.5 g kg1) whereas, SOC was low in crop cultivated plots. Continuous tillage and cultivation of nutrient exhaustive crops might have favoured rapid rate of mineralization than that of accumulation of SOC in these fields. Among crop fields, legumes (groundnut, cowpea) holdpromise for greater accumulation of SOC in the long-term. Soil water retention was found to be significantly correlated with SOC at 0-0.15 m depths only rather than the SOC of whole profile. Soil pH, BD, porosity had significant relationship (P< 0.05) with SOC content.
机译:分析Otisha(Kadalipal Spatershed,Dhenkanal,Otisha)Ziz的水域中一些高地种植/土地利用系统的粒度分布,土壤水保留性能和有机碳(SOC)股票。,森林放牧陆,玉米,米饭,地生,黄瓜,秋葵,豇豆,腰果种植园和贫瘠的土地,并评估了他们的相互关系。样品的土壤纹理概述显示,桑迪粘土壤土纹理在不同的种植系统中构成约60%的样本和不同深度。粘土壤土,砂质壤土和壤土质地分别代表20,15和5%。表面层的批量密度(BD)在C7(CasheNeg Plantation)中的1.39mg m〜3中,森林放牧地(C0)中的1.48毫克M3。土壤曲线的平均粘土含量范围为CO(放牧土地)的23.8%,C6(COWPEA)中的32.6%。表面(0-0.15和0.15-0.30米)的SOC在森林放牧地上(9.6至10.8g KG1)和内部饲养场(12.3至13.5克kg1)较高,而SoC在作物培养的地块中很低。连续耕作和培养养分庄稼可能有利于这些领域中SoC积累的快速矿化率。在作物领域,豆类(Groundnut,Cowpea)持有人在长期内持有SOC的更大积累。发现土壤水保留与SoC的0-0.15米深度而不是整个轮廓的SoC显着相关。土壤pH,BD,孔隙率具有显着关系(P <0.05)SOC含量。

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