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Spatial variability analysis of soil quality parameters in a watershed of Sub-Himalayan Landscape - A case study

机译:喜马拉雅山下景观流域土壤质量参数的空间变异性分析-以一个案例为例

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Soil organic carbon (SOC) is a key component in maintaining soil quality. Mapping thelocal scale variations in the distribution and stratification of SOC and other soil qualityparameters across different layers has always been a challenging task, in the currentglobal scenario of changing climates. The study was aimed to investigate the spatialdistribution of SOC and other soil quality parameters including SOC stratification ratio andCN ratio in a small hilly watershed (? 10 km2) located in the mid Himalayan region ofHimachal Pradesh, India. Soil samples were collected in November 2015, from 75 points attwo depths (0-15 cm and 15-30cm), along with their geographical coordinates using aGlobal Positioning System (GPS). The results revealed that SOC concentration (g kg-1)decreased with increasing soil depth, throughout the study area and differed significantly(P0.01) between the two depths in vertical soil profile. The SOC stratification ratio valueswere greater than 1.2 in major portion of watershed indicating a spatial improvement insoil quality. C: N ratio, another important soil quality attribute values were found to be12:1, indicating high degree of soil quality and increased rate of organic mattermineralization. The spatial distribution maps of SOC content (g kg-1), SOC stratificationratio as well as CN ratio of study area were generated using Inverse Distance Weighted(IDW) interpolation approach. Additionally soil quality index (SQI) was also computedusing various soil quality parameters based on Analytical Hierarchy Process (AHP) andtheir spatial distribution was analyzed in the watershed. Nearly 76% of the study area hadSQI values in the range of 60-75, whereas 22.16% of the area had SQI60 and 2.59% hadSQI75. The overall results indicated that a higher degree of soil quality existed at thehigher elevation regions of the watershed. Majority of the soils in the watershedaccounted for only 60% of the maximum possible value of SQI, which necessitates theadoption of better management practices for improving the soil quality.
机译:土壤有机碳(SOC)是维持土壤质量的关键组成部分。在当前全球气候变化的情况下,绘制不同层上SOC和其他土壤质量参数分布和分层中的局部尺度变化一直是一项艰巨的任务。该研究旨在调查印度喜马mac尔邦喜马拉雅中部小丘陵流域(约10 km2)中SOC的空间分布以及其他土壤质量参数,包括SOC分层比和CN比。使用全球定位系统(GPS)于2015年11月在两个深度(0-15厘米和15-30厘米)的75个点采集了土壤样品,以及它们的地理坐标。结果表明,在整个研究区中,SOC浓度(g kg-1)随土壤深度的增加而降低,并且在垂直土壤剖面的两个深度之间存在显着差异(P <0.01)。流域大部分地区的SOC分层比值均大于1.2,表明土壤质量在空间上有所改善。 C:N比,另一个重要的土壤质量属性值<12:1,表明土壤质量高,有机质矿化率提高。利用反距离加权(IDW)插值方法生成了SOC含量(g kg-1),SOC分层比以及研究区CN比的空间分布图。此外,还基于层次分析法(AHP),使用各种土壤质量参数计算土壤质量指数(SQI),并对其流域内的空间分布进行了分析。研究区域中将近76%的SQI值在60-75范围内,而研究区域的22.16%的SQI <60和2.59%的SQI> 75。总体结果表明,流域高海拔地区土壤质量较高。流域中的大多数土壤仅占SQI最大可能值的60%,因此必须采取更好的管理措施以改善土壤质量。

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