Spatial Variability of Soil Organic Carbon Stock in Gurje Subwatershed, Hadiya Zone, Southern Ethiopia

IF 2.1 Q3 SOIL SCIENCE
Temesgen Addise, B. Bedadi, A. Regassa, Lemma Wogi, Samuel Feyissa
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引用次数: 0

Abstract

Soil organic carbon contents are expected to vary from place to place because of variation in soil properties. However, the extent of variability has not been explored in the study area. This study has, therefore, been initiated to assess the spatial variability of soil organic carbon stock in Gurje subwatershed Hadiya Zone, Southern Ethiopia. A total of 40 randomly predefined sampling points were identified for soil sampling using GIS and a total of 80 composite soil samples and 80 core samples were collected from those points at two sampling soil depths (0–20 cm and 20–40 cm). The ordinary kriging (OK) method was used as a geostatistical tool and applied to model the spatial variability of soil organic carbon in this study. With respect to soil depth, the coefficient of variation (CV%) for SOC and SOCS varied from 40.87 to 51.36%, which indicated moderate variability in the study area. For the land use types, the CV% varied from 7.94 to 42.06%, indicating low to moderate variability for the variables in the study area. The exponential semivariogram model described the spatial structure of SOC at 0–20 cm depth while the spherical one was used for SOCS. Moreover, the exponential model was best suited for SOCS at a soil depth of 20–40 cm, while the circular model was appropriate for SOC at this depth. The nugget/sill ratio (C0/C0 + C) of SOC and SOCS varied from nil to 15.58, reflecting a strong spatial dependence, which could be mainly due to the influence of intrinsic factors (e.g., natural variations in soils) in the study area. Overall, the spatial distributions of SOC and SOCS were higher in the northwestern and eastern parts of the subwatershed.
埃塞俄比亚南部哈迪亚地区Gurje子流域土壤有机碳储量的空间变异性
由于土壤性质的变化,土壤有机碳含量预计会因地而异。然而,尚未在研究领域探讨变异性的程度。因此,本研究旨在评估埃塞俄比亚南部Gurje亚流域Hadiya区土壤有机碳储量的空间变异性。使用GIS确定了总共40个随机预定义的采样点进行土壤采样,并在两个采样土壤深度(0-20 厘米和20–40 cm)。本研究采用普通克里格方法作为地质统计学工具,对土壤有机碳的空间变异性进行了建模。就土壤深度而言,SOC和SOCS的变异系数(CV%)在40.87%至51.36%之间变化,这表明研究区域的变异性中等。对于土地利用类型,CV%在7.94%到42.06%之间变化,表明研究区域内变量的低到中等变异性。指数半变差函数模型描述了0–20时SOC的空间结构 cm的深度,而球形的用于SOCS。此外,指数模型最适合土壤深度为20–40的SOCS cm,而圆形模型适用于该深度的SOC。熔核/门槛比率(C0/C0 + C) SOC和SOCS的变化范围从零到15.58,反映出强烈的空间依赖性,这可能主要是由于研究区域内在因素(如土壤的自然变化)的影响。总体而言,SOC和SOCS的空间分布在亚流域的西北部和东部较高。
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来源期刊
Applied and Environmental Soil Science
Applied and Environmental Soil Science Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
4.50%
发文量
55
审稿时长
18 weeks
期刊介绍: Applied and Environmental Soil Science is a peer-reviewed, Open Access journal that publishes research and review articles in the field of soil science. Its coverage reflects the multidisciplinary nature of soil science, and focuses on studies that take account of the dynamics and spatial heterogeneity of processes in soil. Basic studies of the physical, chemical, biochemical, and biological properties of soil, innovations in soil analysis, and the development of statistical tools will be published. Among the major environmental issues addressed will be: -Pollution by trace elements and nutrients in excess- Climate change and global warming- Soil stability and erosion- Water quality- Quality of agricultural crops- Plant nutrition- Soil hydrology- Biodiversity of soils- Role of micro- and mesofauna in soil
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