Mapping spatial variability of hydric soil properties to delineate Khalong-la-lithunya wetlands

IF 0.6 Q4 DEVELOPMENT STUDIES
Gerard Rasekoele Motlalepula, Mapeshoane Botle, Masopha Makoae, Khoeli Makhala, T. Nkheloane, M. Molefe, Motsoane Thabo, Mots’ets’e Motseko
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引用次数: 1

Abstract

Spatial variability in wetland soils provide insight into underlying ecosystem processes and may itself give an indication of wetland condition. The study was conducted to characterise and delineate soil variability of wetlands of Khalong-la-Lithunya from hydric soil properties. Sampling was carried on three sub catchments within Khalong-la-Lithunya catchment. In each sub catchment soil samples were dug at 100m interval along three transects that were 200m apart. Detailed soil profile description of 36 pits was done following USDA-NRCS (2010) manual. Soil samples were collected to the depth of 90 cm at 15 cm interval and analyzed for soil organic carbon (SOC), Base Cations (Ca2+, Mg2+, Na+, K+) and Cation Exchange Capacity (CEC), available Phosphorus (Av-P), available Nitrogen (Av-N), Soil pH, percentage sand, clay and silt. Mean soil properties were 3.5 mg/kg Av-p, 3.0 mg/kg Av-N, 28.3 % SOC, 5.1 pH, Bulk density 0.7 g/cm3 and the texture is sandy. The means base cations were 2.8, 1.8, 7.9 and 2.3 cmol/ kg for Na, K, Ca and Mg, respectively and CEC 82.5 cmol/kg. Av-P was the most variable property with CV ranging from 115 and 162 % in different soil depths while pH was the least variable with CV ranging from 6 and 12 %. The Nugget/Sill ratios were less than 56 %, indicating random heterogeneity. The semivariograms indicated moderate spatial dependence (25 < DSD ≤ 75%) for soil properties including SOC, Av-P, Av-N, pH and sand. Most properties indicate moderate spatial dependence and hence easily managed. Chemical properties were more variable than physical properties.
绘制水土壤性质的空间变异性以圈定卡龙-拉-lithunya湿地
湿地土壤的空间变异性提供了对潜在生态系统过程的洞察,并可能本身给出湿地状况的指示。从土壤水化特征出发,对卡龙-拉- lithunya湿地的土壤变异性进行了研究。在Khalong-la-Lithunya流域内的三个子流域进行了采样。在每个子集水区中,沿三个相距200米的样带每隔100米挖取土壤样品。根据USDA-NRCS(2010)手册对36个坑进行了详细的土壤剖面描述。取样深度90 cm,间隔15 cm,测定土壤有机碳(SOC)、碱性阳离子(Ca2+、Mg2+、Na+、K+)和阳离子交换容量(CEC)、速效磷(Av-P)、速效氮(Av-N)、土壤pH、砂、粘土和粉土百分比。平均土壤性质为3.5 mg/kg Av-p, 3.0 mg/kg Av-N, 28.3%有机碳,5.1 pH,容重0.7 g/cm3,质地为砂质。Na、K、Ca和Mg的平均碱阳离子分别为2.8、1.8、7.9和2.3 cmol/kg, CEC为82.5 cmol/kg。在不同土壤深度,v- p变化最大,CV值在115 ~ 162%之间,pH值变化最小,CV值在6% ~ 12%之间。Nugget/Sill比值小于56%,显示随机异质性。土壤有机碳、有机磷、有机磷氮、pH和沙粒的半变异图显示出中等的空间依赖性(25 < DSD≤75%)。大多数属性显示适度的空间依赖性,因此易于管理。化学性质比物理性质变化更大。
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