Pardini Giovanni, Gispert Maria, Dunjó Gemma
Soil Science Unit, University of Girona, Avda. Luis Santalo s/n, 17003 Girona, Spain.
Sci Total Environ. 2003 Jun 20;309(1-3):213-24. doi: 10.1016/S0048-9697(03)00007-X.
We investigated the influence of agricultural management and various plant covers related to the period of abandonment on soil properties, erosion and nutrient depletion in a typical Mediterranean area with sandy loam shallow soils. Cultivated soils (CS) with insufficient management, 5 year abandoned soils covered with meadow (A5), 25 year abandoned soils covered with dense scrubs (A25), 50 year abandoned soils covered with cork trees (A50) and soils in a 50 year pine reforested area (P50) were studied over a period of 6 months (May-October 1999). The soils were classified as Lithic Xerorthents. Both the differences in soil properties and response to rainfall events were mainly attributed to the different vegetation types and stages in land management. Principal components analysis (PCA) was performed on the results, by running the overall data determined after five rainfall events. The factors extracted by PCA of the samples by variables matrix represented the response of the environments to different rainfall intensities as a function of management or natural evolution after abandonment. CS environments showed the highest runoff and sediment yield as well as the highest amount of dissolved organic carbon (DOC) and nitrogen in runoff water. The sequence of abandonment (A5, A25 and A50) showed approximately the same runoff production, whereas eroded sediments (ES) and DOC were inversely correlated. Organic carbon in the ES and DOC in runoff water always increased with the period of abandonment, which accounted for consistent nutrient depletion. Nevertheless, the A50 environment (dominated by Quercus suber) showed the best soil properties, whilst the A25 environment with dense cover of Cistus monspeliensis and Calicotome espinosa seemed to cause a worsening effect on the soil's physical and chemical properties. This is probably because these environments are more severely damaged by wild fire occurrence. In terms of sediment yield, the P50 environment followed CS environment, indicating that reforestation followed by insufficient forest management may negatively affect both soil properties and response to the erosive action of rainfall.
我们在一个典型的地中海地区,针对沙壤土浅层土壤,研究了农业管理以及与弃耕期相关的各种植物覆盖对土壤性质、侵蚀和养分耗竭的影响。研究对象包括管理不善的耕地土壤(CS)、覆盖着草地的弃耕5年土壤(A5)、覆盖着茂密灌丛的弃耕25年土壤(A25)、覆盖着栓皮栎的弃耕50年土壤(A50)以及50年松树重新造林区域的土壤(P50),研究时间为6个月(1999年5月至10月)。这些土壤被归类为石质旱成土。土壤性质的差异以及对降雨事件的响应主要归因于不同的植被类型和土地管理阶段。通过对五次降雨事件后测定的总体数据进行主成分分析(PCA)。由变量矩阵对样本进行PCA提取的因子代表了环境对不同降雨强度的响应,这是管理或弃耕后自然演变的函数。CS环境显示出最高的径流和产沙量,以及径流水中溶解有机碳(DOC)和氮的最高含量。弃耕序列(A5、A25和A50)显示出大致相同的径流产生量,而侵蚀沉积物(ES)和DOC呈负相关。ES中的有机碳和径流水中的DOC总是随着弃耕期的延长而增加,这导致了持续的养分耗竭。然而,A50环境(以栓皮栎为主)显示出最佳的土壤性质,而以蒙氏岩蔷薇和刺叶金合欢密集覆盖的A25环境似乎对土壤的物理和化学性质产生了恶化影响。这可能是因为这些环境更容易受到野火的严重破坏。就产沙量而言,P50环境仅次于CS环境,这表明造林后森林管理不善可能会对土壤性质和对降雨侵蚀作用的响应产生负面影响。