湖南省不同地区表土分布特征及总体特征分析

    Analysis on distribution characteristics and general features of topsoil in different regions of Hunan Province

    • 摘要: 为明确湖南省不同区域0~30 cm 表土分布特征,分析适配的表土剥离工艺,并探讨湖南省土壤理化性质,为湖南省耕地质量提升、土壤资源保护与生产建设项目生态修复提供技术支撑。以洞庭湖平原、湘中丘陵、湘东山区、湘南山地、湘西山区五大典型地貌为研究对象,采用野外典型抽样混合采样、区域对比分析与室内理化测试的方法开展研究,通过测定 pH、有机质、氮磷钾、土壤质地、全镉等理化指标,分析湖南省不同地区表土分布特征及总体特征。结果表明:湖南省表土以红壤(51%)、水稻土(16.5%)、黄壤(12.6%)为主,三者合计占全省土壤面积80%以上;全省表土整体为强酸性~酸性(pH 4.5~6.5)、有机质中等~较高(20~40 g·kg−1)、磷普遍缺乏、氮含量中等的共同特征。但不同区域土壤障碍因子差异显著:洞庭湖平原土壤肥力高,局部发生潜育化、镉超标;湘中丘陵土壤黏重酸化,缺磷少钾,部分区域镉富集突出;湘东山区速效钾含量较高,水土流失严重;湘南山地土层偏薄,面临石漠化风险;湘西山区有机质含量全省最高,但冷浸田广布、土壤侵蚀明显。研究结果可为湖南省表土资源保护利用、土地复垦和耕地质量提升提供参考。

       

      Abstract: To clarify the distribution characteristics of 0-30 cm topsoil in different regions of Hunan Province, screen suitable topsoil stripping technologies, and reveal regional soil physicochemical properties, this study aims to provide technical support for the improvement of cultivated land quality, soil resource conservation, and ecological restoration of production and construction projects in Hunan Province. Taking five typical geomorphic units, namely the Dongting Lake Plain, Central Hunan Hilly Area, Eastern Hunan Mountainous Area, Southern Hunan Mountainous Area and Western Hunan Mountainous Area as research objects, field typical mixed sampling, regional comparative analysis and indoor physicochemical tests were adopted. Soil indicators including pH, organic matter, total nitrogen, available phosphorus, available potassium, soil texture and total cadmium were determined to analyze the regional and overall topsoil characteristics of Hunan Province. The results show that red soil(51%), paddy soil(16.5%)and yellow soil(12.6%)are the dominant soil types in Hunan Province, jointly accounting for more than 80 % of the total provincial soil area. The topsoil across the province is generally strongly acidic to slightly acidic(pH 4.5−6.5), with medium-to-high organic matter content(20−40g·kg−1), widespread phosphorus deficiency and medium total nitrogen content. Nevertheless, soil limiting factors vary greatly among regions. The Dongting Lake Plain features highly fertile topsoil, accompanied by local gleyization and cadmium pollution. The Central Hunan Hilly Area suffers from heavy soil texture, soil acidification, insufficient phosphorus and potassium, and prominent cadmium enrichment. The Eastern Hunan Mountainous Area has high available-potassium content yet severe soil-water loss. The Southern Hunan Mountainous Area is characterized by thin topsoil and rocky-desertification risks. The Western Hunan Mountainous Area boasts the highest organic-matter content in Hunan, but is troubled by widespread cold-waterlogged paddy fields and serious soil erosion. This study can offer scientific references for topsoil resource protection and utilization, land reclamation and cultivated-land-quality improvement in Hunan Province.

       

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