【摘要】 基于广东省1980s、2010年以及2015年3期土壤数据,对全省不同区域农田耕作层土壤pH值的时空变异特征进行分析,并初步探讨了可能导致土壤pH变化的因素.结果表明:不同时期广东全省土壤pH值空间分布格局变化显著.全省农田土壤在1980s—2010年间,pH整体下降了0.3,呈酸化趋势,2010—2015年,土壤pH上升了0.09,但不均匀势态有所增强,酸碱分化趋势较明显.从各区域看,1980s—2010年,各区域土壤均呈现酸化趋势; 2010—2015年,珠三角地区农田土壤pH均值上升了0.27,而东、西两翼土壤pH均值分别下降了0.05、0.15,山区土壤pH变化不明显.分析表明:广东省各地区土壤酸化除受土壤自身及降水等自然因素影响外,酸雨、不合理施肥以及高产作物高复种的种植结构等人为因素也是导致土壤酸化的主要原因;工业化、城市化、矿山开发和测土配方施肥的推广导致局部地区土壤pH值有所上升.研究结果可为不同区域控制缓解土壤酸化、提高耕地质量提供理论指导.更多还原

【Abstract】 Based on the three datasets from 1980 s,2010 and 2015 in Guangdong Province,we analyzed the spatial and temporal variations of soil pH in farmlands in different regions of Guangdong Province and analyzed the driving factors for such variations. The results showed that the spatial distribution of soil pH in Guangdong Province changed significantly in different periods. During1980 s to 2010,soil pH showed an acidification trend with a decline of 0.3,and increased by 0.09 from 2010 to 2015,with more uneven trend and more obvious acid base differentiation. From the perspective of each region,there was generally a trend of acidification from the 1980 s to 2010. From2010 to 2015,the average pH value of farmland soil in the Pearl River Delta increased by 0.27,while that on the east wing and west wing decreased by 0.05 and 0.15 respectively,showing a unapparent change of soil pH in the mountainous area. Our results showed that soil acidification in different areas of Guangdong Province was affected by natural factors such as soil itself and precipitation.In addition,anthropogenic factors such as acid rain,unreasonable fertilization and the planting structure of high-yielding crops were also the main causes of soil acidification. Industrialization,urbanization,mining development,and the spread of soil testing formula fertilization increased soil pH in local areas. Our results could provide theoretical guidance for controlling and alleviating soil acidification and improving the quality of cultivated land in different areas.更多还原