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作 者:王汝镛[1] 武志杰[1] 曹承绵[1] 刘永恩[1] 张素君[1] 张岫岚[1] 王春裕[1] 田林杰[1]
机构地区:[1]中国科学院沈阳应用生态研究所,辽宁沈阳110016
出 处:《土壤通报》2001年第z1期3-7,共5页Chinese Journal of Soil Science
摘 要:由中国科学院选定作为黄淮海平原农业综合开发的试验区之一的近代黄河三角洲山东省东营市的高盖镇与胜利乡,广泛分布着滨海氯化物盐渍化土壤,其土壤资源主要包括潮土、盐化潮土、潮盐土及盐化与脱盐,亟待开展改良利用的研究.Paddy soil was distributed widely in the neo-delta of Yellow River. The topography was low and flat, the groundwater table was high and salinization was serious . In the middle of 1980s, the neo-delta of Yellow River, which was selected as one of agricultural comprehensive experimental regions by CAS, was located in the Shengli village, Gaogei Town, Dongying City, Shandong Province. In this area, seaside chloride saline soil was distributed widely, the main soil type included fluvo-aquic soil, salinized fluvo-aquic soil, fluvo-aquic saline soil. The processes of salinization and desalinization both existed. The studies on the reformation and development were needed.
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