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- W3147222788 abstract "专业，踪迹和红土侧面的器官的元素在海南岛上在晚第三纪暗岩上发展了，华南被报导在热带区域调查元素动员和再分配。结果显示强壮的酸环境和有机物(OM ) 能显著地改进不可溶解的元素的转移。在所有元素之中， Th 是最不活动的。至于一般保守元素，在早期的化学捱过期间，移动例如 Ti， Zr， Hf 和 Nb，直到在上面的侧面的 30%40% 。并且为 Fe，艾尔， Cu 和 Ni，趋于与第二等的矿物质被相结合并且在适度的地区被保留，他们从上面的侧面被移开，向下转了，然后在更低的侧面猛抛。另外，包括海盐喷雾器和灰尘，大气的输入在产生沥滤的元素的预算上有深刻效果损失(例如 K， Na 和 Sr ) 。排除地下水的可能性并且和 Sr/Th ， K/Th 和 Na/Th 比率的百分比变化的戏剧性地向上的增加的趋势，在上面的侧面的侵蚀， K 的显著增加， Na 和 Sr 集中显示出那大气的输入，特别海盐喷雾器，贡献体外的海水导出元素，例如到土壤的 K ， Na 和 Sr 。在这侧面的全面元素的行为建议那有机物，大气的输入在在热带区域的极端捱过期间在元素的动员和再分配起一个很重要的作用。" @default.
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- W3147222788 date "2014-01-01" @default.
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- W3147222788 title "Mobilization and redistribution of elements in soils developed from extreme weathering basalt on Hainan Island" @default.
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