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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Application of cosmogenic 10Be to dating soils on the raised coral reef terraces of Kikai Island, southwest Japan.
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Application of cosmogenic 10Be to dating soils on the raised coral reef terraces of Kikai Island, southwest Japan.

机译:宇宙成因10Be在日本西南部Kikai岛凸起的珊瑚礁阶地上的约会土壤中的应用。

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摘要

10Be concentrations of six soils on the raised coral reef terraces of Kikai Island, southwest Japan range from 0.80 to 7.17x109 atoms g-1. The annual deposition rate of 10Be from the atmosphere to Kikai Island from 2000 to 2002 ranges from 2.0 to 3.5x106 atoms cm-2 year-1, with a mean of 2.8+or-0.7x106 atoms cm-2 year-1. Minimum absolute ages, calculated from the inventory of meteoric 10Be in the soils and the annual deposition rate of 10Be, are: Initial Rendzina-like soil, >=8 ka; Rendzina-like soil, >=18 ka; Brown Rendzina-like soil, >=56 ka; Terra fusca-like soil, >=127 ka; Terra rossa-like soil, >=136 ka; and Intergrade between Terra rossa-like and Red-Yellow soil, >=102 ka. Therefore, it was concluded that soil formation during the first ~60 000 years would be as Rendzina-like soils and more than ~100 000 years would be required for Red-Yellow soils to develop on raised coral reef terraces under subtropical humid climatic conditions.
机译:在日本西南部奇凯岛的珊瑚礁阶地上,六种土壤的10Be浓度范围为0.80至7.17x109原子g-1。 2000年至2002年,从大气到基凯岛的10Be年沉积速率范围为2.0至3.5x106原子cm-2年-1,平均2.8+或-0.7x106原子cm-2年-1。根据土壤中10Be的平均存量和10Be的年沉积速率计算的最小绝对年龄为:初始Rendzina样土壤,> = 8 ka; Rendzina样土壤,> = 18 ka;棕色Rendzina样土壤,> = 56 ka; Terra fusca样土壤,> = 127 ka; Terrarossa样土壤,> = 136 ka;以及Terra rossa样和红黄土之间的过渡带,> = 102 ka。因此,得出的结论是,在亚热带湿润气候条件下,最初的约60 000年的土壤形成将类似于Rendzina样的土壤,而红黄土壤在凸起的珊瑚礁阶地上发育则需要约100 000年以上。

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