Deuterium Content of Peat as a Paleoclimatic Recorder
Deuterium Content of Peat as a Paleoclimatic Recorder
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泥炭的氘含量作为古气候记录器
作者：
W. Schiegl
在植物物质转化为泥炭的过程中，初始氢浓度随碳含量的增加而系统地降低。根据这个关系式，可以得出在荷兰泥炭沼泽中形成泥炭的植物的原始氚含量，所获得的值可以与荷兰过去的夏季气温相关联。
During the transformation of vegetable matter into peat the initial deuterium concentration decreases systematically with increasing carbon content. From this relationship the original deuterium content of the plants that formed the peat in Dutch peat bogs can be derived, and the values obtained can be correlated with past summer temperatures in the Netherlands.