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沼泽的泥炭堆积率对研究泥炭的成因和分布规律以及进行工业评价具有重要意义,早就受到重视,并提出了几种计算方法。其中有植物生长率法(Kac,1936)和孢粉法(Durno,1961、Veber,1967、Valk,1971)、C~(14)法(G、B、Rigg等,1957)、标桩法(D.S.Ranwell,1964)和Pb~(210)法(T.V.Armentano,G.W.Woo-dwell,1975)等。所求得的欧亚大陆及美国等地的一些沼泽的泥炭平均年堆积率多为零点几毫米至几毫米。
The marsh peat accumulation rate has great significance for studying the genesis and distribution of peat as well as for industrial evaluation. Several calculation methods have been put forward. Among them are the plant growth rate (Kac 1936) and sporopollen (Durno 1961, Veber 1967, Valk 1971), C 14 (G, B, Rigg et al 1957) DSRanwell, 1964) and Pb ~ (210) method (TVArmentano, GWWoo-dwell, 1975). The average annual accumulation of peat in some swampy peatlands in Eurasia and the United States is mostly from a few millimeters to a few millimeters.