Abstract
Abstract P type humic acid has absorption bands near 615, 570 and 450mµ in the visible region, and is a common component of many soils in north temperate regions (1, 2, 3). Its unusual spectral characteristics are due to a green fraction (Pg), which can be separated from the humic acid dissolved in aqueous alkali by chromatography on Sephadex or cellulose powder, and is precipitated as a reddish-brown substance on acidification (2). In aqueous alkali, it has λmax at 613, 568, 448, 430 (infl.) and 281mµ. The distribution of Pg in different soils is probably related to the presence of fungal sclerotia. The highest content of Pg in p type humic acid is about 10%. We have now obtained evidence that the characteristic colour of Pg is due to the presence of a derivative of 4,9 - dihydroxyperylene - 3,10 - quinone.
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