Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Hula Valley peat: review of chemical and geochemical aspects

Journal Article · · Soil Sci.; (United States)

In the Hula Valley, Israel, four layers of peat of Middle Pleistocene to Holocene age, interbedded with limnic clays and marls, are found above 300-m depth. The main detrital minerals are kaolinite, montmorillonite, and illite. Average elemental values of organic matter of dry peat are: C, 15-29 percent; H, 1.8-3 percent; N, 0.8-1.2 percent; S, 2.3-5 percent. The ash content (on dry basis) is 36-59 percent. The average calorific value ranges from 1670 to 3400 cal/g. Organic constituents isolated from the upper layer (Peat Horizon One) include: C/sub 12/ to C/sub 26/ fatty acids, ..beta..-sitosterol, ..beta..-sitostanol, friedelin and friedelanol, ceryl alcohol, a series of hydrocarbons, among them the polycyclic hydrocarbon, perylene, 13 amino acids and a series of polysaccharides of molecular weight in the range of 40,000. A detailed quantitative investigation of the distribution with depth in the top peat layer of the humic, fulvic, and hymatomelanic acids, as well as of the ..beta..-humus and humin, showed humin to be the dominant fraction of the organic matter. Its amount increases from 62 percent of the organic matter (by weight) at the surface to 70 to 90 percent at 2-m depth. The fulvic acid and polysaccharides show rapid decrease with depth, accompanied by concomitant increase in the ..beta..-humus. The humic acid increases with depth. Analysis of the peat organic fractions for carbon and hydrogen stable isotopes shows that with depth the difference in delta C/sup 13/ between the humic and fulvic acids disappears and the delta C/sup 13/ stabilizes at around -18 parts per thousand. The isotope data indicate the dynamic nature of the fulvic acid in the peat. The delta D values were around -60 parts per thousand, but the data are too meager for any firm conclusion.

Research Organization:
Hebrew Univ., Jerusalem
OSTI ID:
6874339
Journal Information:
Soil Sci.; (United States), Journal Name: Soil Sci.; (United States) Vol. 125:4; ISSN SOSCA
Country of Publication:
United States
Language:
English

Similar Records

Organic pollutant sorption onto dissolved and sorbed humics, fulvics and humin
Conference · Fri Dec 30 23:00:00 EST 1994 · OSTI ID:40057

Chemical and isotopic evidence for the in situ origin of marine humic substances
Journal Article · Sat Jul 01 00:00:00 EDT 1972 · Limnol. Oceanogr.; (United States) · OSTI ID:6504190

A model of humin
Journal Article · Fri Nov 30 23:00:00 EST 1990 · Environmental Science and Technology; (USA) · OSTI ID:5869501