Morphology, chemical properties, and radiocarbon dating of eutrophic peat in Turkey

• Published in: Catena (Giessen) Vol. 85; no. 3; pp. 215 - 220
• Main Authors: Cayci, G., Baran, A., Ozaytekin, H., Kutuk, C., Karaca, S., Cicek, N.
• Format: Journal Article
• Language: English
• Published: Cremlingen-Destedt Elsevier B.V 01.06.2011; Catena
• Subjects: Accretion rate; Asia; Bgi / Prodig; cadmium; calcium; cation exchange capacity; chromium; Classification; copper; Degradation; Environment; groundwater; Haplohemists; Haplosaprists; iron; lead; magnesium; manganese; mercury; nickel; nitrogen content; nutrients; organic matter; organic soils; peat; Peat formation; peatlands; phosphorus; Physical geography; radiocarbon dating; soil horizons; soil sampling; Southwest Asia; zinc; Turkey; Peat formation; Degradation; Environment; Accretion rate; Classification; C 14 dating; Soil properties; Environmental degradation; Geochemistry; Nutrient; Heavy metals; Peat bog
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2011.01.005

Morphologies, classifications, chemical properties and radiocarbon dates of Akgöl–Sakarya peatland located in the northwestern part of Turkey, which has never been studied up to now, were investigated. Three representative profiles were excavated in the study area and soil samples were taken based on soil horizons. Additionally, soil samples were taken at the different depths in each profile for radiocarbon dating. Accretion rates changed between 1.40 and 1.69 mm year − 1 according to 14C measurements. Radiocarbon ages ranged between 365 ± 90 and 195 ± 50 years depending on sampling depth. Profile I was Sapric Haplohemist, profile II was Hydric Haplohemist and profile III was Typic Haplosaprist. Soil properties varied widely depending on the profiles. Fibre contents were between 9.4% and 34.7% due to degree of organic matter decomposition. pH and ECe values varied between 4.20–6.62 and 0.51–2.50 dS m −1, respectively. The cation exchange capacity (CEC) ranged from 100 to 140 cmol kg −1. Total nitrogen and phosphorus ranged from 0.78% to 1.82% and from 0.45% to1.03%, respectively. Total calcium contents were between 1.44% to 3.25%, and magnesium contents varied from 0.22 to 0.71%. Both nutrients were higher in the surface horizons of profiles I and II. Total Fe, Mn, Zn, Cu and B contents varied considerably among profiles. It was found that total amounts of Fe, Zn, Cu and B in samples were between 4660–16220 mg kg − 1 , 89–451 mg kg − 1 , 16–57 mg kg − 1 , 3–11 mg kg − 1 and 12–37 mg kg − 1 , respectively. Cr, Ni and Pb contents in peat samples were 22–55 mg kg − 1 , 24–58 mg kg − 1 , and 3–93 mg kg − 1 , respectively. However, there was no Cd and Hg detected. It was observed that seasonal ground water fluctuations, eutrophic formation and differences in decomposition degrees have a substantial effect on changing of morphological and chemical properties of organic soils in the study area. ► Accretion rates of peats varied between 1.40 and 1.69 mm year –1. ► Profiles were Sapric Haplohemist, Hydric Haplohemist and Typic Haplosaprist. ► Radiocarbon ages were between 195 and 365 years before present time. ► Ground water fluctuations have a substantial effect on properties of organic soils.