Development and magnetic properties of loess-derived forest soils along a precipitation gradient in northern Iran Development and magnetic properties of loess-derived forest soils along a precipitation gradient in northern Iran

最小化 最大化

Vol16 No.8: 1848-1868

Title】Development and magnetic properties of loess-derived forest soils along a precipitation gradient in northern Iran

Author】Masoumeh POURMASOUMI1; Farhad KHORMALI1*; Shamsollah AYOUBI2; Martin KEHL3; Farshad KIANI1

Addresses】1 Department of Soil Science, Faculty of Water and Soil Engineering, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran; 2 Department of Soil Science, College of Agriculture, Isfahan University of Technology, 84156-83111 Isfahan, Iran; 3 Institute of Geography, University of Cologne, Albertus-Magnus-Platz, D-50923 Cologne, Germany

Corresponding author】Farhad KHORMALI

Citation】Pourmasoumi M, Khormali F, Ayoubi S, et al. (2019) Development and magnetic properties of loess-derived forest soils along a precipitation gradient in northern Iran. Journal of Mountain Science 16(8). https://doi.org/10.1007/s11629-018-5288-4

DOI】https://doi.org/10.1007/s11629-018-5288-4

Abstract】In order to investigate the development of forest soils formed on loess, six representative modern soil pedons were selected along a precipitation gradient extending from eastern Golestan (mean annual precipitation, MAP = 500 mm) to eastern Mazandaran Provinces (MAP = 800 mm). Physiochemical, micromorphological and magnetic properties, as well as clay mineralogy of soils were studied using standard methods. Soils are mainly classified as Alfisols and Mollisols. Downward decalcification and the subsequent clay illuviation were the main criteria of soil development in all study areas. Pedogenic magnetic susceptibility of pedons studied varied systematically across the precipitation gradient in Northern Iran, increasing from 14.66 × 108 m3 kg1 at the eastern part to 83.75 × 108 m3 kg1 at the western margin of this transect. The frequency-dependent magnetic susceptibility showed an increasing trend with rainfall as well. The micromorphological study of soils indicated that there is a positive relationship between climate gradient (increasing rainfall) and the micromorphological index of soil development (MISECA). The area and thickness of clay coatings showed an increasing trend with rainfall. Grain size analysis indicates that pedogenic processes are responsible for changing original grain size distribution of loess in our soils. The correlation achieved among modern soil properties and precipitation could be applied to the buried paleosols in the whole study area to refer degree of paleosol development and to reconstruct the paleoclimate.

Keywords】Magnetic properties; Soil formation;Weathering; Precipitation gradient; Loess; Iran