The Applicability of the Exposed Roots of Cupressus sempervirens L. var horizontalis for the Estimation of Soil Erosion in Hassan Abad, Mazandaran Province

Document Type : Research Paper

Authors

1 M.Sc., Department of Soil Sciences, Karaj Branch, Islamic Azad University, Karaj, Iran

2 Assistant Professor Faculty of Agriculture and Natural Resources Karaj Islamic Azad University IRAN

3 Assistant Professor, Department of Wood Sciences, Karaj Branch, Islamic Azad University, Karaj, Iran

Abstract

Anatomical changes of the exposed roots in Cupressus sempervirens L. var horizontalis were used to
estimate soil erosion in Hassan Abad valley, Chaloos, Iran. A total of 30 exposed roots, for five trees,
were used to estimate erosion. Cross-sections of 20 μm were papered and the first year of exposure by
erosion was identified. We finally estimated the mean annual erosion. The statistical relationship of
the mean annual erosion with the percentage of the plant coverage, geographical aspects and slopes
were investigated. The mean erosion of the study area has been estimated around 0.5 mm per year.
There was negative relationship between the annual erosion and slope as well as the percentage of the
plant coverage. The samples obtained in southern and western aspects showed higher annual erosions.
We concluded that anatomical changes of exposed roots of C. sempervirens are valuable tools to date
erosion events, however, the responses of diverse species under different types of erosion remains to
be studied in future.

Keywords


[1]. Alestalo, J. (1971). Dendrochronological interpretation of geomorphic processes. Fennia, 105: 1-140.
[2]. Bahrami, S.H., Mahboobi, F., Sadidi, J., and Jafari Aghdam, M. (2011). Estimating the rate of sheet erosion by dendrogeomorphological analysis of tree roots in Gharechai (Ramian) Catchment. Physical Geography Research, 75: 1-17.
[3]. Goudie, A.S. (2005). Encyclopedia of Geomorphology. London: Routledge Ltd
[4]. Bodoque, J.M., Díez-Herrero, J.F., Rubiales, J.M, Godfrey, A., Pedraza, J., Carrasco, R.M., and Sanz, M.A. (2005). Sheet erosion rates determined by using dendrogeomorphological analysis of exposed tree roots. Two examples from Central Spain. Carena, 64: 81-102.
[5]. Bégin, Y. (2001). Tree-ring dating of extreme lake levels at the Subarctic–Boreal interface. Quaternary Research, 55: 133-139.
[6]. Gärtner, H., Schweingruber, F.H., and Dikau, R. (2001). Determination of erosion rates by analyzing structural changes in the growth pattern of exposed roots. Dendrochronologia, 19: 81-91.
[7]. Gärtner, H. (2003). The applicability of roots in Dendrogeomorphology. In: Schleser G, Winiger M, Bräuning A, Gärtner H, Helle G, Jansma E, Neuwirth B, and Treydte K, editors . TRACE—Tree Rings in Archaeology, Climatology and Ecology, Bonn / Jülich, Germany pp124.
[8]. Gärtner, H. (2007). Tree Roots - Methodological Review and New Development in Dating and Quantifying Erosive Processes. Geomorphology, 86: 243-251.
[9]. Hebertson, E.G., and Jenkins, M.J. (2003). Historic climate factors associated with major avalanche years on the Wasatch Plateau, Utah. Cold Regions Science and Technology, 37: 315-332.
[10]. Perret, S., Stoffel, M., and Kienholz, H. (2006). Spatial and temporal rockfall activity in a forest stand in the Swiss Prealps - a dendrogeomorphological case study. Geomorphology, 74: 219-231.
[11]. Gers, E., Florin, N., Gärtner, H., Glade, T., Dikau, R., and Schweingruber, F.H. (2001). Application of shrubs for dendrogeomorphological analysis to reconstruct spatial and temporal landslide movement patterns a preliminary study. Zeitschrift fur Geomorphologie Upplementband, 125: 163-175.
[12]. Malik, I. (2005). Rates of lateral channel migration along the Mala Panew River (Southern Poland) based on dating riparian trees and coarse woody debris. Dendrochronologia, 23: 29-38.
[13]. Meyer, G.A. (2001). Recent  large-magnitude  floods  and  their  impact on valley-floor environments  of northeastern Yellowstone. Geomorphology, 40: 271-290.
[14]. Stefanini, M.C. (2004). Spatio-temporal analysis of a complex landslide in the Northern Apennines (Italy) by means of dendrochronology. Geomorphology, 63: 191-202.
[15]. Korpela, I. (2004) Individual tree measurements by means of digital aerial Photogrammetry, Silva Fennica, Monographs 3, 93 pp.
[16]. Avery, E.T. (1977) Interpretation of aerial photographs, Burgess Publication, USA, 392 pp.
[17]. Bayramzadeh, V., Funada, R., Kubo, T. (2008).Relationship between vessel element anatomy and physiological as well as morphological traits of leaves in Fagus crenata seedling originated from different provenances. Trees, 22: 217-224.
[18]. Fu, S., Liu, B., Liu, H., and Xu, L. (2011). The effect of slope on interrill erosion at short slopes. Catena, 84: 29-34.
[19]. Sadeghi, S.M.M., Basiri, R. and Firoozbakht, A. (2013). An assessment of Cupressus sempervirens L. var horizontalis stands in south of Zagros forest. First National Conference of Access Solution to the Sustainable Development in Agriculture, Natural Resources, and Environment. Tehran, Iran, pp 6.
[20]. Gyssels, G., Poesen, J., Bochet, E. and Li, Y. (2005). Impact of plant roots on the resistance of soils to erosion by water: A review. Progress in Physical Geography, 29: 189-217.
[21]. Jiao, J., Zou, H., Jia Y., and Wang, N. (2009). Research progress on the effects of soil erosion on vegetation. Acta Ecologica Sinica, 29: 85-91.