TY - JOUR JF - JSTNAR JO - jwss VL - 21 IS - 1 PY - 2017 Y1 - 2017/6/01 TI - Using Nuclear Magnetic Resonance 1H and 13C in soil organic matter covered by forest TT - استفاده از روش رزونانس مغناطیسی هسته 1H و 13C در مطالعه کربن آلی خاک تحت پوشش درختان جنگلی N2 - Soil organic matter is the largest source of organic carbon in the soil surface which played an enormous role in restoring balance, environmental sustainability, soil elements and climatic conditions. Organic materials influence physical, chemical and biological properties of soil and thus soil fertility directly and indirectly. The amount, type and composition of organic matter are different in different soil and climatic conditions. Different soil components can hold different combination of soil organic matter. In this study soil samples were collected from virgin, Populus and Alnus forests from Guilan Province, Iran. The amount of organic matter in the original samples and sand, silt and clay fractions were measured and the quality of organic carbon (13C) and hydrogen (1H) were determined in fractions by Nuclear Magnetic Resonance. Based on the results the amount of organic carbon in the original samples of Alnus forest was highest. among fractions, clay had the highest amount of organic carbon. The result of Nuclear Magnetic Resonance showed presence of different aliphatic and aromatic carbons and hydrogen in different samples. Virgin forest had the highest proportion of alkyl to oxygenated alkyl carbon ratio and Alnus forest showed the highest ratio of aliphatic to aromatic carbon,. Both mentioned ratios was higher in clay fraction than other two fractions. SP - 83 EP - 92 AU - nadi, M. AU - Golchin, A. AU - Sedaghati, E. AU - Shafie, S. AU - Hosseini fard, S. J. AU - Füleky, G. AD - 1. Dept. of Soil Sci. and Agric. Chemistry, Institute of Environ. Sci., Szent Istvan Univ., Godollo. Hungary. KW - Virgin forest KW - Alnus forest KW - Populus forest KW - Nuclear Magnetic Resonance KW - organic carbon UR - http://jstnar.iut.ac.ir/article-1-2734-en.html DO - 10.18869/acadpub.jstnar.21.1.83 ER -