首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Effect of vegetation switch on soil chemical properties
Authors:Noriko Iwashima  Tsugiyuki Masunaga  Reiji Fujimaki  Ayu Toyota  Ichiro Tayasu  Tsutom Hiura
Institution:1. Faculty of Life and Environmental Science , Shimane University , Matsue , Shimane 690-8504 , Japan iwashima@life.shimane-u.ac.jp;3. Faculty of Life and Environmental Science , Shimane University , Matsue , Shimane 690-8504 , Japan;4. Institute of Soil Biology, Biology Centre, Academy of Sciences of Czech Republic , Na Sádkách 7, 370 05 , ?eské Budějovice , Czech Republic;5. Center for Ecological Research , Kyoto University , 509-3, 2, Otsu , Shiga 520-2113 , Japan;6. Tomakomai Research Station, Field Science Center for Northern Biosphere , Hokkaido University , Tomakomai , Hokkaido 053-0035 , Japan
Abstract:Soil chemical properties were investigated under four types of forest to evaluate the effect of replacement of tree species on soil chemical properties in the north of Japan. Two sites had undergone a vegetation switch around 1960 from broadleaved to coniferous trees (BC) and coniferous to broadleaved trees (CB), while the other two sites had had no vegetation change and carried broadleaved trees (BB) and coniferous trees (CC). Soil samples from the four sites were analyzed for pH (water, H2O), electrical conductivity (EC), total carbon (C) and nitrogen (N) content, exchangeable cations Ex. calcium (Ca), magnesium (Mg), potassium (K) and sodium (Na)], inorganic nitrogen (Inorg-N), nitrogen mineralization potential, total phosphorus (P), and available phosphate. Most of the soil chemical properties in both the upper (0–5?cm) and lower (5–10?cm) layers at the BC site had lower values than those at the BB site. Values of soil chemical properties in the upper and lower soil layers were similar at the BC and CC sites. pH, Inorg-N, EC, Ex.Ca and Ex.Mg in the upper layer at the CB site were significantly higher than those at CC site, whereas all soil properties at the CB site except for Inorg-N were similar to those at the BB site. In the lower layer at the CB site, values of soil chemical properties except for the C/N ratio were almost the same as those at the CC site, but lower than those at the BB site. The upper soil layer at sites where a vegetation switch had occurred was affected by the current tree species, whereas in the lower soil layer, the effects differed between the different vegetation switch patterns. At the CB site, where the vegetation switch was from coniferous to broadleaved trees, the soil chemical properties in the lower layer remained similar to those at the coniferous site (CC) 50 years after the vegetation switch, while changes in soil properties have occurred following the switch from broadleaved to coniferous trees. The change in soil nutrient content by vegetation switch was considerably affected by change in not only litter quality but also composition of earthworm community. In particular, a combination of epigeic and endogeic earthworms exhibited important roles for nutrient dynamics to the deeper soil layer.
Keywords:earthworm  litter  nutrient cycling  soil chemical properties  vegetation switch  
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号