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阔叶和杉木人工林对土壤碳氮库的影响比较
引用本文:万晓华,黄志群,何宗明,胡振宏,杨靖宇,余再鹏,王民煌. 阔叶和杉木人工林对土壤碳氮库的影响比较[J]. 应用生态学报, 2013, 24(2): 345
作者姓名:万晓华  黄志群  何宗明  胡振宏  杨靖宇  余再鹏  王民煌
作者单位:(;1.湿润亚热带山地生态国家重点实验室培育基地, 福州 350007; ;2.福建师范大学地理科学学院, 福州 350007; ;3.福建农林大学林学院, 福州 350002)
基金项目:2011教育部新世纪优秀人才计划项目
摘    要:通过比较我国亚热带地区19年生阔叶人工林和杉木人工林土壤碳氮储量,探讨树种对土壤碳氮库的影响.结果表明:阔叶人工林0~40 cm土层碳储量平均为99.41 Mg·hm-2,比杉木人工林增加33.1%;土壤氮储量为6.18 Mg·hm-2,比杉木人工林增加22.6%.阔叶人工林林地枯枝落叶层现存量、碳和氮储量分别是杉木人工林的1.60、1.49和1.52倍,两个树种的枯落叶生物量、碳和氮储量均有显著差异.枯枝落叶层碳氮比值与土壤碳、氮储量之间呈显著负相关.阔叶人工林细根生物量(0~80 cm)是杉木林的1.28倍,其中0~10 cm土壤层细根生物量占48.2%;阔叶人工林细根碳、氮储量均高于杉木人工林.在0~10 cm土层,细根碳储量与土壤碳储量具有显著正相关关系.阔叶树种比杉木的土壤有机碳储存能力更大.

关 键 词:杉木  土壤碳  土壤氮  枯枝落叶层  细根

Effects of broadleaf plantation and Chinese fir (Cunninghamia lanceolata) plantation on soil carbon and nitrogen pools
WAN Xiao-hua,HUANG Zhi-qun,HE Zong-ming,HU Zhen-hong,YANG Jing-yu,YU Zai-peng,WANG Min-huang,. Effects of broadleaf plantation and Chinese fir (Cunninghamia lanceolata) plantation on soil carbon and nitrogen pools[J]. The journal of applied ecology, 2013, 24(2): 345
Authors:WAN Xiao-hua  HUANG Zhi-qun  HE Zong-ming  HU Zhen-hong  YANG Jing-yu  YU Zai-peng  WANG Min-huang  
Affiliation:(;1.Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China; ;2.School of Geographical Science, Fujian Normal University, Fuzhou 350007, China; ;3.Forestry College of Fujian Agriculture and Forestry University, Fuzhou 350002,China)
Abstract:A comparative study was conducted on the soil C and N pools in a 19 year-old broadleaf plantation and a Chinese fir (Cunninghamia lanceolata) plantation in subtropical China, aimed to understand the effects of tree species on the soil C and N pools. In the broadleaf plantation, the C and N stocks in 0-40 cm soil layer were 99.41 Mg·hm-2 and 6.18 Mg·hm-2, being 33.1 % and 22.6 % larger than those in Chinese fir plantation, respectively. The standing biomass and the C and N stocks of forest floor in the broadleaf plantation were 1.60, 1.49, and 1.52 times of those in Chinese fir plantation, respectively, and the differences were statistically significant. There was a significant negative relationship between the forest floor C/N ratio and the soil C and N stocks. In the broadleaf plantation, the fine root biomass in 0-80 cm soil layer was 1.28 times of that in the Chinese fir plantation, and the fine root biomass in 0-10 cm soil layer accounted for 48.2 % of the total fine root biomass. The C and N stocks in the fine roots in the broadleaf plantation were also higher than those in the Chinese fir plantation. In 0-10 cm soil layer, its C stock had a significant positive relationship with the fine root C stock. It was suggested that as compared with Chinese fir plantation, the soil in broadleaf plantation had a greater potential to accumulate organiccarbon.
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