引用本文: | 廖 珂, 沈芳芳, 刘文飞, 孟庆银, 童 浩, 陈官鹏, 徐 晋, 樊后保.长期氮沉降下杉木人工林凋落物与土壤的C、N、P化学计量特征[J].广西植物,2020,40(11):1551-1562.[点击复制] |
LIAO Ke, SHEN Fangfang, LIU Wenfei, MENG Qingyin,
TONG Hao, CHEN Guanpeng, XU Jin, FAN Houbao.C, N and P stoichiometric characteristics of litterfall and soil in a Chinese fir plantation under long-term nitrogen deposition[J].Guihaia,2020,40(11):1551-1562.[点击复制] |
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长期氮沉降下杉木人工林凋落物与土壤的C、N、P化学计量特征 |
廖 珂1, 沈芳芳1, 刘文飞1, 孟庆银2, 童 浩3, 陈官鹏1, 徐 晋1, 樊后保1*
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1. 南昌工程学院, 生态与环境科学研究所/江西省退化生态系统修复与流域生态水文重点实验室, 南昌 330099;2. 福建省沙县官庄国有林场, 福建 沙县 365503;3. 福建省三明市郊国有林场, 福建 三明 365000
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摘要: |
为研究长期氮沉降条件下林木凋落物与土壤养分之间的关系,该文以亚热带杉木(Cunninghamia lanceolata)人工林为研究对象,分析了模拟氮沉降处理第12年时杉木林凋落物不同组分(叶、枝、果)与不同土层土壤(0~20 cm、20~40 cm、40~60 cm)的C、N、P含量及其化学计量比。氮沉降处理分4个水平,分别为N0(0 kg N·hm-2·a-1)、N1(60 kg N·hm-2·a-1)、N2(120 kg N·hm-2·a-1)、N3(240 kg N·hm-2·a-1),每处理重复3次。结果表明:(1)凋落物各组分的C、N、P含量及其化学计量比均高于土壤; 凋落物和土壤化学计量比均表现为C/P>C/N>N/P; 凋落物不同组分的C、N含量表现为叶>果>枝,而P含量表现为叶>枝>果。(2)12 a氮沉降增加了凋落物叶、枝和果的N含量,增幅分别为4.24%、15.97%、6.47%; 同时增加了凋落物枝N/P,降低了凋落物枝C含量、C/N和C/P; 中-高氮沉降(N2、N3)增加了土壤N含量,低氮沉降(N1)增加了土壤C/P、N/P。(3)相关性分析表明凋落物N与土壤N显著正相关,土壤C/P与凋落物C/P、N/P显著负相关,土壤P与凋落物N/P显著负相关。综上结果说明凋落物N是土壤N的重要N素来源之一,而土壤N可能是决定长期氮沉降后凋落物N/P的主要因素。 |
关键词: 氮沉降, 生态化学计量, 凋落物, 土壤, 杉木人工林 |
DOI:10.11931/guihaia.gxzw201911016 |
分类号:Q948.15 |
文章编号:1000-3142(2020)11-1552-12 |
基金项目:国家自然科学基金(31960308,31360175); 福建省三明市林业科学技术研究项目(2018-N-6); 南昌工程学院2019年国家大学生创新创业训练计划项目(201902); 南昌工程学院2019年度研究生创新计划项目(201904)[Supported by the National Natural Science Foundation of China(31960308, 31360175); Sanming Forestry Science and Technology Research Program of Fujian Province(2018-N-6); 2019 National Innovation and Entrepreneurship Training Program for College Student in Nanchang Institute of Technology(201902); 2019 Gradute Innovation Program of Nanchang Institute of Technology(201904)]。 |
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C, N and P stoichiometric characteristics of litterfall and soil in a Chinese fir plantation under long-term nitrogen deposition |
LIAO Ke1, SHEN Fangfang1, LIU Wenfei1, MENG Qingyin2,
TONG Hao3, CHEN Guanpeng1, XU Jin1, FAN Houbao1*
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1. Jiangxi Provincial Key Laboratory for Restoration of Degraded Ecosystems &2.Watershed Ecohydrology/Research Institute of Ecology &3.Environmental Sciences, Nanchang Institute of Technology, Nanchang 330099, China;4.2. Guanzhuang National Forest Farm of
Shaxian, Shaxian 365503, Fujian, China;5.3. Shijiao National Forest Farm of Sanming, Sanming 365000, Fujian, China
1. Jiangxi Provincial Key Laboratory for Restoration of Degraded Ecosystems & Watershed Ecohydrology/Research Institute of Ecology &
Environmental Sciences, Nanchang Institute of Technology, Nanchang 330099, China; 2. Guanzhuang National Forest Farm of
Shaxian, Shaxian 365503, Fujian, China; 3. Shijiao National Forest Farm of Sanming, Sanming 365000, Fujian, China
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Abstract: |
To reveal the relationship between forest litterfall and soil under long-term nitrogen(N)deposition, litterfall and soil samples were collected in the 12th year of nitrogen deposition in a Chinese fir(Cunninghamia lanceolata)plantation. C, N, and P concentrations and stoichiometric characteristics of litterfall(leaf, branch and fruit)and soil(0-20 cm, 20-40 cm, 40-60 cm)were analyzed. Four simulated nitrogen deposition treatment levels were N0(0 kg N·hm-2·a-1), N1(60 kg N·hm-2·a-1), N2(120 kg N·hm-2·a-1)and N3(240 kg N·hm-2·a-1), respectively. Each treatment comprised three replicate plots of 20 m × 20 m which were sprayed with urea on the forest floor at the beginning of each month. The results were as follows:(1)C, N and P contents and stoichiometric ratios of litterfall were higher than that of soil. The stoichiometric ratios of litterfall showed the same order as soil of C/P>C/N>N/P; The C, N contents of litterfall decreased in the order of leaf > fruit > branch, while P decreased in the order of leaf > branch > fruit.(2)N deposition promoted N content in litterfall leaf(+4.24%), branch(+15.97%), and fruit(+6.47%), respectively; N deposition increased N/P while decreased C content, C/N and C/P in litterfall branch; Medium-high level of N deposition(N2 and N3)increased soil N content, and low level of N deposition(N1)increased soil C/P and N/P.(3)Significant positive correlation existed between litterfall N and soil N, while negative correlation between soil C/P and litterfall C/P, N/P, and between soil P and litterfall N/P. It is indicated that litterfall N was one of the important soil N sources, and soil N content mainly influencing the ratio of litterfall N/P after long-term N deposition. |
Key words: nitrogen deposition, ecological stoichiometry, litterfall, soil, Cunninghamia lanceolata plantation |
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