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dc.contributor.author郭剑芬
dc.contributor.author杨玉盛
dc.contributor.author陈光水
dc.contributor.author林鹏
dc.date.accessioned2017-11-14T02:47:28Z
dc.date.available2017-11-14T02:47:28Z
dc.date.issued2005-03-30
dc.identifier.citationJournal of Forestry Research,2005,(01):20-23,85
dc.identifier.issn1007-662X
dc.identifier.otherLYYJ200501004
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/154586
dc.description.abstract尽管溶解有机碳(DOC)和溶解有机氮(DON)在森林养分循环中的作用日渐为人们所关注,但对它们的浓度及动态,特别是对亚热带森林DOC 和DON 的研究甚少。本文于2002 年通过野外天然降水及亚热带木荷和杉木人工林(monoculture plantations of Schima superba and Cunninghamia lanceolata,15 年生)穿透雨和树干茎流各水样的收集及室内各水样中DOC、NO3 -N、NH4 -N 和总溶解有机氮(TDN)浓度的测- +定,其中DON 浓度通过TDN 与NO3 -N、NH4 -N 的浓度差值来计算,- +结果表明,天然降水DOC 和DON 浓度分别为1.7 和0.13 mg·L-1。木荷人工林穿透雨DOC 和DON 浓度分别为11.2 和0.24 mg·L-1,高于杉木人工林的DOC 和DON 浓度(10.3 和0.19 mg·L-1)。杉木人工林树干茎流DOC 和DON 浓度(分别为19.1 和0.66 mg·L-1)明显高于木荷人工林(分别为17.6 和0.48 mg·L-1)。天然降水DOC 浓度的月变化不明显,而DON 浓度在夏季和秋季较高。两林分穿透雨DON 浓度的月动态与树干茎流的十分相似,均在雨季开始时(3 月)浓度增大。两林分穿透雨DOC 浓度在2-4 月间较高,而树干茎流DOC 浓度在9-11 月间较高。图4表2 参24。
dc.description.abstractDespite growing attention to the role of dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) in forest nutrient cycling, their monthly concentration dynamics in forest ecosystems, especially in subtropical forests only were little known. The goal of this study is to measure the concentrations and monthly dynamics of DOC and DON in precipitation, throughfall and stemflow for two planta- tions of Schima superba (SS) and Chinese fir (Cunninghamia lanceolata, CF) in Jianou, Fujian, China. Samples of precipitation, throughfall and stemflow were collected on a rain event base from January 2002 to December 2002. Upon collection, all water samples were analyzed for DOC, NO3 -N, NH4 -N and total dissolved N (TDN). DON was calculated by subtracting NO3 -N and NH4 -N from TDN. The results - + - + showed that the precipitation had a mean DOC concentration of 1.7 mg·L-1 and DON concentration of 0.13 mg·L-1. The mean DOC and DON concentrations in throughfall were 11.2 and 0.24 mg·L-1 in the SS and 10.3 and 0.19 mg·L-1 in the CF respectively. Stemflow DOC and DON concentrations in the CF (19.1 and 0.66 mg·L-1 respectively) were significantly higher than those in the SS (17.6 and 0.48 mg·L-1 respectively). No clear monthly variation in precipitation DOC concentration was found in our study, while DON concentration in precipita- tion tended to be higher in summer or autumn. The monthly variations of DON concentrations were very similar in throughfall and stemflow at both forests, showing an increase at the beginning of the rainy season in March. In contrast, monthly changes of the DOC concentrations in throughfall of the SS and CF were different to those in stemflow. Throughfall DOC concentrations were higher from February to April, while relatively higher DOC concentrations in stemflow were found during September-November period.
dc.description.sponsorshipThis study was supported by the Teaching and Research Award program for MOE P. R. C. (TRAPOYT).
dc.language.isozh_CN
dc.subject溶解有机碳(DOC)
dc.subject溶解有机氮(DON)
dc.subject天然降水
dc.subject穿透雨
dc.subject树干茎流
dc.subject木荷
dc.subject杉木
dc.subject人工林
dc.subjectDissolved organic carbon (DOC)
dc.subjectDissolved organic nitrogen (DON)
dc.subjectPrecipitation
dc.subjectThroughfall
dc.subjectStemflow
dc.subjectSchima superba
dc.subjectCunninghamia lanceolata
dc.subjectPlantation
dc.title木荷和杉木人工林天然降水、穿透雨和树干茎流DOC和DON 浓度及动态(英文)
dc.title.alternativeDissolved organic carbon and nitrogen in precipitation, throughfall and stemflow from Schima superba and Cunninghamia lanceolata plantations in subtropical China
dc.typeArticle


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