Nutr ient Character istics of Stem-Flow in D ifferentTree Spec ies in M iddle Subtropics

CHEN Shu-jun; YAN Wen-de; XIANG Wen-hua; LEI Pi-feng

Volume 20 Issue 3

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Nutr ient Character istics of Stem-Flow in D ifferentTree Spec ies in M iddle Subtropics

1.
College of Forestry, Northwest Agriculture and Forestry University, Yangling　712100, Shaanxi, China
2.
Research Section of Ecology, Central South University of Forestry and Technology, Changsha　410004, Hu’nan, China

Received Date: 2006-04-28

Abstract

The concentrations of 9 nutrient elements (N、P、K、Ca、Mg、Cu、Zn、Mn、SiO2 ) in stem-flow, and rainfallwere measured in 22～25 years old Cinnam om um cam phora, Pinus taeda, Quercus a liena,M ichelia m acclurei from Ap ril of 2003 to July of 2004 at Zhuzhou. The results showed: the concentrations of the nutrients in rainfall varied according to the month; The concentration sequence of the nutrient elements in p recip itation were follows: Ca >NH4-N > SiO2 > Zn > K >NO3-N >Mg > Fe >Mn > P > Cu; The concentrations of the nutrients in stem-flow also variedin the same way and changed seasonally. Compared with that in p recip itation, most of them increased; The nutrientcharacteristics of stem-flow for different tree species differed significantly and the concentration sequence of the totalnutrient elements in stem-flow were follows: Pinus taeda, Quercus aliena、Cinnam om um cam phora, M ichelia m acclurei; Proportion of nutrient in stem-flow of different nutrient elements also differed significantly among all nutrientsanalysed. It was found that the highest concentration was for NH4-N, Ca, K, SiO2 , middle forMg,NO3-N, Zn,Mn,and the lowest for P, Fe, Cu; Compared with atmospheric p recip itation, the stem2flow of four tree species togetherperformance were, the concentration of Cu nearly did not change, other element content had a bigger change, Cinnam om um cam phora stem-flow Zn, SiO2 , Fe, Cu; Pinus taeda, Quercus aliena stem-flow Zn, Fe; M ichelia m acclureistem-flow Zn were lower than those in p recip itation, significant variation was especially noted for Zn in the four treespecies
- precip itation,
- stem-flow,
- nutrient concentration,
- sub-tropic zone

References

[1]	Lindberg S E, Lovett GM, RichterD D, et al. Atmospheric deposition and canopy interactions of major ions in a forest [J]. Science,1986, 231: 141～145
[2]	李凌浩. 武夷山甜槠林生态系统的养分平衡研究[J]. 植物生态学报, 1998, 22 (3) : 193～201
[3]	Park G G. Through2fall and Stem-flow in the forest nutrient cycle[J]. Adv Ecol Res, 1983, 13: 57～134
[4]	MartinezMeza E,Whitford W G. Stem-flow , through-fall and channelization of Stem-flow by roots in three Chihuanhuan desert shrubs[J]. J Arid Environ, 1996, 32: 271～281
[5]	马雪华. 在杉木林和马尾松林中雨水的养分淋溶作用[J]. 生态学报, 1989, 9 (1) : 15～20
[6]	马雪华. 森林生态系统定位研究方法[M]. 北京:中国林业出版社, 1994: 187～190
[7]	中国科学院南京土壤研究所. 土壤理化分析[M]. 上海:上海科学与技术出版社, 1978: 388～411
[8]	于小军,汪思龙,邓仕坚,等. 亚热带常绿阔叶林和杉木人工林茎流和穿透雨的养分特征[J]. 生态学杂志, 2003, 22 (6) : 7～11
[9]	程伯容,许广山,耿晓源,等. 长白山红松云冷杉林生态系统中穿透雨的养分输入[J]. 应用生态学报, 1993, 4 (4) : 447～449
[10]	Holland E A, Dentener F J, BraswellB H, et al. Contemporary andPer-industrial global reactive nitrogen budgets [J]. Biogeochemistry, 1999, 46: 7～43
[11]	张颖,刘学军,张福锁,等. 华北平原大气氮素沉降的时空变异[J]. 生态学报, 2006, 26 (6) : 1633～1639
[12]	Schroth GM, Elias K, Uguen R, et al. Nutrient fluxes in rain-fall,Through-fall and stem-flow in tree-based land use systems and spontaneoustree vegetation of central Amazonia[J]. Agriculture, Ecosystems and Environment, 2001, 87: 37～49
[13]	BarnesB V, Zak D R, Denton S R, et al. Forest Ecology(4th editon)[M]. NewYork: JohnWiley&Sons, Inc, 1998: 488～489
[14]	刘世海,余新晓. 北京密云水库库区水源涵养林冠层水文特征研究[J]. 林业科学, 2005, 41 (1) : 194～197
[15]	田大伦,项文化,杨晚华. 第二代杉木幼林生态系统水化学特征[J]. 生态学报, 2002, 22 (6) : 859～865
[16]	雷瑞德,吕喻良. 锐齿栎林生态系统对水质的影响及评价[J].西北林学院学报, 2003, 18 (4) : 1～4
[17]	Jesus R A, J imenezM S, DomingoM, et al. Net below canopy fluxes in Canarian laurel forest canop ies [J]. Journal of Hydrology,2002, 264: 201～212
[18]	Hou B F, Wei H. Estimation of dry deposition and canopy exchange inChinese fir plantation[J]. Forest EcolManag, 2001, 147: 99～107
[19]	Draaijers G P J, Erisman JW, Van Leeuwen N FM, et al. The impact of canopy exchange on differences observed between atmospheric deposition and throughfall fluxes[J]. Atmos Environ, 1997,31 (3) : 387～397
[20]	樊后保. 杉木林截留对降水化学的影响[J]. 林业科学, 2000, 36(4) : 2～8
[21]	刘世海,余新晓,于志民. 密云水库集水区人工油松水源保护林水化学元素性质研究[J]. 应用生态学报, 2001, 12 (5) : 697～700
[22]	陶豫萍,吴宁,罗鹏,等. 森林对污染物湿沉降过滤作用的研究[J]. 水资源保护, 2006, 22 (3) : 16～23
[23]	刘世荣,王兵,周光益,等. 中国森林生态系统水文生态功能规律[M]. 北京:中国林业出版社, 1996: 236～245

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沈阳化工大学材料科学与工程学院沈阳 110142

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Nutr ient Character istics of Stem-Flow in D ifferentTree Spec ies in M iddle Subtropics

1. College of Forestry, Northwest Agriculture and Forestry University, Yangling　712100, Shaanxi, China

2. Research Section of Ecology, Central South University of Forestry and Technology, Changsha　410004, Hu’nan, China

Received Date: 2006-04-28

Abstract: The concentrations of 9 nutrient elements (N、P、K、Ca、Mg、Cu、Zn、Mn、SiO2 ) in stem-flow, and rainfallwere measured in 22～25 years old Cinnam om um cam phora, Pinus taeda, Quercus a liena,M ichelia m acclurei from Ap ril of 2003 to July of 2004 at Zhuzhou. The results showed: the concentrations of the nutrients in rainfall varied according to the month; The concentration sequence of the nutrient elements in p recip itation were follows: Ca >NH4-N > SiO2 > Zn > K >NO3-N >Mg > Fe >Mn > P > Cu; The concentrations of the nutrients in stem-flow also variedin the same way and changed seasonally. Compared with that in p recip itation, most of them increased; The nutrientcharacteristics of stem-flow for different tree species differed significantly and the concentration sequence of the totalnutrient elements in stem-flow were follows: Pinus taeda, Quercus aliena、Cinnam om um cam phora, M ichelia m acclurei; Proportion of nutrient in stem-flow of different nutrient elements also differed significantly among all nutrientsanalysed. It was found that the highest concentration was for NH4-N, Ca, K, SiO2 , middle forMg,NO3-N, Zn,Mn,and the lowest for P, Fe, Cu; Compared with atmospheric p recip itation, the stem2flow of four tree species togetherperformance were, the concentration of Cu nearly did not change, other element content had a bigger change, Cinnam om um cam phora stem-flow Zn, SiO2 , Fe, Cu; Pinus taeda, Quercus aliena stem-flow Zn, Fe; M ichelia m acclureistem-flow Zn were lower than those in p recip itation, significant variation was especially noted for Zn in the four treespecies

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Reference (23)

[1]	Lindberg S E, Lovett GM, RichterD D, et al. Atmospheric deposition and canopy interactions of major ions in a forest [J]. Science,1986, 231: 141～145
[2]	李凌浩. 武夷山甜槠林生态系统的养分平衡研究[J]. 植物生态学报, 1998, 22 (3) : 193～201
[3]	Park G G. Through2fall and Stem-flow in the forest nutrient cycle[J]. Adv Ecol Res, 1983, 13: 57～134
[4]	MartinezMeza E,Whitford W G. Stem-flow , through-fall and channelization of Stem-flow by roots in three Chihuanhuan desert shrubs[J]. J Arid Environ, 1996, 32: 271～281
[5]	马雪华. 在杉木林和马尾松林中雨水的养分淋溶作用[J]. 生态学报, 1989, 9 (1) : 15～20
[6]	马雪华. 森林生态系统定位研究方法[M]. 北京:中国林业出版社, 1994: 187～190
[7]	中国科学院南京土壤研究所. 土壤理化分析[M]. 上海:上海科学与技术出版社, 1978: 388～411
[8]	于小军,汪思龙,邓仕坚,等. 亚热带常绿阔叶林和杉木人工林茎流和穿透雨的养分特征[J]. 生态学杂志, 2003, 22 (6) : 7～11
[9]	程伯容,许广山,耿晓源,等. 长白山红松云冷杉林生态系统中穿透雨的养分输入[J]. 应用生态学报, 1993, 4 (4) : 447～449
[10]	Holland E A, Dentener F J, BraswellB H, et al. Contemporary andPer-industrial global reactive nitrogen budgets [J]. Biogeochemistry, 1999, 46: 7～43
[11]	张颖,刘学军,张福锁,等. 华北平原大气氮素沉降的时空变异[J]. 生态学报, 2006, 26 (6) : 1633～1639
[12]	Schroth GM, Elias K, Uguen R, et al. Nutrient fluxes in rain-fall,Through-fall and stem-flow in tree-based land use systems and spontaneoustree vegetation of central Amazonia[J]. Agriculture, Ecosystems and Environment, 2001, 87: 37～49
[13]	BarnesB V, Zak D R, Denton S R, et al. Forest Ecology(4th editon)[M]. NewYork: JohnWiley&Sons, Inc, 1998: 488～489
[14]	刘世海,余新晓. 北京密云水库库区水源涵养林冠层水文特征研究[J]. 林业科学, 2005, 41 (1) : 194～197
[15]	田大伦,项文化,杨晚华. 第二代杉木幼林生态系统水化学特征[J]. 生态学报, 2002, 22 (6) : 859～865
[16]	雷瑞德,吕喻良. 锐齿栎林生态系统对水质的影响及评价[J].西北林学院学报, 2003, 18 (4) : 1～4
[17]	Jesus R A, J imenezM S, DomingoM, et al. Net below canopy fluxes in Canarian laurel forest canop ies [J]. Journal of Hydrology,2002, 264: 201～212
[18]	Hou B F, Wei H. Estimation of dry deposition and canopy exchange inChinese fir plantation[J]. Forest EcolManag, 2001, 147: 99～107
[19]	Draaijers G P J, Erisman JW, Van Leeuwen N FM, et al. The impact of canopy exchange on differences observed between atmospheric deposition and throughfall fluxes[J]. Atmos Environ, 1997,31 (3) : 387～397
[20]	樊后保. 杉木林截留对降水化学的影响[J]. 林业科学, 2000, 36(4) : 2～8
[21]	刘世海,余新晓,于志民. 密云水库集水区人工油松水源保护林水化学元素性质研究[J]. 应用生态学报, 2001, 12 (5) : 697～700
[22]	陶豫萍,吴宁,罗鹏,等. 森林对污染物湿沉降过滤作用的研究[J]. 水资源保护, 2006, 22 (3) : 16～23
[23]	刘世荣,王兵,周光益,等. 中国森林生态系统水文生态功能规律[M]. 北京:中国林业出版社, 1996: 236～245

Nutr ient Character istics of Stem-Flow in D ifferentTree Spec ies in M iddle Subtropics

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通讯作者: 陈斌, bchen63@163.com

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Nutr ient Character istics of Stem-Flow in D ifferentTree Spec ies in M iddle Subtropics

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