So il Respira tion of the Representa tive Artif ic ia l Forests Dur ing theM inor Growing Sea son in the Hilly Reg ion of North-China

WANG He-song; ZHANG Jin-song; MENG Ping; GAO Jun; JIA Chang-rong

Volume 20 Issue 6

Article Contents

Turn off MathJax

Article Navigation > Forest Research > 2007 > 20(6): 820-825

Citation:

So il Respira tion of the Representa tive Artif ic ia l Forests Dur ing theM inor Growing Sea son in the Hilly Reg ion of North-China

1.
Research Institute of Forestry, CAF
2.
Key Laboratory of Tree Breeding and Cultivation, State Forestry Administration, Beijing　100091, China

Received Date: 2006-09-04

Abstract

Soil resp iration of two rep resentative artificial forests during the minor growing season in the hilly region ofNorth2China, in case of 30 years old Platycladus orienta lis and 25 years old Ouercus variabili, were analyzed. Soilresp iration rate wasmeasured by L i-8100 automatic monitoring system, and the soil temperature and soilwater content wasmeasured by AR-A-ECH automatic monitoring system from Nov. of 2005 toMar. of 2006 . The main results are as follows: ( 1 ) For both the two artificial forests, soil resp iration rate ( SRR ) in clear-cloudy day wasmarkedly higher than that in overcast day, but the diurnal variation of SRR was not apparent under the two weatherconditions. Daily SRR changed significantly, and characterized with that SRR decreased sharp ly from November toJanuary of the next year, and maintained at a relatively low value in February, and then increased rap idly after themiddle ofMarch. Snowingmade SRR rise varying extents during this season. The average SRR of Platycladus orienta lis and Ouercus variabiliwere 0. 61μmol?m-2 ?s-1 and 0. 39μmol?m-2 ?s-1 respectively in the whole minor growing season. (2) Significant relationship were found between the two artificial forests SRR and soil temperaturesat the 0, 5, 10, 15 and 20 cm dep th from the soil surface ( p -2 ?s-1 and 1. 60-μmol?m-2 ?s-1 respectively. SRR was also correlatedwith the soilwater content ( p < 0. 01) , the regression equation for Platycladus orienta liswas linear, butmultinomialfor Ouercus variabili. SRR was significantly related to soil temperature ( Ts) and soil water content ( SW ) at 5 cmdep th. Ts was the most important factor that effected on SRR for both the two artificial forests through comparing thepartial coefficient of Ts and SW at the 5 cm dep th.
- hilly region ofNorth-China,
- Pla tycladus orientalis,
- Ouercus variabili,
- soil resp iration,
- minor growing season

References

[1]	Raich J W, Potter C S. Global patterns of carbon dioxide emissionsfrom soils[J]. Global Biogeochem Cycles, 1995, 9: 23～36
[2]	SchlesingerW H, Andrews J A. Soil resp iration and the global carbon cycle [J]. Biogeochemistry, 2000, 48: 7～20
[3]	PostW M, EmanuelW R, Zinke P J, et al. Soil pool and world lifezones [J]. Nature, 1982, 298: 156～159
[4]	Russell KM. Winter forest soil resp iration controlled by climate andmicrobial community composition [J]. Nature, 2006, 439: 711～714
[5]	Monson R K, Sparks J P, Rosenstiel T N, et al. Climatic influenceson net ecosystem CO2 exchange during the transition from wintertimecarbon source to sp ringtime carbon sink in a high-elevation, subalp ine forest [J]. Oecologia, 2005, 146: 130～147
[6]	Hubbard R M, Ryan M G, Elder, et al. Seasonal patterns in soilsurface CO2 flux under snow cover in 50 and 300 year old subalp ineforests[J] . Biogeochemistry, 2005, 73: 93～107
[7]	蒋延玲,周广胜,赵敏,等. 长白山阔叶红松林生态系统土壤呼吸作用研究[J]. 植物生态学报, 2005, 29 (3) : 411～414
[8]	易志刚,蚁伟民,周国逸,等. 鼎湖山三种主要植被类型土壤碳释放研究[J]. 生态学报, 2003, 23 (8) : 1673～1678
[9]	周存宇,周国逸,王迎红,等. 鼎湖山针阔叶混交林土壤呼吸的研究[J]. 北京林业大学学报, 2005, 27 (4) : 23～27
[10]	陈光水,杨玉盛,王小国,等. 格氏栲天然林与人工林根系呼吸季节动态及影响因素[J]. 生态学报, 2005, 25 ( 8 ) : 1941～1947
[11]	骆土寿, 陈步峰,李意德,等. 海南岛尖峰岭热带山地雨林土壤和凋落物呼吸研究[J]. 生态学报, 2001, 21 (12) : 2013～2017
[12]	李意德,吴仲民,曾庆波,等. 尖峰岭热带山地雨林生态系统碳平衡的初步研究[J]. 生态学报, 1998, 18 (4) : 371～378
[13]	肖复明,汪思龙,杜天真,等. 杉木人工林林地土壤呼吸研究[J]. 江西农业大学学报, 2005, 27 (4) : 580～584
[14]	房秋兰, 沙丽清. 西双版纳热带季节雨林与橡胶林土壤呼吸[J]. 植物生态学报, 2006, 30 (1) : 97～103
[15]	刘建军,王得祥,雷瑞德,等. 火地塘林区锐齿栎林土壤碳循环的动态模拟[J]. 西北农林科技大学学报(自然科学版) , 2003,31 (6) : 14～18
[16]	刘建军,王得祥,雷瑞德,等. 秦岭天然油松锐齿栎林地土壤呼吸与CO2释放[J]. 林业科学, 2003, 39 (2) : 8～13
[17]	马钦彦,张学培,韩海荣,等. 山西太岳山森林土壤夏日CO2释放速率的研究[J]. 北京林业大学学报, 2000, 22 (4) : 89～91
[18]	刘绍辉,方精云,清田信. 北京山地温带森林的土壤呼吸[J]. 植物生态学报, 1998, 22 (2) : 119～126
[19]	Eric B, Elizabeth B, Richard B. Soil water content and temperature as independent or confounded factors controlling soil resp irationin a temperature mixed hardwood forest[J]. Global Change Biology, 1998, 4: 217～227
[20]	Luitgard S, Edzo V, Tania B, et al. Spatial and temporal variationin soil CO2 efflux in an old-growth neotrop ical rain forest, La Selva,Costa Rica[J]. Biogeochemistry, 2003, 64: 111～128
[21]	蒋高明, 黄银晓. 北京山区辽东栎林土壤释放CO2的模拟实验研究[J]. 生态学报, 1997, 17 (5) : 477～482
[22]	崔骁勇,陈佐忠,陈四清. 草地土壤呼吸研究进展[J]. 生态学报, 2001, 21 (2) : 315～325
[23]	易志刚,蚁伟民. 森林生态系统中土壤呼吸研究进展[J]. 生态环境, 2003, 12 (3) : 361～365

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article views(3593) PDF downloads(1613) Cited by()

Proportional views

So il Respira tion of the Representa tive Artif ic ia l Forests Dur ing theM inor Growing Sea son in the Hilly Reg ion of North-China

1. Research Institute of Forestry, CAF

2. Key Laboratory of Tree Breeding and Cultivation, State Forestry Administration, Beijing　100091, China

Received Date: 2006-09-04

Abstract: Soil resp iration of two rep resentative artificial forests during the minor growing season in the hilly region ofNorth2China, in case of 30 years old Platycladus orienta lis and 25 years old Ouercus variabili, were analyzed. Soilresp iration rate wasmeasured by L i-8100 automatic monitoring system, and the soil temperature and soilwater content wasmeasured by AR-A-ECH automatic monitoring system from Nov. of 2005 toMar. of 2006 . The main results are as follows: ( 1 ) For both the two artificial forests, soil resp iration rate ( SRR ) in clear-cloudy day wasmarkedly higher than that in overcast day, but the diurnal variation of SRR was not apparent under the two weatherconditions. Daily SRR changed significantly, and characterized with that SRR decreased sharp ly from November toJanuary of the next year, and maintained at a relatively low value in February, and then increased rap idly after themiddle ofMarch. Snowingmade SRR rise varying extents during this season. The average SRR of Platycladus orienta lis and Ouercus variabiliwere 0. 61μmol?m-2 ?s-1 and 0. 39μmol?m-2 ?s-1 respectively in the whole minor growing season. (2) Significant relationship were found between the two artificial forests SRR and soil temperaturesat the 0, 5, 10, 15 and 20 cm dep th from the soil surface ( p -2 ?s-1 and 1. 60-μmol?m-2 ?s-1 respectively. SRR was also correlatedwith the soilwater content ( p < 0. 01) , the regression equation for Platycladus orienta liswas linear, butmultinomialfor Ouercus variabili. SRR was significantly related to soil temperature ( Ts) and soil water content ( SW ) at 5 cmdep th. Ts was the most important factor that effected on SRR for both the two artificial forests through comparing thepartial coefficient of Ts and SW at the 5 cm dep th.

HTML

Reference (23)

[1]	Raich J W, Potter C S. Global patterns of carbon dioxide emissionsfrom soils[J]. Global Biogeochem Cycles, 1995, 9: 23～36
[2]	SchlesingerW H, Andrews J A. Soil resp iration and the global carbon cycle [J]. Biogeochemistry, 2000, 48: 7～20
[3]	PostW M, EmanuelW R, Zinke P J, et al. Soil pool and world lifezones [J]. Nature, 1982, 298: 156～159
[4]	Russell KM. Winter forest soil resp iration controlled by climate andmicrobial community composition [J]. Nature, 2006, 439: 711～714
[5]	Monson R K, Sparks J P, Rosenstiel T N, et al. Climatic influenceson net ecosystem CO2 exchange during the transition from wintertimecarbon source to sp ringtime carbon sink in a high-elevation, subalp ine forest [J]. Oecologia, 2005, 146: 130～147
[6]	Hubbard R M, Ryan M G, Elder, et al. Seasonal patterns in soilsurface CO2 flux under snow cover in 50 and 300 year old subalp ineforests[J] . Biogeochemistry, 2005, 73: 93～107
[7]	蒋延玲,周广胜,赵敏,等. 长白山阔叶红松林生态系统土壤呼吸作用研究[J]. 植物生态学报, 2005, 29 (3) : 411～414
[8]	易志刚,蚁伟民,周国逸,等. 鼎湖山三种主要植被类型土壤碳释放研究[J]. 生态学报, 2003, 23 (8) : 1673～1678
[9]	周存宇,周国逸,王迎红,等. 鼎湖山针阔叶混交林土壤呼吸的研究[J]. 北京林业大学学报, 2005, 27 (4) : 23～27
[10]	陈光水,杨玉盛,王小国,等. 格氏栲天然林与人工林根系呼吸季节动态及影响因素[J]. 生态学报, 2005, 25 ( 8 ) : 1941～1947
[11]	骆土寿, 陈步峰,李意德,等. 海南岛尖峰岭热带山地雨林土壤和凋落物呼吸研究[J]. 生态学报, 2001, 21 (12) : 2013～2017
[12]	李意德,吴仲民,曾庆波,等. 尖峰岭热带山地雨林生态系统碳平衡的初步研究[J]. 生态学报, 1998, 18 (4) : 371～378
[13]	肖复明,汪思龙,杜天真,等. 杉木人工林林地土壤呼吸研究[J]. 江西农业大学学报, 2005, 27 (4) : 580～584
[14]	房秋兰, 沙丽清. 西双版纳热带季节雨林与橡胶林土壤呼吸[J]. 植物生态学报, 2006, 30 (1) : 97～103
[15]	刘建军,王得祥,雷瑞德,等. 火地塘林区锐齿栎林土壤碳循环的动态模拟[J]. 西北农林科技大学学报(自然科学版) , 2003,31 (6) : 14～18
[16]	刘建军,王得祥,雷瑞德,等. 秦岭天然油松锐齿栎林地土壤呼吸与CO2释放[J]. 林业科学, 2003, 39 (2) : 8～13
[17]	马钦彦,张学培,韩海荣,等. 山西太岳山森林土壤夏日CO2释放速率的研究[J]. 北京林业大学学报, 2000, 22 (4) : 89～91
[18]	刘绍辉,方精云,清田信. 北京山地温带森林的土壤呼吸[J]. 植物生态学报, 1998, 22 (2) : 119～126
[19]	Eric B, Elizabeth B, Richard B. Soil water content and temperature as independent or confounded factors controlling soil resp irationin a temperature mixed hardwood forest[J]. Global Change Biology, 1998, 4: 217～227
[20]	Luitgard S, Edzo V, Tania B, et al. Spatial and temporal variationin soil CO2 efflux in an old-growth neotrop ical rain forest, La Selva,Costa Rica[J]. Biogeochemistry, 2003, 64: 111～128
[21]	蒋高明, 黄银晓. 北京山区辽东栎林土壤释放CO2的模拟实验研究[J]. 生态学报, 1997, 17 (5) : 477～482
[22]	崔骁勇,陈佐忠,陈四清. 草地土壤呼吸研究进展[J]. 生态学报, 2001, 21 (2) : 315～325
[23]	易志刚,蚁伟民. 森林生态系统中土壤呼吸研究进展[J]. 生态环境, 2003, 12 (3) : 361～365

So il Respira tion of the Representa tive Artif ic ia l Forests Dur ing theM inor Growing Sea son in the Hilly Reg ion of North-China

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Proportional views

So il Respira tion of the Representa tive Artif ic ia l Forests Dur ing theM inor Growing Sea son in the Hilly Reg ion of North-China

HTML

Catalog

Export File

Citation

Format

Content