Effects of different nitrogen addition forms and levels on N<sub>2</sub>O emission in the temperate forest soil

XU Ke; WANG Chun-mei; ZHANG Yi; YANG Xin-tong; HAN Jin-feng; GUI Rong-rong

doi:10.13332/j.1000-1522.20160103

Journal of Beijing Forestry University > 2017 > 39(3): 74-80. > DOI: 10.13332/j.1000-1522.20160103

XU Ke, WANG Chun-mei, ZHANG Yi, YANG Xin-tong, HAN Jin-feng, GUI Rong-rong. Effects of different nitrogen addition forms and levels on N₂O emission in the temperate forest soil[J]. Journal of Beijing Forestry University, 2017, 39(3): 74-80. DOI: 10.13332/j.1000-1522.20160103

Citation:

PDF (965 KB)

Effects of different nitrogen addition forms and levels on N₂O emission in the temperate forest soil

1.
College of Environmental Science & Engineering, Beijing Forestry University, Beijing, 100083, P. R. China
2.
Zoige National Nature Reserve, Zoige, Sichuan, 624500, P. R. China

More Information

Received Date: March 27, 2016
Revised Date: June 02, 2016
Published Date: February 28, 2017

Graphical Abstract

Abstract

Abstract

Nitrous oxide (N₂O) emission can be affected by the amounts and forms of nitrogen (N) available in soils. To improve our understanding of the response of N₂O emission to different N addition levels and forms, a manipulative field experiment was conducted to investigate the effects of different forms (ammonium sulfate, As:(NH₄)₂SO₄; sodium nitrate, Na:NaNO₃; ammonium nitrate, AN:NH₄NO₃) and levels (control: 0 kg/(ha·year); low N, LN: 50 kg/(ha·year); MN: 100 kg/(ha·year) and high N, HN: 150 kg/(ha·year)) of N addition on N₂O emission of temperate Pinus tabuliformis forest soil using the static closed chamber method at Experimental Forest Station of Beijing Forestry University in Beijing, northern China. Our results showed that soil N₂O emission showed a trend of seasonal variation: higher in summer (May to August) but relatively low in the remaining seasons. The minimum value appeared in January. Different levels of N addition increased annual N₂O emission in the order of HN>MN>LN>control. The three N forms increased annual N₂O emission in the order of AN>As>Na, but the difference was insignificant (P>0.05) between As and AN or As and Na. These results suggested that the N₂O emission from temperate forest soil sensitively responded to N addition forms and levels. In addition, soil temperature, air temperature and water-filled pore space also influenced soil N₂O fluxes. Annual soil N₂O emission factors ranged from 0.34% to 0.94% for different N addition treatments, with an overall emission factor value of 0.364%. The emission factor values were far less than the mean default emission factor proposed by the Intergovernmental Panel on Climate Change (IPCC).
- N addition level,
- N addition form,
- N₂O emission,
- temperate forest soil,
- Pinus tabuliformis

FullText(HTML)

References (37)

References

[1]	FANG Y, YOH M, KOBA K, et al. Nitrogen deposition and forest nitrogen cycling along an urban-rural transect in southern China[J]. Global Change Biology, 2011, 17(2): 872-885. doi: 10.1111/j.1365-2486.2010.02283.x
[2]	GALLOWAY J N, COWLING E B. Reactive nitrogen and the world: 200 years of change[J]. AMBIO: A Journal of the Human Environment, 2002, 31(2): 64-71. doi: 10.1579/0044-7447-31.2.64
[3]	BOBBINK R, HICKS K, GALLOWAY J, et al. Global assessment of nitrogen deposition effects on terrestrial plant diversity: a synthesis[J]. Ecological Applications, 2010, 20(1): 30-59. doi: 10.1890/08-1140.1
[4]	BUTTERBACH-BAHL K, ROTHE A, PAPEN H. Effect of tree distance on N₂O and CH₄ fluxes from soils in temperate forest ecosystems[J]. Plant and Soil, 2002, 240(1): 91-103. doi: 10.1023/A:1015828701885
[5]	SOLOMON S. IPCC (2007): climate change the physical science basis[J]. American Geophysical Union, 2007, 9(1): 123-124.
[6]	RAVISHANKARA A, DANIEL J S, PORTMANN R W. Nitrous oxide (N₂O): the dominant ozone-depleting substance emitted in the 21st century[J]. Science, 2009, 326: 123-125. doi: 10.1126/science.1176985
[7]	HANSEN J E, LACIS A A. Sun and dust versus greenhouse gases: an assessment of their relative roles in global climate change[J]. Nature, 1990, 346: 713-719. doi: 10.1038/346713a0
[8]	BRUMME R, VERCHOT L V, MARTIKAINEN P J, et al. Contribution of trace gases nitrous oxide (N₂O) and methane (CH₄) to the atmospheric warming balance of forest biomes[J]. Seb Experimental Biology, 2005, 27(7): 293-317. http://europepmc.org/abstract/MED/17633041
[9]	方华军, 程淑兰, 于贵瑞, 等.大气氮沉降对森林土壤甲烷吸收和氧化亚氮排放的影响及其微生物学机制[J].生态学报, 2014, 34(17): 4799-4806. http://d.old.wanfangdata.com.cn/Periodical/stxb201417001 FANG H J, CHENG S L, YU G R, et al. Microbial mechanisms responsible for the effects of atmospheric nitrogen deposition on methane uptake and nitrous oxide emission in forest soils: a review[J]. Acta Ecologica Sinica, 2014, 34(17): 4799-4806. http://d.old.wanfangdata.com.cn/Periodical/stxb201417001
[10]	莫江明, 方运霆, 林而达, 等.鼎湖山主要森林土壤N₂O排放及其对模拟N沉降的响应[J].植物生态学报, 2006, 30(6): 901-910. doi: 10.3321/j.issn:1005-264X.2006.06.003 MO J M, FANG Y T, LIN E D, et al. Soil N₂O emission and its response to simulated N deposition in the main forests of Ding Hushan in subtropical china[J]. Chinese Journal of Plant Ecology, 2006, 30(6): 901-910. doi: 10.3321/j.issn:1005-264X.2006.06.003
[11]	ADAMS M, INESON P, DAN B, et al. Soil functional responses to excess nitrogen inputs at global scale[J]. Ambio A Journal of the Human Environment, 2004, 33(8): 530-536. doi: 10.1579/0044-7447-33.8.530
[12]	CHEN G C, TAM N F Y, YE Y. Spatial and seasonal variations of atmospheric N₂O and CO₂ fluxes from a subtropical mangrove swamp and their relationships with soil characteristics[J]. Soil Biology & Biochemistry, 2012, 48(4): 175-181. https://www.sciencedirect.com/science/article/abs/pii/S0038071712000508
[13]	ZHU J, MULDER J, SOLHEIMSLID S O, et al. Functional traits of denitrification in a subtropical forest catchment in China with high atmogenic N deposition[J]. Soil Biology & Biochemistry, 2013, 57(3): 577-586. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=52b212985a958c0e6b39fc77f5ccbee8
[14]	PENG Q, QI Y, DONG Y, et al. Soil nitrous oxide emissions from a typical semiarid temperate steppe in Inner Mongolia: effects of mineral nitrogen fertilizer levels and forms[J]. Plant and Soil, 2011, 342(1-2): 345-357. doi: 10.1007/s11104-010-0699-1
[15]	WANG L, CAI Z. Nitrous oxide production at different soil moisture contents in an arable soil in China[J]. Soil Science & Plant Nutrition, 2008, 54(5): 786-793. doi: 10.1111/j.1747-0765.2008.00297.x
[16]	WANG F, LI J, WANG X, et al. Nitrogen and phosphorus addition impact soil N₂O emission in a secondary tropical forest of South China[J]. Sci Rep, 2014, 4: 5615-5615. https://www.nature.com/articles/srep05615
[17]	BAI E, LI W, LI S L, et al. Pulse increase of soil N₂O emission in response to N addition in a temperate forest on Mt Changbai, Northeast China[J]. Plos One, 2014, 9(7): e102765-e102765. doi: 10.1371/journal.pone.0102765
[18]	LIU X, DONG Y, QI Y, et al. Response of N₂O emission to water and nitrogen addition in temperate typical steppe soil in Inner Mongolia, China[J]. Soil and Tillage Research, 2015, 151(1): 9-17. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=27d040258af08910c79d76190dfa17ae
[19]	HATCH D, JARVIS S, PHILIPPS L. Field measurement of nitrogen mineralization using soil core incubation and acetylene inhibition of nitrification[J]. Plant and Soil, 1990, 124(1): 97-107. doi: 10.1007/BF00010937
[20]	DONG Y, ZHANG S, QI Y, et al. Fluxes of CO₂, N₂O and CH₄ from a typical temperate grassland in Inner Mongolia and its daily variation[J]. Chinese Science Bulletin, 2000, 45(17): 1590-1594. doi: 10.1007/BF02886219
[21]	MATSON A, PENNOCK D, BEDARD-HAUGHN A. Methane and nitrous oxide emissions from mature forest stands in the boreal forest, Saskatchewan, Canada[J]. Forest Ecology and Management, 2009, 258(7): 1073-1083. doi: 10.1016/j.foreco.2009.05.034
[22]	YUPING Y, LIQING S, MIN C, et al. Fluxes of CH₄ and N₂O from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China[J]. Journal of Environmental Sciences, 2008, 20(2): 207-215. doi: 10.1016/S1001-0742(08)60033-9
[23]	VAN GROENIGEN J W, VELTHOF G L, VAN DER BOLT F J, et al. Seasonal variation in N₂O emissions from urine patches: effects of urine concentration, soil compaction and dung[J]. Plant and Soil, 2005, 273(1-2): 15-27. doi: 10.1007/s11104-004-6261-2
[24]	DONOSO L, SANTANA R, SANHUEZA E. Seasonal variation of N₂O fluxes at a tropical savannah site: soil consumption of N₂O during the dry season[J]. Geophysical Research Letters, 1993, 20(13): 1379-1382. doi: 10.1029/93GL01537
[25]	欧阳扬, 李叙勇.干湿交替频率对不同土壤CO₂和N₂O释放的影响[J].生态学报, 2013, 33(4): 1251-1259. http://d.old.wanfangdata.com.cn/Periodical/stxb201304025 OUYANG Y, LI X Y. Impacts of drying-wetting cycles on CO₂ and N₂O emissions from soils in different ecosystems[J]. Acta Ecologica Sinica, 2013, 33(4): 1251-1259. http://d.old.wanfangdata.com.cn/Periodical/stxb201304025
[26]	LIN S, IQBAL J, HU R, et al. Nitrous oxide emissions from rape field as affected by nitrogen fertilizer management: a case study in Central China[J]. Atmospheric Environment, 2011, 45(9): 1775-1779. doi: 10.1016/j.atmosenv.2011.01.003
[27]	陈哲, 陈媛媛, 高霁, 等.不同施肥措施对黄河上游灌区油葵田土壤N₂O排放的影响[J].应用生态学报, 2015, 26(1): 129-139. http://d.old.wanfangdata.com.cn/Periodical/yystxb201501018 CHEN Z, CHEN Y Y, GAO J, et al. Effects of different fertilization measures on N₂O emission in oil sunflower field in irrigation area of upper Yellow River[J]. The Journal of Applied Ecology, 2015, 26(1): 129-139. http://d.old.wanfangdata.com.cn/Periodical/yystxb201501018
[28]	王海云, 邢光熹.不同施氮水平对稻麦轮作农田氧化亚氮排放的影响[J].农业环境科学学报, 2009, 28(12): 2631-2636. doi: 10.3321/j.issn:1672-2043.2009.12.030 WANG H Y, XING G X. Effect of nitrogen fertilizer rates on nitrous oxide emission from paddy field under rice-wheat rotation[J]. Journal of Agro-Environment Science, 2009, 28(12): 2631-2636. doi: 10.3321/j.issn:1672-2043.2009.12.030
[29]	蔺照兰, 王春梅, 王汝南.冻融期温带森林土壤N₂O排放对模拟大气氮沉降的响应[J].生态环境学报, 2012, 21(11): 1804-1809. doi: 10.3969/j.issn.1674-5906.2012.11.006 LIN Z L, WANG C M, WANG R N. Effects of simulated N deposition on N₂O emssion from temperate forest soil subject to freezing-thawing process[J]. Ecology and Environmental Sciences, 2012, 21(11): 1804-1809. doi: 10.3969/j.issn.1674-5906.2012.11.006
[30]	ZHU J, MULDER J, WU L P, et al. Spatial and temporal variability of N₂O emissions in a subtropical forest catchment in China[J]. Biogeosciences, 2013, 10(3): 1309-1321. doi: 10.5194/bg-10-1309-2013
[31]	HEFTING M M, BOBBINK R, DE CALUWE H. Nitrous oxide emission and denitrification in chronically nitrate-loaded riparian buffer zones[J]. Journal of Environmental Quality, 2003, 32(4): 1194-1203. doi: 10.2134/jeq2003.1194
[32]	DAVIDSON E A. Sources of nitric oxide and nitrous oxide following wetting of dry soil[J]. Soil Science Society of America Journal, 1992, 56(1): 95-102. doi: 10.2136/sssaj1992.03615995005600010015x
[33]	LIU D Y, SONG C C. Effects of inorganic nitrogen and phosphorus enrichment on the emission of N₂O from a freshwater marsh soil in Northeast China[J]. Environmental Earth Sciences, 2010, 60(4): 799-807. doi: 10.1007/s12665-009-0217-z
[34]	STAPLETON L M, CROUT N M J, SÄWSTRÖM C, et al. Microbial carbon dynamics in nitrogen amended Arctic tundra soil: measurement and model testing[J]. Soil Biology and Biochemistry, 2005, 37(11): 2088-2098. doi: 10.1016/j.soilbio.2005.03.016
[35]	LIU D Y, SONG C C. Effects of phosphorus enrichment on mineralization of organic carbon and contents of dissolved carbon in a freshwater marsh soil[J]. China Environmental Science, 2008, 28(9): 769-774. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghjkx200809001
[36]	LUBETSKY J, STEINER B A, LANZA R. 2006 IPCC guidelines for national greenhouse gas inventories[M]. Arlington: Institute for Global Environmental Strategies, 2006.
[37]	HE F F, JIANG R F, CHEN Q, et al. Nitrous oxide emissions from an intensively managed greenhouse vegetable cropping system in Northern China[J]. Environmental Pollution, 2009, 157(5): 1666-1672. doi: 10.1016/j.envpol.2008.12.017

[1]	Sun Fan, Ma Yanguang, Liu Zhanmin, Yang Boning, Wang Huili, Li Wei. Parental selection strategies of high generation seed orchard of Pinus tabuliformis[J]. Journal of Beijing Forestry University, 2024, 46(4): 28-39. DOI: 10.12171/j.1000-1522.20230138
[2]	Zhou Hangyu, Fu Qiyao, Liang Wanting, Song Zhaopeng, Hou Jihua. Changing patterns of nitrogen and phosphorus contents in leaf-branch-root of natural Pinus tabuliformis with precipitation and temperature[J]. Journal of Beijing Forestry University, 2024, 46(1): 44-54. DOI: 10.12171/j.1000-1522.20210275
[3]	Liu Fengchen, Tian Na, Cheng Xiaoqin. Releasing variation and bacteriostatic effects of botanic volatile organic compounds from Pinus tabuliformis[J]. Journal of Beijing Forestry University, 2022, 44(9): 72-82. DOI: 10.12171/j.1000-1522.20210125
[4]	Shang Shuaishuai, Song Minghua, Wang Chunmei, Qiu Jingcong, Wang Xinqing, Wang Shiqi, Cui Jiayi. Effects of long-term polymorphic nitrogen addition on soil N₂O emission in temperate artificial Quercus liaotungensis forests[J]. Journal of Beijing Forestry University, 2022, 44(6): 63-73. DOI: 10.12171/j.1000-1522.20220136
[5]	Chen Minsi, Du Jianhua, Wang Wei, Yu Haichen, Wang Bo, Gu Ze, Liu Xiaodong. Characteristics and potential fire behavior of combustibles in the canopy of Pinus tabuliformis forest in Badaling Forest Farm of Beijing[J]. Journal of Beijing Forestry University, 2022, 44(3): 55-64. DOI: 10.12171/j.1000-1522.20210084
[6]	Li Xiarong, Chen Yixin, Chen Jingfei, Zhu Jiyou, Sun Guangpeng, Wei Liuduan, Zhang Xinna, Xu Chengyang. Comparative study on the effects of climate change on radial growth of Pinus tabuliformis in near and outer suburbs of Beijing[J]. Journal of Beijing Forestry University, 2022, 44(1): 19-28. DOI: 10.12171/j.1000-1522.20200329
[7]	Wang Yansong, Ma Baoming, Gao Haiping, Wang Baitian, Li Sha, Dong Xiuqun. Response of soil nutrients and their stoichiometric ratios to stand density in Pinus tabuliformis and Robinia pseudoacacia plantations in the loess region of western Shanxi Province, northern China[J]. Journal of Beijing Forestry University, 2020, 42(8): 81-93. DOI: 10.12171/j.1000-1522.20190287
[8]	ZHANG Min, ZHANG Wei, GONG Zai-xin, ZHENG Cai-xia. Morphologic and anatomical observations in the process of ovulate strobilus generation and development in Pinus tabuliformis[J]. Journal of Beijing Forestry University, 2017, 39(6): 1-12. DOI: 10.13332/j.1000-1522.20160411
[9]	SONG Jie, ZHU Min, LIU Xiao-dong, REN Yun-mao, WANG Qi-feng, JIN Ying-shan. Effects of thinning on fuel characteristics and potential fire behaviors of Pinus tabuliformis forest in Beijing West Mountain[J]. Journal of Beijing Forestry University, 2017, 39(5): 41-47. DOI: 10.13332/j.1000-1522.20160353
[10]	ZHANG Xin-bo, LI Yue, YUAN Hu-wei, LI Wei, FU Yu-hua, LIU Zhi-yuan, ZHU Song-lin. Genetic variations of growth traits in a 21-year-old stand progeny of Shanxi natural Pinus tabuliformis forests.[J]. Journal of Beijing Forestry University, 2014, 36(3): 104-109. DOI: 10.13332/j.cnki.jbfu.2014.03.016

Cited By

Cited by

Periodical cited type(4)

1.	沈子雅，程金花，赵溦，管凝，曾合州，秦建淼，赵梦圆. 降雨条件下灌草配置方式对褐土坡面径流泥沙特征的影响. 水土保持学报. 2022(05): 17-23 .
2.	宋鑫，徐杉，熊芹. 狗牙根抗逆研究进展. 草学. 2021(06): 9-14 .
3.	秦东远，肖培青，郝仕龙，杨春霞. 黄丘区野外坡面产流产沙过程对不同植被覆盖结构的响应. 水土保持学报. 2019(02): 73-78 .
4.	魏小燕，毕华兴，霍云梅，肖聪颖，杨晓琪. 高羊茅草地地表径流系数影响因素研究. 北京林业大学学报. 2017(05): 82-88 . 本站查看

Other cited types(5)

Get Citation

PDF

XML

Article views (2055) PDF downloads (36) Cited by(9)

Turn off MathJax

Article Contents

Abstract

References

Effects of different nitrogen addition forms and levels on N₂O emission in the temperate forest soil