豫西黄土丘陵区不同林龄栎类和侧柏人工林碳、氮储量

doi:10.13287/j.1001-9332.201801.009

应用生态学报 ›› 2018, Vol. 29 ›› Issue (1): 25-32.doi: 10.13287/j.1001-9332.201801.009

豫西黄土丘陵区不同林龄栎类和侧柏人工林碳、氮储量

王艳芳^1,2, 刘领¹, 李志超³, 石晓峰⁴, 杨小艳⁴, 上官周平^2*

¹河南科技大学农学院, 河南洛阳 471023;
²西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌 712100;
³洛阳市林业调查规划管理站, 河南洛阳 471000;
⁴偃师市林业局, 河南偃师 471900

收稿日期:2017-06-14 出版日期:2018-01-18 发布日期:2018-01-18
通讯作者: * E-mail: shangguan@ms.iswc.ac.cn
作者简介:王艳芳, 女, 1977年生, 博士研究生. 主要从事森林生态系统碳汇研究. E-mail: wyfll1977@126.com
基金资助:
本文由国家自然科学基金项目(31700367)、国家重点研发计划项目(2016YFC0501605)、国家科技基础性工作专项(2014FY210100)和河南科技大学学科提升振兴A计划项目(13660001)资助

Storage of carbon and nitrogen in Quercus and Platycladus orientalis plantations at different ages in the hilly area of western Henan Province, China.

WANG Yan-fang^1,2, LIU Ling¹, LI Zhi-chao³, SHI Xiao-feng⁴, YANG Xiao-yan⁴, SHANGGUAN Zhou-ping^2*

¹College of Agriculture, Henan University of Science and Technology, Luoyang 471023, Henan, China;
²State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest Agriculture and Forestry University, Yangling 712100, Shaanxi, China;
³Luoyang Forest Inventory and Planning Station, Luoyang 471000, Henan, China;
⁴Yanshi Forestry Bureau, Yanshi 471900, Henan, China

Received:2017-06-14 Online:2018-01-18 Published:2018-01-18
Contact: * E-mail: shangguan@ms.iswc.ac.cn
Supported by:
This work was supported by the National Natural Science Foundation of China (31700367), the National Key Research and Development Program of China (2016YFC0501605), the National Sci-Tech Basic Program of China (2014FY210100) and the HAUST Discipline Improvement and Promotion Plan A (13660001).

摘要/Abstract

摘要： 利用空间代替时间样地调查法,分析了豫西黄土丘陵区栎类和侧柏人工林生态系统碳、氮储量的分布格局,以及不同土层碳储量和氮储量随林龄的动态变化.结果表明: 随着树龄的增加,两类人工林乔木层和枯落物层碳储量均增加,土壤碳储量和氮储量主要在表层(0～20 cm)汇聚,且各土层碳储量和氮储量随着林龄增加表现为减少-增加-减少的趋势.各林龄栎类人工林土壤表层碳、氮储量分别为20.31～50.07和1.68～2.12 t·hm^-2;不同林龄侧柏人工林土壤表层碳、氮储量分别为23.99～48.76和1.59～2.34 t·hm^-2;各林龄栎类和侧柏人工林生态系统的碳储量分别为52.04～275.82和62.18～279.81 t·hm^-2;侧柏人工林碳汇能力略高于栎类人工林.土壤C/N随着造林年限的增加呈增加趋势.

Abstract: In the study, the method of space substituting time was used to investigate the distribution pattern of carbon and nitrogen storages in Quercus and Platycladus orientalis plantation ecosystems at different ages in hilly area of western Henan Province, China. We also analyzed the dynamic changes of soil carbon and nitrogen storages in different soil layers in the two plantation ecosystems. The results showed that the carbon storage in the arbor and litter layers increased with the increasing tree age. The storage of carbon and nitrogen in soil aggregated mainly in the surface layer and showed a trend of decrease-increase-decrease with the increasing tree age in all soil layers. The ranges of carbon and nitrogen storage in the surface soil were 20.31-50.07 and 1.68-2.12 t·hm^-2 in Quercus plantation, and 23.99-48.76 and 1.59-2.34 t·hm^-2 in P. orientalis plantation, respectively. Carbon storage ranges in Quercus and P. orientalis plantation ecosystems at different ages were 52.04-275.82 and 62.18-279.81 t·hm^-2, respectively. The carbon sequestration capacity in P. orientalis plantation was a little higher than that in Quercus plantation. Soil C/N increased with the increase of afforestation age.

王艳芳, 刘领, 李志超, 石晓峰, 杨小艳, 上官周平. 豫西黄土丘陵区不同林龄栎类和侧柏人工林碳、氮储量[J]. 应用生态学报, 2018, 29(1): 25-32.

WANG Yan-fang, LIU Ling, LI Zhi-chao, SHI Xiao-feng, YANG Xiao-yan, SHANGGUAN Zhou-ping. Storage of carbon and nitrogen in Quercus and Platycladus orientalis plantations at different ages in the hilly area of western Henan Province, China.[J]. Chinese Journal of Applied Ecology, 2018, 29(1): 25-32.

参考文献

[1] Laganière J, Angers DA, Paré D. Carbon accumulation in agricultural soils after afforestation: A meta-analysis. Global Change Biology, 2009, 16: 439-453
[2] Li DJ, Niu SL, Luo YQ. Global patterns of the dynamics of soil carbon and nitrogen stocks following afforestation: A meta-analysis. New Phytologist, 2012, 195: 172-181
[3] Lal R. Carbon sequestration. Philosophical Transactions of the Royal Society B: Biological Sciences, 2008, 363: 815-830
[4] Dixon RK, Solomon AM, Brown S, et al. Carbon pools and flux of global forest ecosystem. Science, 1994, 263: 185-190
[5] Post WM, Kwon KC. Soil carbon sequestration and land-use change: Processes and potential. Global Change Biology, 2000, 6: 317-327
[6] Reich PB, Hobbie SE, Lee T, et al. Nitrogen limitation constrains sustainability of ecosystem response to CO₂. Nature, 2006, 440: 922-925
[7] Liu Y, Li P, Wang G, et al. Above- and below-ground biomass distribution and morphological characteristics respond to nitrogen addition in Pinus tabuliformis. New Zealand Journal of Forestry Science, 2016, 46: doi: 10.1186/s40490-016-0083-x
[8] Luo YQ, Su B, Currie WS, et al. Progressive nitrogen limitation of ecosystem responses to rising atmospheric carbon dioxide. BioScience, 2004, 54: 731-739
[9] The State Forestry Administration of the People’s Republic of China (国家林业局). Guides for Monitoring Carbon Sequestration of Afforestation Projects. Beijing: Chinese Forestry Press, 2011 (in Chinese)
[10] Wang T (王婷). A Study on the Community Structure, Biomass and Species Diversity of Platycladus orientalis Plantation in Songshan Mountain. Master Thesis. Zhengzhou: Henan Agricultural University, 2000 (in Chinese)
[11] Jia GM, Cao J, Wang CY, et al. Microbial biomass and nutrients in soil at the different stages of secondary forest succession in Ziwuling, northwest China. Forest Ecology and Management, 2005, 217: 117-125
[12] Nelson DW, Sommers LE. Methods of soil analysis// Page AL, Miller RH, Keeney, eds. Total Carbon, Organic Carbon, and Organic Matter. Madison, WI:American Society of Agronomy, 1982: 1-129
[13] Bremner JM. Methods of soil analysis. Ⅲ. Chemical methods// Sparks DL, ed. Nitrogen-total. Madison, WI: American Society of Agronomy, 1996: 1085-1121
[14] Li H-K (李海奎), Lei Y-C (雷渊才). Estimation and Evaluation of Forest Biomass Carbon Storage in China. Beijing: Chinese Forestry Press, 2010 (in Chinese)
[15] Singh K, Pandey VC, Singh B, et al. Ecological restoration of degraded sodic lands through afforestation and cropping. Ecological Engineering, 2012, 43: 70-80
[16] Rytter RM. Stone and gravel contents of arable soils influence estimates of C and N stocks. Catena, 2012, 95: 153-159
[17] Ming A-G (明安刚), Jia H-Y (贾宏炎), Tian Z-W (田祖为), et al. Characteristics of carbon storage and its allocation in Erythrophleum fordii plantations with different ages. Chinese Journal of Applied Ecology (应用生态学报), 2014, 25(4): 940-946 (in Chinese)
[18] Mei L (梅莉), Zhang Z-W (张卓文), Gu J-C (谷加存), et al. Carbon and nitrogen storages and allocation in tree layers of Fraxinus mandshurica and Larix gmelinii plantations. Chinese Journal of Applied Ecology (应用生态学报), 2009, 20(8): 1791-1796 (in Chinese)
[19] Yang YH, Luo YQ, Finzi AC. Carbon and nitrogen dynamics during forest stand development: A global synthesis. New Phytologist, 2011, 190: 977-989
[20] Wang FM, Xu X, Zou B, et al. Biomass accumulation and carbon sequestration in four different aged Casuarina equisetifolia coastal shelterbelt plantations in south China. PLoS One, 2013, 8(10): e77449
[21] Deng L, Wang KB, Chen ML, et al. Soil organic carbon storage capacity positively related to forest succession on the Loess Plateau, China. Catena, 2013, 110: 1-7
[22] Kirschbaum MUF, Guo LB, Gifford RM. Observed and modelled soil carbon and nitrogen changes after planting a Pinus radiata stand onto former pasture. Soil Biology and Biochemistry, 2008, 40: 247-257
[23] Sartori F, Lal R, Ebinger MH, et al. Changes in soil carbon and nutrient pools along a chronosequence of poplar plantations in the Columbia Plateau, Oregon, USA. Agriculture, Ecosystems & Environment, 2007, 122: 325-339
[24] Ritter E. Carbon, nitrogen and phosphorus in volcanic soils following afforestation with native birch (Betula pubescens) and introduced larch (Larix sibirica) in Iceland. Plant and Soil, 2007, 295: 239-251
[25] Wang C-M (王春梅), Liu Y-H (刘艳红), Shao B (邵彬), et al. Quantifying the soil carbon changes following the afforestation of former arable land. Journal of Beijing Forestry University (北京林业大学学报), 2007, 29(3): 112-119 (in Chinese)
[26] Paul KI, Polglase PJ, Nyakuengama JG, et al. Change in soil carbon following afforestation. Forest Ecology and Management, 2002, 168: 241-257
[27] Don A, Rebmann C, Kolle O, et al. Impact of afforestation-associated management changes on the carbon balance of grassland. Global Change Biology, 2009, 15: 1990-2002
[28] Lu N, Liski J, Chang RY, et al. Soil organic carbon dynamics of black locust plantations in the middle Loess Plateau area of China. Biogeosciences, 2013, 10: 7053-7063
[29] Ai Z-M (艾泽民), Chen Y-M (陈云明), Cao Y (曹扬). Storage and allocation of carbon and nitrogen in Robinia pseudoacacia plantation at different ages in the loess hilly region, China. Chinese Journal of Applied Ecology (应用生态学报), 2014, 25(2): 333-341 (in Chinese)
[30] Li DF, Shao MA. Soil organic carbon and influencing factors in different landscapes in an arid region of northwestern China. Catena, 2014, 116: 95-104
[31] Wang D (王棣), She D (佘雕), Geng Z-C (耿增超), et al. Vertical distribution of soil active carbon and soil organic carbon storage under different forest. Chinese Journal of Applied Ecology (应用生态学报), 2014, 25(6): 1569-1577 (in Chinese)
[32] Song BL, Yan MJ, Hou H, et al. Distribution of soil carbon and nitrogen in two typical forests in the semiarid region of the Loess Plateau, China. Catena, 2016, 143: 159-166
[33] Wu Q-B (吴庆标), Wang X-K (王效科), Duan X-N (段晓男), et al. Carbon sequestration and its potential by forest ecosystems in China. Acta Ecolgica Sinica (生态学报), 2008, 28(2): 517-524 (in Chinese)
[34] An SS, Huang YM, Zheng FL. Evaluation of soil microbial indices along a revegetation chronosequence in grassland soils on the Loess Plateau, Northwest China. Applied Soil Ecology, 2009, 41: 286-292
[35] Fu BJ, Chen LD, Ma KM, et al. The relationships between land use and soil conditions in the hilly area of the Loess Plateau in northern Shaanxi, China. Catena, 2000, 39: 69-78
[36] Murty D, Kirschbaum MUF, McMurtie RE, et al. Does conversion of forest to agricultural land change soil carbon and nitrogen? A review of the literature. Global Change Biology, 2002, 8: 105-123
[37] Nelson JDJ, Schoenau JJ, Malhi SS. Soil organic carbon changes and distribution in cultivated and restored grassland soils in Saskatchewan. Nutrient Cycling in Agroecosystems, 2008, 82: 137-148

豫西黄土丘陵区不同林龄栎类和侧柏人工林碳、氮储量

Storage of carbon and nitrogen in Quercus and Platycladus orientalis plantations at different ages in the hilly area of western Henan Province, China.

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 0

编辑推荐

Metrics

本文评价