HUO Lili, ZOU Yuanchun, LYU Xianguo, ZHANG Zhongsheng, WANG Xuehong, AN Yi. Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China[J]. Chinese Geographical Science, 2018, 28(2): 325-336. doi: 10.1007/s11769-018-0939-5
Citation: HUO Lili, ZOU Yuanchun, LYU Xianguo, ZHANG Zhongsheng, WANG Xuehong, AN Yi. Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China[J]. Chinese Geographical Science, 2018, 28(2): 325-336. doi: 10.1007/s11769-018-0939-5

Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China

doi: 10.1007/s11769-018-0939-5
Funds:  Under the auspices of National Natural Science Foundation of China (No. 41501102, 41471081, 41601104), Science and Technology Innovation Project of China Academy of Agricultural Sciences (No. 2017-cxgc-lyj), Science & Technology Project of Industry (No. 201403014).
More Information
  • Corresponding author: AN Yi.E-mail:family198610@163.com
  • Received Date: 2017-05-03
  • Rev Recd Date: 2017-07-12
  • Publish Date: 2018-04-27
  • Content and density of soil organic carbon (SOC) and labile and stable SOC fractions in peat mire soil in wetland, soybean field and rice paddy field reclaimed from the wetland around Xingkai Lake in Northeast China were studied. Studies were designed to investigate the impact of reclamation of wetland for soybean and rice farming on stability of SOC. After reclamation, SOC content and density in the top 0-30 cm soil layer decreased, and SOC content and density in soybean field were higher than that in paddy field. Content and density of labile SOC fractions also decreased, and density of labile SOC fractions and their ratios with SOC in soybean field were lower than that observed in paddy field. In the 0-30 cm soil layer, densities of labile SOC fractions, namely, dissolved organic carbon (DOC), microbial biomass carbon (MBC), readily oxidized carbon (ROC) and readily mineralized carbon (RMC), in both soybean field and paddy field were all found to be lower than those in wetland by 34.00% and 13.83%, 51.74% and 35.13%, 62.24% and 59.00%, and 64.24% and 17.86%, respectively. After reclamation, SOC density of micro-aggregates (< 0.25 mm) as a stable SOC fraction and its ratio with SOC in 0-5, 5-10, 10-20 and 20-30 cm soil layers increased. SOC density of micro-aggregates in the 0-30 cm soil layer in soybean field was 50.83% higher than that in paddy field. Due to reclamation, SOC density and labile SOC fraction density decreased, but after reclamation, most SOC was stored in a more complex and stable form. Soybean farming is more friendly for sustainable SOC residence in the soils than rice farming.
  • [1] Amundson R, 2001. The carbon budget in soils. Annual Review of Earth and Planetary Sciences, 29:535-562. doi: 10.1146/annurev.earth.29.1.535.
    [2] Asensio V, Vega F A, Covelo E F, 2014. Effect of soil reclamation process on soil C fractions. Chemosphere, 95:511-518. doi: 10.1016/j.chemosphere.2013.09.108
    [3] Bao K S, Zhao H M, Xing W et al., 2011. Carbon accumulation in temperate wetlands of Sanjiang Plain, Northeast China. Soil Science Society of America Journal, 75(6):2386-2397. doi: 10.2136/sssaj2011.0157
    [4] Benbi D K, Brar K, Toor A S et al., 2015a. Total and labile pools of soil organic carbon in cultivated and undisturbed soils in northern India. Geoderma, 237-238:149-158. doi:10.1016/j. geoderma.2014.09.002
    [5] Benbi D K, Brar K, Toor A S et al., 2015b. Sensitivity of labile soil organic carbon pools to long-term fertilizer, straw and manure management in rice-wheat system. Pedosphere, 25(4):534-545. doi: 10.1016/S1002-0160(15)30034-5
    [6] Blair G J, Lefroy R D B, Lisle L, 1995. Soil carbon fractions based on their degree of oxidation, and the development of a carbon management index for agricultural systems. Australian Journal of Agricultural Research, 46(7):1459-1466. doi:10. 1071/AR9951459
    [7] Bockheim J G, Hinkel K M, Nelson F E, 2003. Predicting carbon storage in Tundra Soils of Arctic Alaska. Soil Science Society of America Journal, 67(3):948-950. doi:10.2136/sssaj2003. 9480
    [8] Budge K, Leifeld J, Hiltbrunner E et al., 2011. Alpine grassland soils contain large proportion of labile carbon but indicate long turnover times. Biogeosciences, 8(7):1911-1923. doi:10. 5194/bg-8-1911-2011
    [9] Chen Z M, Wang H Y, Liu X W et al., 2017. Changes in soil microbial community and organic carbon fractions under short-term straw return in a rice-wheat cropping system. Soil and Tillage Research, 165:121-127. doi:10.1016/j.still.2016. 07.018
    [10] Davidson E A, Janssens I A, 2006. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change. Nature, 440(7081):165-173. doi: 10.1038/nature04514
    [11] Eglin T, Ciais P, Piao S L et al., 2010. Historical and future perspectives of global soil carbon response to climate and land-use changes. Tellus B:Chemical and Physical Meteorology, 62(5):700-718. doi:10.1111/j.1600-0889.2010. 00499.x
    [12] Ewing S A, Sanderman J, Baisden W T et al., 2006. Role of large-scale soil structure in organic carbon turnover:evidence from California grassland soils. Journal of Geophysical Research, 111(G3):G03012. doi: 10.1029/2006JG000174
    [13] Fauci M F, Dick R P, 1994. Soil microbial dynamics:short-and long-term effects of inorganic and organic nitrogen. Soil Science Society of America Journal, 58(3):801-806. doi: 10.2136/sssaj1994.03615995005800030023x
    [14] Feller C, Balesdent J, Nicolardot B et al., 2001. Approaching "functional" soil organic matter pools through particle-size fractionation:examples for tropical soils. In:Lal R, Kimble J M, Follett R F, et al. (eds.). Assessment Methods for Soil Carbon. Boca Raton, Florida:Lewis Publishers, 53-67.
    [15] Francaviglia R, Renzi G, Ledda L et al., 2017. Organic carbon pools and soil biological fertility are affected by land use intensity in Mediterranean ecosystems of Sardinia, Italy. Science of the Total Environment, 599-600:789-796. doi: 10.1016/j.scitotenv.2017.05.021
    [16] Gabarrón-Galeote M A, Trigalet S, Van Wesemael B, 2015. Effect of land abandonment on soil organic carbon fractions along a Mediterranean precipitation gradient. Geoderma, 249-250:69-78. doi: 10.1016/j.geoderma.2015.03.007
    [17] Gabriel C E, Kellman L, 2014. Investigating the role of moisture as an environmental constraint in the decomposition of shallow and deep mineral soil organic matter of a temperate coniferous soil. Soil Biology and Biochemistry, 68:373-384. doi: 10.1016/j.soilbio.2013.10.009
    [18] Gerke H H, Rieckh H, Sommer M, 2016. Interactions between crop, water, and dissolved organic and inorganic carbon in a hummocky landscape with erosion-affected pedogenesis. Soil and Tillage Research, 156:230-244. doi:10.1016/j.still.2015. 09.003
    [19] Guidi C, Magid J, Rodeghiero M et al., 2014. Effects of forest expansion on mountain grassland:changes within soil organic carbon fractions. Plant and Soil, 385(1-2):373-387. doi: 10.1007/s11104-014-2315-2
    [20] Guimarães D V, Gonzaga M I S, Da Silva T O et al., 2013. Soil organic matter pools and carbon fractions in soil under different land uses. Soil and Tillage Research, 126:177-182. doi: 10.1016/j.still.2012.07.010
    [21] Haynes R J, 2005. Labile organic matter fractions as central components of the quality of agricultural soils:an overview. Advances in Agronomy, 85:221-268. doi: 10.1016/S0065-2113(04)85005-3
    [22] Huang Z Q, Wan X H, He Z M et al., 2013. Soil microbial biomass, community composition and soil nitrogen cycling in relation to tree species in subtropical China. Soil Biology and Biochemistry, 62:68-75. doi: 10.1016/j.soilbio.2013.03.008
    [23] Huo Lili, Lv Xianguo, 2011. Effect of different reclamation patterns on soil organic carbon distribution of aggregates in the topsoil of the Calamagrostis angustifolia Wetland in Sanjiang Plain, China. China Environmental Science, 31(10):1711-1717. (in Chinese)
    [24] Huo L L, Chen Z K, Zou Y C et al., 2013. Effect of Zoige alpine wetland degradation on the density and fractions of soil organic carbon. Ecological Engineering, 51:287-295. doi: 10.1016/j.ecoleng.2012.12.020
    [25] Huo L L, Guo J W, Zou Y C et al., 2015. Effect of reclamation on microbial biomass and activity in peat mire soil around Xingkai Lake in northeast China. Fresenius Environmental Bulletin, 24(3B):1098-1107
    [26] Joergensen R G, 1996. The fumigation-extraction method to estimate soil microbial biomass:calibration of the kEC value. Soil Biology and Biochemistry, 28(1):25-31. doi: 10.1016/0038-0717(95)00102-6
    [27] Jones D L, Willett V B, 2006. Experimental evaluation of methods to quantify dissolved organic nitrogen (DON) and dissolved organic carbon (DOC) in soil. Soil Biology and Biochemistry, 38(5):991-999. doi:10.1016/j.soilbio.2005. 08.012
    [28] Kögel-Knabner I, Amelung W, Cao Z H et al., 2010. Biogeochemistry of paddy soils. Geoderma, 157(1-2):1-14. doi: 10.1016/j.geoderma.2010.03.009
    [29] Ladd J N, Oades J M, Amato M, 1981. Microbial biomass formed from 14C, 15N-labelled plant material decomposing in soils in the field. Soil Biology and Biochemistry, 13(2):119-126. doi: 10.1016/0038-0717(81)90007-9
    [30] Lal R, 2004. Soil carbon sequestration to mitigate climate change. Geoderma, 123(1-2):1-22. doi:10.1016/j.geoderma.2004.01. 032
    [31] Liao J D, Boutton T W, 2008. Soil microbial biomass response to woody plant invasion of grassland. Soil Biology and Biochemistry, 40(5):1207-1216. doi:10.1016/j.soilbio.2007. 12.018
    [32] Loginow W, Wisniewski W, Gonet S S et al., 1987. Fractionation of organic carbon based on susceptibility to oxidation. Polish Journal of Soil Science, 20(1):47-52.
    [33] McLauchlan K K, Hobbie S E, 2004. Comparison of labile soil organic matter fractionation techniques. Soil Science Society of America Journal, 68(5):1616-1625. doi:10.2136/sssaj2004. 1616
    [34] Müller M, Alewell C, Hagedorn F, 2009. Effective retention of litter-derived dissolved organic carbon in organic layers. Soil Biology and Biochemistry, 41(6):1066-1074. doi:10.1016/j. soilbio.2009.02.007
    [35] Nahrawi H, Husni M H A, Radziah O, 2012. Labile carbon and carbon management index in peat planted with various crops. Communications in Soil Science and Plant Analysis, 43(12):1647-1657. doi: 10.1080/00103624.2012.681736
    [36] Nie M, Pendalla E, Bellb C et al., 2014. Soil aggregate size distribution mediates microbial climate change feedbacks. Soil Biology and Biochemistry, 68:357-365. doi:10.1016/j.soilbio. 2013.10.012
    [37] Nyamadzawo G, Nyamangara J, Nyamugafata P et al., 2009. Soil microbial biomass and mineralization of aggregate protected carbon in fallow-maize systems under conventional and no-tillage in Central Zimbabwe. Soil and Tillage Research, 102(1):151-157. doi: 10.1016/j.still.2008.08.007
    [38] Pabst H, Kühnel A, Kuzyakova Y, 2013. Effect of land-use and elevation on microbial biomass and water extractable carbon in soils of Mt. Kilimanjaro ecosystems. Applied Soil Ecology, 67:10-19. doi: 10.1016/j.apsoil.2013.02.006
    [39] Plante A F, Fernández J M, Haddix M L et al., 2011. Biological, chemical and thermal indices of soil organic matter stability in four grassland soils. Soil Biology and Biochemistry, 43(5):1051-1058. doi: 10.1016/j.soilbio.2011.01.024
    [40] Poeplau C, Don A, 2013. Sensitivity of soil organic carbon stocks and fractions to different land-use changes across Europe. Geoderma, 192:189-201. doi:10.1016/j.geoderma.2012.08. 003
    [41] Powlson D S, Prookes P C, Christensen B T, 1987. Measurement of soil microbial biomass provides an early indication of changes in total soil organic matter due to straw incorporation. Soil Biology and Biochemistry, 19(2):159-164. doi:10. 1016/0038-0717(87)90076-9
    [42] Puissant J, Mills R T E, Robroek B J M et al., 2017. Climate change effects on the stability and chemistry of soil organic carbon pools in a subalpine grassland. Biogeochemistry, 132(1-2):123-139. doi: 10.1007/s10533-016-0291-8
    [43] Qualls R G, Richardson C J, 2003. Factors controlling concentration, export, and decomposition of dissolved organic nutrients in the Everglades of Florida. Biogeochemistry, 62(2):197-229. doi: 10.1023/A:1021150503664
    [44] Raiesi F, Beheshti A, 2014. Soil specific enzyme activity shows more clearly soil responses to paddy rice cultivation than absolute enzyme activity in primary forests of northwest Iran. Applied Soil Ecology, 75:63-70. doi:10.1016/j.apsoil.2013. 10.012
    [45] Schlesinger W H, Bernhardt E S, 2013. Chapter 5-The biosphere:the carbon cycle of terrestrial ecosystems. In:Schlesinger W H and Bernhardt E S (eds.). Biogeochemistry (Third Edition). Boston:Academic Press, 135-172.
    [46] Sheng H, Zhou P, Zhang Y Z et al., 2015. Loss of labile organic carbon from subsoil due to land-use changes in subtropical China. Soil Biology and Biochemistry, 88:148-157. doi: 10.1016/j.soilbio.2015.05.015
    [47] Six J, Conant R T, Paul E A et al., 2002. Stabilization mechanisms of soil organic matter:implications for C-saturation of soils. Plant and Soil, 241(2):155-176. doi: 10.1023/A:1016125726789
    [48] Six J, Bossuyt H, Degryze S et al., 2004. A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics. Soil and Tillage Research, 79(1):7-31. doi: 10.1016/j.still.2004.03.008
    [49] Song Changchun, Wang Yiyong, Yan Baixing et al., 2004. The changes of the soil hydrothermal condition and the dynamics of C, N after the mire tillage. Environmental Science, 25(3):150-154. (in Chinese)
    [50] Trumbore S E, Bonani G, Wolfli W, 1990. The Rates of carbon cycling in several soils from AMS14C measurements of fractionated soil organic matter. In:Bouwman A F (ed.). Soils and the Greenhouse Effect. New York:John Wiley and Sons, 405-414.
    [51] Vicente-Vicente J L, Gómez-Muñoz B, Hinojosa-Centeno M B et al., 2017. Carbon saturation and assessment of soil organic carbon fractions in Mediterranean rainfed olive orchards under plant cover management. Agriculture, Ecosystems & Environment, 245:135-146. doi: 10.1016/j.agee.2017.05.020
    [52] Von Lützow M, Kögel-Knabner I, Ekschmitt K et al., 2007. SOM fractionation methods:relevance to functional pools and to stabilization mechanisms. Soil Biology and Biochemistry, 39(9):2183-2207. doi: 10.1016/j.soilbio.2007.03.007
    [53] Walkley A, Black I A, 1934. An examination of the degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Science, 37(1):29-38. doi: 10.1097/00010694-193401000-00003
    [54] Wickings K, Grandy A S, Reed S C et al., 2012. The origin of litter chemical complexity during decomposition. Ecology Letters, 15(10):1180-1188. doi:10.1111/j.1461-0248.2012. 01837.x Wickland K P, Neff J C, Aiken G R, 2007. Dissolved organic carbon in Alaskan boreal forest:sources, chemical characteristics, and biodegradability. Ecosystems, 10(8):1323-1340. doi:10.1007/s10021-007-9101-4
    [55] Wu X, Li Z S., Fu B J et al., 2014. Restoration of ecosystem carbon and nitrogen storage and microbial biomass after grazing exclusion in semi-arid grasslands of Inner Mongolia. Ecological Engineering, 73:395-403. doi:10.1016/j.ecoleng. 2014.09.077
    [56] Xu M, Li X L, Cai X B et al., 2017. Land use alters arbuscular mycorrhizal fungal communities and their potential role in carbon sequestration on the Tibetan Plateau. Scientific Reports, 7:3067. doi: 10.1038/s41598-017-03248-0
    [57] Xu X F, Thornton P E, Post W M, 2013. A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems. Global Ecology and Biogeography, 22(6):737-749. doi: 10.1111/geb.12029
    [58] Yu P J, Li Q, Jia H T et al., 2014. Effect of cultivation on dynamics of organic and inorganic carbon stocks in Songnen plain. Agronomy Journal, 106(5):1574-1582. doi: 10.2134/agronj14.0113
    [59] Yu P J, Liu S W, Han K X et al., 2017. Conversion of cropland to forage land and grassland increases soil labile carbon and enzyme activities in northeastern China. Agriculture, Ecosystems & Environment, 245:83-91. doi:10.1016/j.agee. 2017.05.013
    [60] Zhang C B, Wang J, Liu W L et al., 2010. Effects of plant diversity on microbial biomass and community metabolic profiles in a full-scale constructed wetland. Ecological Engineering, 36(1):62-68. doi: 10.1016/j.ecoleng.2009.09.010
    [61] Zhao S C, Li K J, Zhou W et al., 2016. Changes in soil microbial community, enzyme activities and organic matter fractions under long-term straw return in north-central China.
    [62] griculture, Ecosystems & Environment, 216:82-88. doi:10. 1016/j.agee.2015.09.028
  • 加载中
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(286) PDF downloads(525) Cited by()

Proportional views
Related

Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China

doi: 10.1007/s11769-018-0939-5
Funds:  Under the auspices of National Natural Science Foundation of China (No. 41501102, 41471081, 41601104), Science and Technology Innovation Project of China Academy of Agricultural Sciences (No. 2017-cxgc-lyj), Science & Technology Project of Industry (No. 201403014).
    Corresponding author: AN Yi.E-mail:family198610@163.com

Abstract: Content and density of soil organic carbon (SOC) and labile and stable SOC fractions in peat mire soil in wetland, soybean field and rice paddy field reclaimed from the wetland around Xingkai Lake in Northeast China were studied. Studies were designed to investigate the impact of reclamation of wetland for soybean and rice farming on stability of SOC. After reclamation, SOC content and density in the top 0-30 cm soil layer decreased, and SOC content and density in soybean field were higher than that in paddy field. Content and density of labile SOC fractions also decreased, and density of labile SOC fractions and their ratios with SOC in soybean field were lower than that observed in paddy field. In the 0-30 cm soil layer, densities of labile SOC fractions, namely, dissolved organic carbon (DOC), microbial biomass carbon (MBC), readily oxidized carbon (ROC) and readily mineralized carbon (RMC), in both soybean field and paddy field were all found to be lower than those in wetland by 34.00% and 13.83%, 51.74% and 35.13%, 62.24% and 59.00%, and 64.24% and 17.86%, respectively. After reclamation, SOC density of micro-aggregates (< 0.25 mm) as a stable SOC fraction and its ratio with SOC in 0-5, 5-10, 10-20 and 20-30 cm soil layers increased. SOC density of micro-aggregates in the 0-30 cm soil layer in soybean field was 50.83% higher than that in paddy field. Due to reclamation, SOC density and labile SOC fraction density decreased, but after reclamation, most SOC was stored in a more complex and stable form. Soybean farming is more friendly for sustainable SOC residence in the soils than rice farming.

HUO Lili, ZOU Yuanchun, LYU Xianguo, ZHANG Zhongsheng, WANG Xuehong, AN Yi. Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China[J]. Chinese Geographical Science, 2018, 28(2): 325-336. doi: 10.1007/s11769-018-0939-5
Citation: HUO Lili, ZOU Yuanchun, LYU Xianguo, ZHANG Zhongsheng, WANG Xuehong, AN Yi. Effect of Wetland Reclamation on Soil Organic Carbon Stability in Peat Mire Soil Around Xingkai Lake in Northeast China[J]. Chinese Geographical Science, 2018, 28(2): 325-336. doi: 10.1007/s11769-018-0939-5
Reference (62)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return