YU Xiaofei, ZHANG Yuxia, ZHAO Hongmei, LU Xianguo, WANG Guoping. Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils[J]. Chinese Geographical Science, 2010, 20(3): 209-217. doi: 10.1007/s11769-010-0209-7
Citation: YU Xiaofei, ZHANG Yuxia, ZHAO Hongmei, LU Xianguo, WANG Guoping. Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils[J]. Chinese Geographical Science, 2010, 20(3): 209-217. doi: 10.1007/s11769-010-0209-7

Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils

doi: 10.1007/s11769-010-0209-7
Funds:  Under the auspices of Knowledge Innovation Programs of Chinese Academy of Sciences (No.KZCX2-YW-309);National Natural Science Foundation of China (No.40871089, 40830535)
  • Received Date: 2009-09-11
  • Rev Recd Date: 2010-01-28
  • Publish Date: 2010-04-01
  • The effects of freeze-thaw cycles on sorption/desorption of dissolved organic carbon (DOC) in two wetland soils and one reclaimed wetland soil were investigated. DOC concentrations added were 0-600 mg/L. Laboratory incubations of sorption/desorption of DOC had been carried out at -15℃ for 10 h, and then at +5℃ for 13 h. Soil samples were refrozen and thawed subsequently for 5 cycles. Initial Mass model was used to describe sorption behavior of DOC. The results indicate that freeze-thaw cycles can significantly increase the sorption capacity of DOC and reduce the desorption capacity of DOC in the three soils. The freeze-thaw effects on desorption of DOC in soils increase with the increasing freeze-thaw cycles. The conversion of natural wetlands to soybean farmland can decrease the sorption capacity and increase the desorption capacity of DOC in soils. Global warming and reclamation may increase DOC release, and subsequently increase the loss of carbon and the emission of greenhouse gas.
  • [1] Bao S D,2000.Soil Agrochemical Analysis.Third Edition.Beijing:China Agriculture Press,495.(in Chinese)
    [2] Bullock M S,Kemper W D,Nelson S D,1988.Soil cohesion as affected by freezing,water content,time and tillage.Soil Science Society of America Journal,52(3):770-776.
    [3] Dawson H J,Ugolini F C,Hrutfiord B F et al.,1978.Role of soluble organics in the soil processes of a podzol,Central Cascades,Washington.Soil Science,126(5):290-296.
    [4] Gu B H,Schmitt J,Chen Z H et al.,1994.Adsorption and desorption of natural organic matter on iron-oxide-Mechanisms and models.Environmental Science & Technology,28(1):38-46.DOI:10.1021/es00050a007
    [5] Guggenberger G,Zech W,1992.Retention of dissolved organic carbon and sulfate in aggregated acid forest soils.Journal of Environmetal Quality,21(4):643-653.
    [6] Guggenberger G,Kaise,L,2003.Dissolved organic matter in soil:Challenging the paradigm of sorptive preservation.Geoderma,113(3-4):293-310.DOI:10.1016/S0016-7061(02)00366-X
    [7] Henry H A L,2007.Soil freeze-haw cycle experiments:Trends,methodological weaknesses and suggested improvements.Soil Biology & Biochemistry,39(5):977-986.DOI:10.1016/j.soilbio.2006.11.017
    [8] Hinman W G,1970.Effects of freezing and thawing on some chemical properties of three soils.Canadian Journal of Soil Scicence,50(2):179-182.
    [9] Jardine P M,Weber N L,McCarthy J F.,1989.Mechanisms of dissolved organic carbon adsorption on soil.Soil Science Society of America Journal,53:1378-1385.
    [10] Kaiser L,Zech Z,1999.Release of natural organic matter sorbed to oxides and a subsoil.Soil Science Society of America Journal,63(5):1157-1166.
    [11] Lilienfein J,Quails R G,Uselman S M et al.,2004.Adsorption of dissolved organic and inorganic phosphorus in soils of a weathering chronosequence.Soil Science Society of America Journal,68(2):620-628.
    [12] Lipson D A,Schmidt S K,2004.Seasonal changes in an alpine soil bacterial community in the Colorado Rocky Mountains.Applied and Environmental Microbiology,70(5):2867-2879.DOI:10.1128/AEM.70.5.2867-2879.2004
    [13] Maehlum T,Jenssen P D,Wame W S,1995.Cold-climate constructed wetlands.Water Science and Technology,32(3):95-101.
    [14] Magill A H,Aber J D,2000.Variation in soil net mineralization rates with dissolved organic carbon additions.Soil Biology & Biochemistry,32:597-601.
    [15] Moore T R,Souza W D,Koprivnjak J F,1992.Controls on the sorption of dissolved organic carbon by soils.Soil Science,154(2):120-129.
    [16] Moore T R,Matos L,1999.The influence of source on the sorption of dissolved organic carbon by soils.Canadian Journal of Soil Scicence,79(2):321-324.
    [17] Nodvin S C,Driscoll C T,Likens G E,1986.Simple partitioning of anions and dissolved organic carbon in a forest soil.Soil Science,143(1):27-34.
    [18] Oztas T,Fayetorbay F,2003.Effect of freezing and thawing processes on soil aggregate stability.Catena,52(1):1-8.DOI:10.1016/S0341-8162(02)00177-7
    [19] Raulund-Rasmussen K,Borrggaard O K,Hansen H C B et al.,1998.Effect of natural soil solutes on weathering rates of soil minerals.European Journal of Soil Science,49(3):397-406.
    [20] Riffaldi R,Levi-Minzi R,Saviozzi A et al.,1998.Adsorption on soil of dissolved organic carbon from farmyard manure.Agriculture Ecosystem & Environment,69(2):113-119.
    [21] Schadt C W,Martin A P,Lipson,D A et al,,2003.Seasonal dynamics of previously unknown fungal lineages in tundra soils.Science,301(5638):1359-1361.
    [22] Shen Y H,1999.Sorption of natural dissolved organic matter on soil.Chemosphere,38(7):1505-1515.
    [23] Six J,Bossuyt H,Degryse S,Denef K,2004.A history of research on the link between(micro)aggregates,soil biota,and soil organic matter dynamics.Soil & Tillage Research,79(1):7-31.DOI:10.1016/j.still.2004.03.008
    [24] Sjursen H,Michelsen A,Holmstrup M,2005.Effects of freezethaw cycles on microarthropods and nutrient availability in a sub-Arctic soil.Applied Soil Ecology,28(1):79-93.DOI:10.1016/j.apsoil.2004.06.003
    [25] Su L,Zhang Y S,Lin X Y,2001.Change of iron shape and phosphorus adsorption in paddy soils during alternate drying and wetting process.Plant Nutrition and Fertilizer Science,7(4):410-415.(in Chinese)
    [26] Travis C C,Etnier E L,1981.A survey of sorption relationships for reactive solutes in soil.Journal of Environtal Quality,10(1):8-17.
    [27] Unger P W,1991.Overwinter changes in physical-properties of no-tillage soil.Soil Science Society of America Journal,55(3):778-782.
    [28] Ussiri D A N,Johnson C E,2004.Sorption of organic carbon fractions by Spodosol mineral horizons.Soil Science Society of America Journal,68(1):253-262.
    [29] Vandenbruwane J,De Neve S,Quails R G et al.,2007.Comparison of different isotherm models for dissolved organic carbon DOC and nitrogen DON sorption to mineral soil.Geoderma,139(1-2):144-153.DOI:10.1016/j.geoderma.2007.01.012
    [30] Wang G,Liu J,Wang J et al.,2006.Soil phosphorus forms and their variations in depressional and riparian freshwater wetlands Sanjiang Plain,Northeast China.Geoderma,132(1-2):59-74.DOI:10.1016/j.geoderma.2005.04.021
    [31] Wang G,Liu J,Zhao H et al.,2007.Phosphorus sorption by freeze-thaw treated wetland soils derived from a winter-cold zone.Geoderma,138(1-2):153-161.DOI:10.1016/j.geoderma.2006.11.006
    [32] Williams C F,Agassi M,Letey J et al.,2000.Facilitated transport of napropamide by dissolve organic matter through soil colunms.Soil Science Society of America Journal,64:590-594.
    [33] Zou Y C,Jiang M,Lu X G,2008.Characteristics of wetland soil iron under different ages of reclamation.Environmental Science,29(3):271-275.(in Chinese)
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Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils

doi: 10.1007/s11769-010-0209-7
Funds:  Under the auspices of Knowledge Innovation Programs of Chinese Academy of Sciences (No.KZCX2-YW-309);National Natural Science Foundation of China (No.40871089, 40830535)

Abstract: The effects of freeze-thaw cycles on sorption/desorption of dissolved organic carbon (DOC) in two wetland soils and one reclaimed wetland soil were investigated. DOC concentrations added were 0-600 mg/L. Laboratory incubations of sorption/desorption of DOC had been carried out at -15℃ for 10 h, and then at +5℃ for 13 h. Soil samples were refrozen and thawed subsequently for 5 cycles. Initial Mass model was used to describe sorption behavior of DOC. The results indicate that freeze-thaw cycles can significantly increase the sorption capacity of DOC and reduce the desorption capacity of DOC in the three soils. The freeze-thaw effects on desorption of DOC in soils increase with the increasing freeze-thaw cycles. The conversion of natural wetlands to soybean farmland can decrease the sorption capacity and increase the desorption capacity of DOC in soils. Global warming and reclamation may increase DOC release, and subsequently increase the loss of carbon and the emission of greenhouse gas.

YU Xiaofei, ZHANG Yuxia, ZHAO Hongmei, LU Xianguo, WANG Guoping. Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils[J]. Chinese Geographical Science, 2010, 20(3): 209-217. doi: 10.1007/s11769-010-0209-7
Citation: YU Xiaofei, ZHANG Yuxia, ZHAO Hongmei, LU Xianguo, WANG Guoping. Freeze-thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils[J]. Chinese Geographical Science, 2010, 20(3): 209-217. doi: 10.1007/s11769-010-0209-7
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