Carbon input from 13C-labelled soybean residues in particulate organic carbon fractions in a Mollisol

详细信息    查看全文

• 作者：Tengxiang Lian ; Guanghua Wang ; Zhenhua Yu ; Yansheng Li…
• 关键词：13C labelling ; Soybean residue ; Decomposition rate ; Microbial activity ; Particulate organic carbon
• 刊名：Biology and Fertility of Soils
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：52
• 期：3
• 页码：331-339
• 全文大小：516 KB
• 参考文献：Abiven S, Recous S, Reyes V, Oliver R (2005) Mineralisation of C and N from root, stem and leaf residues in soil and role of their biochemical quality. Biol Fertil Soils 42:119–128CrossRef
  Al-Kaisi MM, Guzman JG (2013) Effects of tillage and nitrogen rate on decomposition of transgenic Bt and near-isogenic non-Bt maize residue. Soil Till Res 129:32–39CrossRef
  An T, Schaeffer S, Zhuang J, Radosevich M, Li S, Li H, Pei J, Wang J (2015) Dynamics and distribution of 13C-labeled straw carbon by microorganisms as affected by soil fertility levels in the Black Soil region of Northeast China. Biol Fertil Soils 51:605–613CrossRef
  Bajgai Y, Kristiansen P, Hulugalle N, McHenry M (2014) Changes in soil carbon fractions due to incorporating corn residues in organic and conventional vegetable farming systems. Soil Res 52:244–252CrossRef
  Balesdent J, Balabane M (1996) Major contribution of roots to soil carbon storage inferred from maize cultivated soils. Soil Biol Biochem 28:1261–1263CrossRef
  Blagodatskaya E, Yuyukina T, Blagodatsky S, Kuzyakov Y (2011) Turnover of soil organic matter and of microbial biomass under C 3–C 4 vegetation change: consideration of 13C fractionation and preferential substrate utilization. Soil Biol Biochem 43:159–166CrossRef
  Bronick CJ, Lal R (2005) Soil structure and management: a review. Geoderma 124:3–22CrossRef
  Butterly C, Bhatta Kaudal B, Baldock J, Tang C (2011) Contribution of soluble and insoluble fractions of agricultural residues to short-term pH changes. Eur J Soil Sc 62:718–727CrossRef
  Cambardella C, Elliott E (1992) Particulate soil organic-matter changes across a grassland cultivation sequence. Soil Sci Soc Am J 56:777–783CrossRef
  Cambardella C, Elliott E (1993) Methods for physical separation and characterization of soil organic matter fractions. Geoderma 56:449–457CrossRef
  Cattaneo F, Barbanti L, Gioacchini P, Ciavatta C, Marzadori C (2014) 13C abundance shows effective soil carbon sequestration in Miscanthus and giant reed compared to arable crops under Mediterranean climate. Biol Fertil Soils 50:1121–1128CrossRef
  Chan K (1997) Consequences of changes in particulate organic carbon in vertisols under pasture and cropping. Soil Sci Soc Am J 61:1376–1382CrossRef
  Chenu C, Plante AF (2006) Clay-sized organo–mineral complexes in a cultivation chronosequence: revisiting the concept of the ‘primary organo–mineral complex’. Eur J Soil Sci 57:596–607CrossRef
  Chivenge P, Vanlauwe B, Gentile R, Six J (2011) Comparison of organic versus mineral resource effects on short-term aggregate carbon and nitrogen dynamics in a sandy soil versus a fine textured soil. Agr Ecosyst Environ 140:361–371CrossRef
  Christensen B (1996) Carbon in primary and secondary organomineral complexes. In: Cater MR, Stewart BA (eds) Structure and organic matter storage in agricultural soils. CRC Press, Boca Ratons, pp 97–165
  Comeau LP, Lemke R, Knight J, Bedard-Haughn A (2013) Carbon input from 13C-labeled crops in four soil organic matter fractions. Biol Fertil Soils 49:1179–1188CrossRef
  Dignac MF, Bahri H, Rumpel C, Rasse DP, Bardoux G, Balesdent J, Girardin C, Chenu C, Mariotti A (2005) Carbon-13 natural abundance as a tool to study the dynamics of lignin monomers in soil: an appraisal at the Closeaux experimental field (France). Geoderma 128:3–17CrossRef
  Domanski G, Kuzyakov Y, Siniakina S, Stahr K (2001) Carbon flows in the rhizosphere of ryegrass (Lolium perenne). J Plant Nutr Soil Sc 164:381–387CrossRef
  Fabrizzi KP, Moron A, García FO (2003) Soil carbon and nitrogen organic fractions in degraded vs. non-degraded Mollisols in Argentina. Soil Sci Soc Am J 67:1831–1841CrossRef
  Fan F, Yang Q, Li Z, Wei D, Xa C, Liang Y (2011) Impacts of organic and inorganic fertilizers on nitrification in a cold climate soil are linked to the bacterial ammonia oxidizer community. Microb Ecol 62:982–990CrossRef PubMed
  Fan F, Yin C, Tang Y, Li Z, Song A, Wakelin SA, Zou J, Liang Y (2014) Probing potential microbial coupling of carbon and nitrogen cycling during decomposition of maize residue by 13C-DNA-SIP. Soil Biol Biochem 70:12–21CrossRef
  Gill R, Burke IC, Milchunas DG, Lauenroth WK (1999) Relationship between root biomass and soil organic matter pools in the shortgrass steppe of eastern Colorado. Ecosystems 2:226–236CrossRef
  Goering HK, Van Soest PJ (1970) Forage fiber analyses (apparatus, reagents, procedures, and some applications). USDA Agr Handb
  Hadas A, Kautsky L, Goek M, Kara EE (2004) Rates of decomposition of plant residues and available nitrogen in soil, related to residue composition through simulation of carbon and nitrogen turnover. Soil Biol Biochem 36:255–266CrossRef
  Haynes RJ, Mokolobate MS (2001) Amelioration of Al toxicity and P deficiency in acid soils by additions of organic residues: a critical review of the phenomenon and the mechanisms involved. Nutr Cycl Agroecosys 59:47–63CrossRef
  Helfrich M, Ludwig B, Buurman P, Flessa H (2006) Effect of land use on the composition of soil organic matter in density and aggregate fractions as revealed by solid-state 13C NMR spectroscopy. Geoderma 136:331–341CrossRef
  Hütsch BW, Augustin J, Merbach W (2002) Plant rhizodeposition—an important source for carbon turnover in soils. J Plant Nutr Soil Sc 165:397–407CrossRef
  Jacinthe PA, Lal R, Kimble J (2002) Carbon budget and seasonal carbon dioxide emission from a central Ohio Luvisol as influenced by wheat residue amendment. Soil Till Res 67:147–157CrossRef
  Janssen B (1996) Nitrogen mineralization in relation to C: N ratio and decomposability of organic materials. Plant Soil 181:39–45CrossRef
  Jin J, Liu XB, Wang GH, Mi L, Shen ZB, Chen XL, Herbert SJ (2010) Agronomic and physiologic contributions to the yield improvement of soybean cultivars released from 1950 to 2006 in Northeast China. Field Crop Res 115:116–123CrossRef
  Jin J, Wang G, Liu J, Yu Z, Liu X, Herbert SJ (2013) The fate of soyabean photosynthetic carbon varies in Mollisols differing in organic carbon. Eur J Soil Sc 64:500–507CrossRef
  Joergensen RG (1996) The fumigation-extraction method to estimate soil microbial biomass: calibration of the k(EC) value. Soil Biol Biochem 28:25–31CrossRef
  Kögel-Knabner I (1993) Biodegradation and humification processes in forest soils. Soil Biochem 8:101–105
  Kögel-Knabner I (2002) The macromolecular organic composition of plant and microbial residues as inputs to soil organic matter. Soil Biol Biochem 34:139–162CrossRef
  Kong AY, Six J (2010) Tracing root vs. residue carbon into soils from conventional and alternative cropping systems. Soil Sci Soc Am J 74:1201–1210CrossRef
  Kong AY, Six J, Bryant DC, Denison RF, Van Kessel C (2005) The relationship between carbon input, aggregation, and soil organic carbon stabilization in sustainable cropping systems. Soil Sci Soc Am J 69:1078–1085CrossRef
  Li Z, Liu M, Wu X, Han F, Zhang T (2010) Effects of long-term chemical fertilization and organic amendments on dynamics of soil organic C and total N in paddy soil derived from barren land in subtropical China. Soil Till Res 106:268–274CrossRef
  Liu X, Herbert SJ (2002) Fifteen years of research examining cultivation of continuous soybean in northeast China: a review. Field Crop Res 79:1–7CrossRef
  Liu X, Herbert S, Hashemi A, Zhang X, Ding G (2006) Effects of agricultural management on soil organic matter and carbon transformation—a review. Plant Soil Environ 52:531–543
  Liu X, Burras CL, Kravchenko YS, Duran A, Huffman T, Morras H, Studdert G, Zhang X, Cruse RM, Yuan X (2012) Overview of Mollisols in the world: distribution, land use and management. Can J Soil Sci 92:383–402CrossRef
  Lu Y, Watanabe A, Kimura M (2003) Carbon dynamics of rhizodeposits, root-and shoot-residues in a rice soil. Soil Biol Biochem 35:1223–1230
  Majumder B, Kuzyakov Y (2010) Effect of fertilization on decomposition of 14C labelled plant residues and their incorporation into soil aggregates. Soil Till Res 109:94–102CrossRef
  Malhi S, Kutcher H (2007) Small grains stubble burning and tillage effects on soil organic C and N, and aggregation in northeastern Saskatchewan. Soil Till Res 94:353–361CrossRef
  Marschner B, Noble AD (2000) Chemical and biological processes leading to the neutralisation of acidity in soil incubated with litter materials. Soil Biol Biochem 32:805–813CrossRef
  Marschner P, Umar S, Baumann K (2011) The microbial community composition changes rapidly in the early stages of decomposition of wheat residue. Soil Biol Biochem 43:445–451CrossRef
  Marschner P, Hatam Z, Cavagnaro T (2015) Soil respiration, microbial biomass and nutrient availability after the second amendment are influenced by legacy effects of prior residue addition. Soil Biol Biochem 88:169–177CrossRef
  Mazzilli SR, Kemanian AR, Ernst OR, Jackson RB, Piñeiro G (2015) Greater humification of belowground than aboveground biomass carbon into particulate soil organic matter in no-till corn and soybean crops. Soil Biol Biochem 85:22–30CrossRef
  Nicolardot B, Bouziri L, Bastian F, Ranjard L (2007) A microcosm experiment to evaluate the influence of location and quality of plant residues on residue decomposition and genetic structure of soil microbial communities. Soil Biol Biochem 39:1631–1644CrossRef
  Plante AF, Conant RT, Stewart CE, Paustian K, Six J (2006) Impact of soil texture on the distribution of soil organic matter in physical and chemical fractions. Soil Sci Soc Am J 70:287–296CrossRef
  Pocknee S, Sumner ME (1997) Cation and nitrogen contents of organic matter determine its soil liming potential. Soil Sci Soc Am J 61:86–92CrossRef
  Poirier V, Angers DA, Rochette P, Whalen JK (2013) Initial soil organic carbon concentration influences the short-term retention of crop-residue carbon in the fine fraction of a heavy clay soil. Biol Fertil Soils 49:527–535CrossRef
  Puttaso A, Vityakon P, Rasche F, Saenjan P, Treloges V, Cadisch G (2013) Does organic residue quality influence carbon retention in a tropical sandy soil? Soil Sci Soc Am J 77:1001–1011CrossRef
  Qin J, Yang RQ, Jiang CX, Li WB, Li YH, Guan RX, Chang RZ, Qiu LJ (2010) Discovery and transmission of functional QTL in the pedigree of an elite soybean cultivar Suinong 14. Plant Breed 129:235–242CrossRef
  Rasse DP, Rumpel C, Dignac MF (2005) Is soil carbon mostly root carbon? Mechanisms for a specific stabilisation. Plant Soil 269:341–356CrossRef
  Rasse DP, Dignac MF, Bahri H, Bahri C, Rumpel A, Mariotti CC (2006) Lignin turnover in an agricultural field: from plant residues to soil-protected fractions. Eur J Soil Sci 57:530–538CrossRef
  Rui J, Peng J, Lu Y (2009) Succession of bacterial populations during plant residue decomposition in rice field soil. Appl Environ Microb 75:4879–4886CrossRef
  Salvo L, Hernández J, Ernst O (2010) Distribution of soil organic carbon in different size fractions, under pasture and crop rotations with conventional tillage and no-till systems. Soil Till Res 109:116–122CrossRef
  Sangster A, Knight D, Farrell R, Bedard‐Haughn A (2010) Repeat-pulse 13CO2 labeling of canola and field pea: implications for soil organic matter studies. Rapid Commun Mass Sp 24:2791–2798CrossRef
  Schmidt MWI, Torn MS, Abiven S, Dittmar T, Guggenberger G, Janssens IA, Kleber M, Kögel-Knabner I, Lehmann J, Manning DAC, Nannipieri P, Rasse DP, Weiner S, Susan E, Trumbore SE (2011) Persistence of soil organic matter as an ecosystem property. Nature 478:49–56CrossRef PubMed
  Shinjo H, Fujita H, Gintzburger G, Kosaki T (2000) Soil aggregate stability under different landscapes and vegetation types in a semiarid area in northeastern Syria. Soil Sci Plant Nutr 46:229–240CrossRef
  Six J, Conant R, Paul EA, Paustian K (2002) Stabilization mechanisms of soil organic matter: implications for C-saturation of soils. Plant Soil 241:155–176CrossRef
  Six J, Bossuyt H, Degryze S, Denef K (2004) A history of research on the link between (micro) aggregates, soil biota, and soil organic matter dynamics. Soil Till Res 79:7–31CrossRef
  Smil V (1999) Crop residues: agriculture’s largest harvest crop residues incorporate more than half of the world's agricultural phytomass. Bioscience 49:299–308CrossRef
  Steel RG, Torrie JH (1980) Principles and procedures of statistics: a biometrical approach, 2nd edn. McGraw-Hill, New York
  Tian G, Badejo M, Okoh A, Ishida F, Kolawole G, Hayashi Y, Salako F (2007) Effects of residue quality and climate on plant residue decomposition and nutrient release along the transect from humid forest to Sahel of West Africa. Biogeochemistry 86:217–229CrossRef
  Tong X, Xu M, Wang X, Bhattacharyya R, Zhang W, Cong R (2014) Long-term fertilization effects on organic carbon fractions in a red soil of China. Catena 113:251–259CrossRef
  Trinsoutrot I, Recous S, Bentz B, Linères M, Chèneby D, Nicolardot B (2000) Biochemical quality of crop residues and carbon and nitrogen mineralization kinetic under nonlimiting nitrogen conditions. Soil Sci Soc Am J 64:918–926CrossRef
  Vance E, Brookes P, Jenkinson D (1987) An extraction method for measuring soil microbial biomass C. Soil Biol Biochem 19:703–707CrossRef
  Wang Y, Xu J, Shen J, Luo Y, Scheu S, Ke X (2010) Tillage, residue burning and crop rotation alter soil fungal community and water-stable aggregation in arable fields. Soil Till Res 107:71–79CrossRef
  Wang J, Thornton B, Yao H (2014) Incorporation of urea-derived 13C into microbial communities in four different agriculture soils. Biol Fertil Soils 50:603–612CrossRef
  Wills RBH, Balmer N, Greenfield H (1980) Composition of Australian foods, 2. Methods of analysis. Food Technology in Australia
  Xu J, Tang C, Chen ZL (2006) The role of plant residues in pH change of acid soils differing in initial pH. Soil Biol Biochem 38:709–719CrossRef
  Yan F, Schubert S, Mengel K (1996) Soil pH changes during legume growth and application of plant material. Biol Fertil Soils 23:236–242CrossRef
  
• 作者单位：Tengxiang Lian (1) (2)
  Guanghua Wang (1)
  Zhenhua Yu (1)
  Yansheng Li (1)
  Xiaobing Liu (1)
  Jian Jin (1)
  
  1. Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin, 150081, China
  2. University of Chinese Academy of Sciences, Beijing, 100049, China
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Life Sciences
  Agriculture
  Soil Science and Conservation
  
• 出版者：Springer Berlin / Heidelberg
• ISSN：1432-0789

文摘

Understanding the decomposition processes of crop residues and the quantity of residue carbon (C) incorporated into soil organic C (SOC) pools in the soil is crucial for optimizing C management in agricultural systems. This study is highly valuable in Mollisols in northeastern China, where SOC is markedly decreasing. Soybean is a major crop in this region; however, the decomposition processes of soybean residues and their contributions to physically separated SOC pools remain unknown. Thus, a 150-day incubation experiment was conducted with different 13C-labelled residues of soybean, i.e., leaf, stalk, and root, incorporated into a Mollisol. The leaves had the highest decomposition rate. At the end of the incubation, cumulative respiration reached 7.76 mg CO<sub>2sub>-C g−1 in the leaf-incorporated soil, but only 5.98 and 5.51 mg CO<sub>2sub>-C g−1 was recorded for the stalk- and root-amended soils. Furthermore, similar trends were found for the microbial biomass C and dissolved organic C. Different residue sources greatly affected the residue-derived C incorporation in the SOC fractions, resulting in a ranking of root > stalk > leaf. The root-derived C incorporation values were 49.5, 17.2, and 5.0 g residue C kg−1 in the coarse particulate organic C (POC), fine POC, and mineral-associated C (MOC) fractions, respectively, which were significantly higher than those for the stalk- and leaf-derived C. These results indicate that C input from roots can play an important role in C stability in this Mollisol by incorporating more C in the POC and MOC.