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Dissolved organic carbon loss fluxes through runoff and sediment on sloping upland of purple soil in the Sichuan Basin

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Abstract

Runoff is a major driver for dissolved organic carbon (DOC) diffusing into aquatic ecosystems. Transport of DOC in runoff is important in the C cycle of soils in an agricultural ecosystem. This study provides a combined dataset on DOC loss pathways and fluxes from sloping upland in the purple soil area of southwestern China. A free-drain lysimeter experiment was conducted to quantify DOC loss through overland flow (2010–2012), interflow (2010–2012) and sediment (2011–2012). Average annual cumulative discharges of overland and interflow were 58.3 ± 3.1 and 289.4 ± 5.4 mm, accounting for 6.8 and 33.8 % of the totals during the entire rainy season, respectively. Average annual cumulative sediment loss flux was 183.5 ± 14.6 g m−2. Average DOC concentrations in overland flow and interflow were 3.44 ± 0.36 and 3.04 ± 0.24 mg L−1, respectively. Average DOC content in sediment was 73.76 ± 4.09 mg kg−1. The relationship between DOC concentration and discharge in overland flow events could be described by a significant exponential decaying function (R = 0.53, P = 0.027). Average annual DOC loss fluxes through overland flow, interflow and sediment were 163.6 ± 28.5, 865.5 ± 82.5 and 9.4 ± 1.5 mg m−2, respectively, and total DOC loss was 1,038.5 ± 112.5 mg m−2. The results suggest that interflow is the major driver of DOC leaching loss on sloping upland. It is shown that interflow is fundamentally important for reducing DOC loss on sloping croplands in the Sichuan Basin and possibly beyond.

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References

  • Asano Y, Uchida T, Mimasu Y, Ohte N (2009) Spatial patterns of stream solute concentrations in a steep mountainous catchment with a homogeneous landscape. Water Resour Res. doi:10.1029/2008WR007466

    Google Scholar 

  • David LK, Yoshimi S, Christopher G (1991) High turnover rates of dissolved organic carbon during a spring phytop1ankton bloom. Nature 352:6l2–6l4

    Article  Google Scholar 

  • Dawson JC, Billett MF, Neal C, Hill S (2002) A comparison of particulate, dissolved and gaseous carbon in two contrasting upland streams in the UK. J Hydrol 257:226–246

    CAS  Google Scholar 

  • Fraser AI, Harrod TR, Haygarth PM (1999) The effect of rainfall intensity on soil erosion and particulate phosphorus transfer from arable soils. Water Sci Technol 39:41–45

    Article  CAS  Google Scholar 

  • Froberg M, Berggren D, Bergkvist B (2005) Dissolved organic carbon leaching from a coniferous forest floor: a field manipulation experiment. Biogeochemistry 75:271–287

    Article  Google Scholar 

  • Fujii K, Uemura M, Hayakawa C, Funakawa S, Kosaki T, Sukartiningsih, Ohta S (2009) Fluxes of dissolved organic carbon in two tropical forest ecosystems of East Kalimantan, Indonesia. Geoderma 152:127–136

    Article  CAS  Google Scholar 

  • Gong ZT (1999) Chinese soil taxonomy. Science Press, Beijing (In Chinese)

    Google Scholar 

  • Grieve IC (1994) Dissolved organic carbon dynamics in two streams draining forested catchments at Loch Ard, Scotland. Hydrol Process 8:457–464

    Article  Google Scholar 

  • Guo ZL, Zhong C, Cai CF, Ding SW, Wang ZM (2008) Nitrogen competition in contour hedgerow systems in subtropical China. Nutr Cycl Agroecosys 81:71–83

    Article  Google Scholar 

  • Haaland S, Mulder J (2010) Dissolved organic carbon concentrations in runoff from shallow heathland catchments: effects of frequent excessive leaching in summer and autumn. Biogeochemistry 97:45–53

    Article  Google Scholar 

  • Hartmann R, Hofman G (2009) Residue cover and rainfall intensity effects on runoff soil organic carbon loss. Catena 78:81–86

    Article  Google Scholar 

  • Jones DL, Willett VB (2006) Experimental evaluation of methods to quantify dissolved organic nitrogen (DON) and dissolved organic carbon (DOC) in soil. Soil Biol Biochem 38:991–999

    Article  CAS  Google Scholar 

  • Jones JR, Knowlton MF, Obrecht DV, Cook EA (2004) Importance of landscape variables and morphology on nutrients in Missouri reservoirs. Can J Fish Aquat Sci 61:1503–1512

    Article  Google Scholar 

  • Kalbitz K, Solinger S, Park JH (2000) Controls on the dynamics of dissolved organic matter in soils: a review. Soil Sci 165:277–304

    Article  CAS  Google Scholar 

  • Kleinman PJA, Srinivasan MS, Dell CJ, Schmidt JP, Sharpley AN, Bryant RB (2006) Role of rainfall intensity and hydrology in nutrient transport via surface runoff. J Environ Qual 35:1248–1259

    Article  CAS  PubMed  Google Scholar 

  • Li Z, Shuman LM (1997) Mobility of Zn, Cd and Pb in soils as affected by poultry litter extract-I. Leaching in soil columns. Environ Pollut 95:219–226

    Article  CAS  PubMed  Google Scholar 

  • Li ZM, Zhang XW, He YR, Tang SJ (1991) Purple soil in China (A). Science Press, Beijing (In Chinese)

    Google Scholar 

  • Li K, Xing B, Torello WA (2005) Effect of organic fertilizers derived dissolved organic matter on pesticide sorption and leaching. Environ Pollut 134:187–194

    Article  CAS  PubMed  Google Scholar 

  • Lohse KA, Brooks PD, McIntosh JC, Meixner T, Huxman TE (2009) Interactions between biogeochemistry and hydrologic systems. Annu Rev Environ Resour 34:65–96

    Article  Google Scholar 

  • Lu RK (1999) Soil agro-chemical analysis methods. China Agroscience Press, Beijing (In Chinese)

    Google Scholar 

  • Martin HC (2003) Dissolved and water–extractable organic matter in soils: a review on the influence of land use and management practices. Geoderma 113:357–380

    Article  Google Scholar 

  • Michalzik B, Tipping E, Mulder J, Gallardo Lancho JF, Matzner E, Clarke N, Lofts S, Vicente Esteban MA (2003) Modelling the production and transport of dissolved organic carbon in forest soils. Biogeochemistry 66(3):241–264

    Article  CAS  Google Scholar 

  • Monaghan RM, Wilcock RJ, Smith LC, Tikkisetty B, Thorrold BS, Costall D (2007) Linkages between land management activities and water quality in an intensively farmed catchment in southern New Zealand. Agric Ecosyst Environ 118:211–222

    Article  Google Scholar 

  • Shi XN, Wu LS, Chen WP, Wang QJ (2011) Solute Transfer from the soil surface to overland flow: a review. Soil Sci Soc Am J 75:1214–1225

    Article  CAS  Google Scholar 

  • Wang T, Zhu B (2011) Nitrate loss via overland flow and interflow from a sloped farmland in the hilly area of purple soil, China. Nutr Cycl Agroecosys 90:309–319

    Article  CAS  Google Scholar 

  • Xiong Y, Li QK (1986) Soils in China. Science Press, Beijing (In Chinese)

    Google Scholar 

  • Zhong XH (2000) Montology outline and mountain research in China. Chengdu, Sichuan Science and Technology Press In Chinese

    Google Scholar 

  • Zhou MH, Zhu B, Klaus BB, Wang T, Jessica B, Nicolas B, Wang ZH, Li TK, Kuang FH (2012) Nitrate leaching, direct and indirect nitrous oxide fluxes from sloping cropland in the purple soil area, southwestern China. Environ Pollut 162:361–368

    Article  CAS  PubMed  Google Scholar 

  • Zhu B, Wang T, Kuang FH, Luo ZX, Tang JL, Xu TP (2009) Measurements of nitrate leaching from a hillslope cropland in the Central Sichuan Basin, China. Soil Sci Soc Am J 73:1419–1426

    Article  CAS  Google Scholar 

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Acknowledgments

Funding for this research project was provided by National Program on Key Basic Research Plan of China (Grant No. 2012CB417101), the Special Program of Strategical Science & Technology of the Chinese Academy of Sciences (Grant No. XDA05050506), Natural Science Foundation of China (Grant No. 41371302) and Talent introduction Program for Anhui Academy of Agricultural Sciences. We sincerely thank Dr. Jialiang Tang and the staff at Yanting station for their support in the field measurements. We also appreciate the constructive comments of two anonymous reviewers.

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Authors and Affiliations

  1. Key Laboratory of Mountain Surface Processes and Ecological Regulation, Chinese Academy of Sciences, Chengdu, 610041, China

    Keke Hua, Bo Zhu & Xiaoguo Wang

  2. Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610041, China

    Keke Hua, Bo Zhu & Xiaoguo Wang

  3. Soil and Fertilizer Research Institute, Anhui Academy of Agricultural Sciences, Hefei, 230001, China

    Keke Hua

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  1. Keke Hua
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  2. Bo Zhu
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  3. Xiaoguo Wang
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Correspondence to Bo Zhu.

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Hua, K., Zhu, B. & Wang, X. Dissolved organic carbon loss fluxes through runoff and sediment on sloping upland of purple soil in the Sichuan Basin. Nutr Cycl Agroecosyst 98, 125–135 (2014). https://doi.org/10.1007/s10705-014-9601-5

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  • DOI: https://doi.org/10.1007/s10705-014-9601-5

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