Abstract
We measured DOM fluxes from the O horizon of Hawaiiansoils that varied in nutrient availability and mineralcontent to examine what regulates the flux ofdissolved organic carbon (DOC), nitrogen (DON) andphosphorus (DOP) from the surface layer of tropicalsoils. We examined DOM fluxes in a laboratory study from N, P and N+Pfertilized and unfertilized sites on soils that rangedin age from 300 to 4 million years old. The fluxesof DOC and DON were generally related to the % Cand % N content of the soils across the sites. Ingeneral, CO2 and DOC fluxes were not correlatedsuggesting that physical desorption, dissolution andsorption reactions primarily control DOM release fromthese surface horizons. The one exception to thispattern was at the oldest site where there was asignificant relationship between DOC and CO2flux. The oldest site also contained the lowestmineral and allophane content of the three sites andthe DOC-respiration correlation indicates arelationship between microbial activity and DOC fluxat this site. N Fertilization increased DON fluxes by50% and decreased DOC:DON ratios in the youngest,most N poor site. In the older, more N rich sites, Nfertilization neither increased DON fluxes nordecreased DOM C:N ratios. Similarly, short termchanges in N availability in laboratory-based soil Nand P fertilization experiments did not affect the DOMC:N ratios of leachate. DOM C:N ratios were similar tosoil organic matter C:N ratios, and changes in DOM C:Nratios with fertilization appeared to have beenmediated through long term effects on SOM C:N ratiosrather than through changes in microbial demand for Cand N. There was no relationship between DON andinorganic N flux during these incubations suggestingthat the organic and inorganic components of N fluxfrom soils are regulated by different factors and thatDON fluxes are not coupled to immediate microbialdemand for N. In contrast to the behavior of DON, thenet flux of dissolved organic phosphorus (DOP) and DOMC:P ratios responded to both long-term P fertilizationand natural variation in reactive P availability. There was lower DOP flux and higher DOM C:P ratiosfrom soils characterized by low P availability andhigh DOP flux and narrow DOM C:P ratios in sites withhigh P availability. DOP fluxes were also closelycorrelated with dissolved inorganic P fluxes. PFertilization increased DOP fluxes by 73% in theyoungest site, 31% in the P rich intermediate agesite and 444% in the old, P poor site indicating thatDOP fluxes closely track P availability in soils.
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References
Beck T, Joergensen G, Kandeler E, Makeschin F, Nuss E, Oberholzer HR & Scheu S (1997) An inter-laboratory comparison of ten different ways of measuring soil microbial biomass C. Soil Biol. Biochem. 29: 1023–1032
Brookes PC, Landman A, Pruden G & Jenkinson DS (1985) Chloroform fumigation and the release of soil nitrogen: a rapid direct extraction method to measure microbial biomass nitrogen in soil. Soil Biol. Biochem. 17: 837–842
Brooks PD, McKnight DM & Bencala EE (1999) The relationship between over-winter soil heterotrophic activity and DOC export in high elevation catchments. Water Resour. Res. 35: 1895–1902
Burford JR & Bremner JM (1975) Relationships between dentrification capacities of soils and total water soluble and readily decomposable soil organic matter. Soil Biol. Biochem. 7: 389–394
Chadwick OA, Derry LA, Vitousek PM, Huebert BA & Hedin LO (1999) Changing sources of nutrients during four million years of ecosystem development. Nature 397: 491–497
Christ MJ & David MB (1996) Temperature and moisture effects on the flux of dissolved organic carbon in a Spodosol. Soil Biol. Biochem. 28: 1191–1199
Crews TE, Kitayama K, Fownes JH, Riley RH, Herber DA, Mueller-Dombois D & Vitousek PM (1995) Changes in soil phosphorus fractions and ecosystem dynamics across a long chronosequence in Hawaii. Ecology 76: 1407–1424
Currie WS, Aber JD, McDowell WH, Boone RD & Magill AH (1996) Vertical transport of dissolved organic C and N under long-term N amendments in pine and hardwood forests. Biogeochemistry 35: 471–505
Gödde M, David MB, Christ MJ, Kaupenjohann M & Vance GF (1996) Carbon mobilization from the forest floor under red spruce in the northeastern U.S.A. Soil Biol. Biochem. 28: 1181–1189
Gressel N, McColl JG, Preston CM, Newman RH and Powers RF (1996) Linkages between phosphorus transformations and carbon composition in a forest soil. Biogeochemistry 33: 97–123.
Hedin LO, Armesto JJ & Johnson AH (1995) Patterns of nutrient loss from unpolluted oldgrowth temperate forest: evaluation of biogeochemical theory. Ecology 76: 493–509
Herbert DA & Fownes JH (1995) Phosphorus limitation of forest leaf area and net primary productivity on highly weather tropical montane soils in Hawaii. Biogeochemistry 29: 223–235
Jandl R & Sollins P (1997) Water-extractable soil carbon in relation to the belowground carbon cycle. Biol. Fertility Soils 25: 196–201
Johnson DW, Cole DW, van Meigroet H, Horng FW(1986) Factors affecting anion movement and retention in four forest soils. Soil Sci. Soc. Am. J. 50: 776–783
Kaiser K, Guggenberger G & Zech W (1996) Sorption of DOM and DOM fractions to forest soils. Geoderma 74: 281–303
Kaiser K & Zech W (1998) Soil dissolved organic matter sorption as influenced by organic and sesquioxide coating and sorbed sulfate. Soil Sci. Soc. Am. J. 62: 129–136
Kielland K (1994) Amino acid absorption by arctic plans: implications for plant nutrition and nitrogen cycling. Ecology 75: 2373–2383
Lajtha K, Seely B & Valiela I (1995) Retention and leaching losses of atmospherically-derived nitrogen in the aggrading coastal watershed of Waquoit Bay, MA. Biogeochemistry 28: 33–54
McDowell WH & Wood T (1984) Podzolization: soil processes control dissolved organic carbon concentrations in stream water. Soil Science 137: 23–32
McDowell WH & Likens GE (1988) Origin, composition and flux of dissolved organic carbon in the Hubbard Brook Valley. Ecological Monographs 58: 177–195
McDowell WH (1998) Internal nutrient fluxes in a Puerto Rican rain forest. J. Tropical Ecology 14: 521–536
McGill WB & Cole CV (1981) Comparative aspects of cycling of organic carbon, nitrogen, sulfur and phosphorus through soil organic matter. Geoderma 26: 267–286
Moore TR & Jackson RJ (1989) Dynamics of dissolved organic carbon in forested and disturbed catchments, Westland, New Zealand, 2. Larry River. Water Resour. Res. 25: 1331
Moore TR, de Souza W & Koprivnjak JF (1992) Controls on the sorption of dissolved organic carbon by soils. Soil Science 154 (2): 120–129
Moore TR & Dalva M (in review) Controls on the release of dissolved organic carbon by plant tissues and soils. Soil Sci. Soc. Am. J.
Nelson PN, Baldock JA & Oades JM (1993) Concentration and composition of dissolved organic carbon in streams in relation to catchment soil properties. Biogeochemistry 19: 27–50
Nodvin SC, Driscoll CT & Likens GE (1986) Simple partitioning of anions and dissolved organic carbon in a forest soil. Soil Science 142: 27–35
Olander LP & Vitousek PM (in press) How nitrogen and phosphorus availability regulate the activity of soil enzymes essential to nitrogen and phosphorus mineralization. Biogeochemistry
Qualls RG, Haines BL & Swank WT (1991) Fluxes of dissolved organic nutrients and humic substances in a deciduous forest. Ecology 72: 254–266
Qualls RG & BL Haines (1992) Biodegradability of dissolved organic matter in forest throughfall, soil solution and stream water. Soil Sci. Soc. Am. J. 56: 578–586
Seto M & Yanagiya K (1983) Rate of carbon dioxide evolution from soil in relation to temperature and amount of dissolved organic carbon. Jap. J. Ecol. 33: 199–206
Schoenau JJ & Bettany JR (1987) Organic matter leaching as a component of carbon, nitrogen, phosphorus and sulfur cycles in a forest, grassland and gleyed soil. Soil Sci. Soc. Am. J. 51: 646–651
Sollins P & McCorison FM (1981) Nitrogen and carbon solution chemistry of an old growth coniferous forest watershed before and after cutting. Water Resour. Res. 17: 1409–1418
Solorzano L & Sharp JH (1980) Determination of total dissolved nitrogen in natural waters. Limnology and Oceanography 25: 751–754
Toland DE & Zak DR (1994) Seasonal patterns of soil respiration in intact and clear-cut northern hardwood forests. Canad. J. Forest Res. 24: 1711–1716
Torn MS, Trumbore SE, Chadwick OA, Vitousek PM & Hendricks DM(1997) Mineral control of soil organic matter carbon storage and turnover. Nature 389: 170–173
Vance GF & David MB (1992) Dissolved organic carbon and sulfate sorption by Spodosol mineral horizons. Soil Science 154: 136–144
Vitousek PM, Walker LR, Whiteaker LD & Matson PA (1993) Nutrient limitation to plant growth during primary succession in Hawaii Volcanos National Park. Biogeochemistry 23: 197–215
Vitousek PM & Farrington H (1997) Nutrient limitation and soil development: experimental test of a biogeochemical theory. Biogeochemistry 37: 63–75
Vitousek PM, Hedin LO, Matson PA, Fownes JH & Neff JC (1998) Within-system element cycles, input-output budgets and nutrient limitation. In: Groffman PM & Pace ML (Eds) Successes, Limitations and Frontiers in Ecosystem Science (pp 432–451). Springer, New York
Zsolnay A & Steindl H (1991) Geovariability and biodegradability of the water-extractable organic material in an agricultural soil. Soil Biol. Biochem. 23: 1077–1082
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Neff, J.C., Hobbie, S.E. & Vitousek, P.M. Nutrient and mineralogical control on dissolved organic C, N and P fluxes and stoichiometry in Hawaiian soils. Biogeochemistry 51, 283–302 (2000). https://doi.org/10.1023/A:1006414517212
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DOI: https://doi.org/10.1023/A:1006414517212