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Biology and Fertility of Soils

, Volume 53, Issue 7, pp 715–721 | Cite as

Prior exposure to diurnal heating influences soil respiration and N availability upon rewetting

  • Bo Zheng
  • Tan Dang
  • Petra Marschner
Short Communication

Abstract

On sunny summer days, the top 10 cm of soil in southern Australia are heated to temperatures between 50 and 80 °C for a few hours a day, often for several successive days. These extreme temperature events are likely to have profound effects on the microbiota in these soils, but we do not know how this recurrent heat exposure influences microbial dynamics and associated nutrient cycling. In this study, an air-dry soil from southern Australia was exposed to one or two diurnal heating events with maximum temperature of 50 or 70 °C. The control was left at ambient temperature (Amb). All soils were rapidly rewet. Soil respiration was measured for 7 days after rewetting; microbial biomass C, available N and P were determined before rewetting and 1 and 7 days after rewetting. After heating and before rewetting compared to Amb, microbial biomass C (MBC) was 50–80% lower, but available P was 25% higher in heated soils. Available N differed little between Amb and heated soils. Rewetting resulted in a flush of respiration in Amb and soils heated once, but there was no respiration flush in soils heated twice. Cumulative respiration compared to Amb was about 10% higher in soils heated once and about 25% lower in soils heated twice. In Amb, MBC 1 day after rewetting was similar as before rewetting. But in heated soils, MBC increased from before rewetting to 1 day after rewetting about fourfold. Compared to Amb, available N 1 day after rewetting was 20–30% higher in soils heated to 70 °C. Seven days after rewetting, available N was 10% higher than Amb only in soils heated twice to 70 °C. It can be concluded that diurnal heating kills a large proportion of the microbial biomass and influences soil respiration and nutrient availability after rewetting of soils. The effect of heating depends on both maximum temperature and number of events.

Keywords

Available N Diurnal heating Microbial biomass Rewetting Soil respiration 

Notes

Acknowledgements

T. Dang received a postgraduate scholarship from Vietnam International Education Development (VIED).

References

  1. Anderson J, Ingram J (1993) Colorimetric determination of ammonium tropical soil biology and fertility, a handbook of methods, second edn. CAB International, Wallingford, pp 73–74Google Scholar
  2. Austin AT, Yahdjian L, Stark JM, Belnap J, Porporato A, Norton U, Ravetta DA, Schaeffer SM (2004) Water pulses and biogeochemical cycles in arid and semiarid ecosystems. Oecologia 141:221–235. doi: 10.1007/s00442-004-1519-1 CrossRefPubMedGoogle Scholar
  3. Bååth E, Frostegård A, Pennanen T, Fritze H (1995) Microbial community structure and pH response in relation to soil organic matter quality in wood-ash fertilized, clear-cut or burned coniferous forest soils. Soil Biol Biochem 27:229–240. doi: 10.1016/0038-0717(94)00140-v CrossRefGoogle Scholar
  4. Barcenas-Moreno G, Bååth E (2009) Bacterial and fungal growth in soil heated at different temperatures to simulate a range of fire intensities. Soil Biol Biochem 41:2517–2526. doi: 10.1016/j.soilbio.2009.09.010 CrossRefGoogle Scholar
  5. Beringer J, Hutley LB, McHugh I, Arndt SK, Campbell D, Cleugh HA, Cleverly J (2016) An introduction to the Australian and New Zealand flux tower network—Ozflux. Biogeosciences 13:5895–5916CrossRefGoogle Scholar
  6. Borken W, Matzner E (2009) Reappraisal of drying and wetting effects on C and N mineralization and fluxes in soils. Glob Change Biol 15:808–824. doi: 10.1111/j.1365-2486.2008.01681.x CrossRefGoogle Scholar
  7. Bottner P (1985) Response of microbial biomass to alternate moist and dry condition in a soil incubated with 14C-labelled and 15N labelled plant material. Soil Biol Biochem 17:329–337. doi: 10.1016/0038-0717(85)90070-7 CrossRefGoogle Scholar
  8. Brown LE, Holden J, Palmer SM, Johnston K, Ramchunder SJ, Grayson R (2015) Effects of fire on the hydrology, biogeochemistry, and ecology of peatland river systems. Freshwater Sci 34:1406–1425. doi: 10.1086/683426 CrossRefGoogle Scholar
  9. Butterly CR, Marschner P, McNeill AM, Baldock JA (2010) Rewetting CO2 pulses in Australian agricultural soils and the influence of soil properties. Biol Fertil Soils 46:739–753. doi: 10.1007/s00374-010-0481-9 CrossRefGoogle Scholar
  10. Chittleborough D, Oades J (1979) The development of a red-brown earth. I. A reinterpretation of published data. Soil Res 17:371–381CrossRefGoogle Scholar
  11. Feng W, Zhang YQ, Jia X, Wu B, Zha TS, Qin SG, Wang B, Shao CX, Liu JB, Fa KY (2014) Impact of environmental factors and biological soil crust types on soil respiration in a desert ecosystem. PLoS One 9. doi: 10.1371/journal.pone.0102954
  12. Fierer N, Schimel JP (2003) A proposed mechanism for the pulse in carbon dioxide production commonly observed following the rapid rewetting of a dry soil. Soil Sci Soc Amer J 67:798–805CrossRefGoogle Scholar
  13. Fraser FC, Corstanje R, Deeks LK, Harris JA, Pawlett M, Todman LC, Whitmore AP, Ritz K (2016) On the origin of carbon dioxide released from rewetted soils. Soil Biol Biochem 101:1–5. doi: 10.1016/j.soilbio.2016.06.032 CrossRefPubMedPubMedCentralGoogle Scholar
  14. Fumagalli I, Gruening C, Marzuoli R, Cieslik S, Gerosa G (2016) Long-term measurements of NOx and O-3 soil fluxes in a temperate deciduous forest. Agricult Forest Meteorol 228:205–216. doi: 10.1016/j.agrformet.2016.07.011 CrossRefGoogle Scholar
  15. Gee G, Or D (2002) Particle size analysis. In: Dane JH, Topp GC (eds) Methods of soil analysis. Part 4. Physical methods. Soil Science Society of America, Madison, pp 255–294Google Scholar
  16. Goberna M, Garcia C, Insam H, Hernandez M, Verdu M (2012) Burning fire-prone Mediterranean Shrublands: immediate changes in soil microbial community structure and ecosystem functions. Microb Ecol 64:242–255. doi: 10.1007/s00248-011-9995-4 CrossRefPubMedGoogle Scholar
  17. Hanson W (1950) The photometric determination of phosphorus in fertilizers using the phosphovanado-molybdate complex. J Sci Food Agric 1:172–173CrossRefGoogle Scholar
  18. Isbell R (2002) The Australian soil classification. Revised edn (CSIRO Publishing: Collingwood)Google Scholar
  19. Kouno K, Tuchiya Y, Ando T (1995) Measurement of soil microbial biomass phosphorus by an anion exchange membrane method. Soil Biol Biochem 27:1353–1357CrossRefGoogle Scholar
  20. Meisner A, Bååth E, Rousk J (2013) Microbial growth responses upon rewetting soil dried for four days or one year. Soil Biol Biochem 66:188–192. doi: 10.1016/j.soilbio.2013.07.014 CrossRefGoogle Scholar
  21. Meisner A, Leizeaga A, Rousk J, Bååth E (2017) Partial drying accelerates bacterial growth recovery to rewetting. Soil Biol Biochem 112:269–276CrossRefGoogle Scholar
  22. Meisner A, Rousk J, Bååth E (2015) Prolonged drought changes the bacterial growth response to rewetting. Soil Biol Biochem 88:314–322. doi: 10.1016/j.soilbio.2015.06.002 CrossRefGoogle Scholar
  23. Miranda KM, Espey MG, Wink DA (2001) A rapid, simple spectrophotometric method for simultaneous determination of nitrate and nitrite. Nitric Oxide 5:62–71CrossRefPubMedGoogle Scholar
  24. Murphy J, Riley JP (1962) A modified single solution method for the determination of phosphate in natural waters. Anal Chim Acta 27:31–36CrossRefGoogle Scholar
  25. Oliverio AM, Bradford MA, Fierer N (2017) Identifying the microbial taxa which consistently respond to soil warming across time and space. Glob Chang Biol 23:2117–2129CrossRefPubMedGoogle Scholar
  26. Pietikainen J, Pettersson M, Bååth E (2005) Comparison of temperature effects on soil respiration and bacterial and fungal growth rates. FEMS Microbiol Ecol 52:49–58. doi: 10.1016/j.femsec.2004.10.002 CrossRefPubMedGoogle Scholar
  27. Rayment G, Higginson FR (1992) Australian laboratory handbook of soil and water chemical methods. Inkata Press Pty Ltd.Google Scholar
  28. Romanya J, Casals P, Vallejo VR (2001) Short-term effects of fire on soil nitrogen availability in Mediterranean grasslands and shrublands growing in old fields. Forest Ecol Manag 147:39–53. doi: 10.1016/s0378-1127(00)00433-3 CrossRefGoogle Scholar
  29. Romanya J, Khanna PK, Raison RJ (1994) Effects of slash burning on soil phosphorus fractions and sorption and desorption of phosphorus. Forest Ecol Manag 65:89–103. doi: 10.1016/0378-1127(94)90161-9 CrossRefGoogle Scholar
  30. Rutigliano FA, De Mario A, D'Ascoli R, Castaldi S, Gentile A, Virzo de Santo A (2007) Impact of fire on fungal abundance and microbial efficiency in C assimiliation and mineralisation in a Mediterranean maquis soil. Biol Fertil Soils 44:377–381CrossRefGoogle Scholar
  31. Scheer C, Wassmann R, Klenzler K, Lbragimov N, Eschanov R (2008) Nitrous oxide emissions from fertilized irrigated cotton (Gossypium hirsutum L.) in the Aral Sea Basin, Uzbekistan: influence of nitrogen applications and irrigation practices. Soil Biol Biochem 40:290–301. doi: 10.1016/j.soilbio.2007.08.007 CrossRefGoogle Scholar
  32. Setia R, Smith P, Marschner P, Baldock J, Chittleborough D, Smith J (2011) Introducing a decomposition rate modifier in the Rothamsted carbon model to predict soil organic carbon stocks in saline soils. Environ Sci Technol 45:6396–6403CrossRefPubMedGoogle Scholar
  33. Shi A, Marschner P (2015) The number of moist days determines respiration in drying and rewetting cycles. Biol Fertil Soils 51:33–41. doi: 10.1007/s00374-014-0947-2 CrossRefGoogle Scholar
  34. Tucker CL, Reed SC (2016) Low soil moisture during hot periods drives apparent negative temperature sensitivity of soil respiration in a dryland ecosystem: a multi-model comparison. Biogeochemistry 128:155–169. doi: 10.1007/s10533-016-0200-1 CrossRefGoogle Scholar
  35. Van Gestel M, Merckx R, Vlassak K (1993) Microbial biomass responses to soil drying and rewetting: the fate of fast- and slow-growing microorganisms in soils from different climates. Soil Biol Biochem 25:109–123CrossRefGoogle Scholar
  36. Vance ED, Brookes PC, Jenkinson DS (1987) An extraction method for measuring soil microbial biomass C. Soil Biol Biochem 19:703–707. doi: 10.1016/0038-0717(87)90052-6 CrossRefGoogle Scholar
  37. Vanlauwe B, Nwoke O, Sanginga N, Merckx R (1996) Impact of residue quality on the C and N mineralization of leaf and root residues of three agroforestry species. Plant Soil 183:221–231CrossRefGoogle Scholar
  38. Walkley A, Black IA (1934) An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Sci 37:29–38CrossRefGoogle Scholar
  39. Wan SQ, Hui DF, Luo YQ (2001) Fire effects on nitrogen pools and dynamics in terrestrial ecosystems: a meta-analysis. Ecol Appl 11:1349–1365. doi: 10.2307/3060925 CrossRefGoogle Scholar
  40. Wilke B-M (2005) Determination of chemical and physical soil properties. In: Monitoring and Assessing Soil Bioremediation. Springer, pp 47–95Google Scholar
  41. Willis RB, Montgomery ME, Allen PR (1996) Improved method for manual, colorimetric determination of total Kjeldahl nitrogen using salicylate. J Agric Food Chem 44:1804–1807CrossRefGoogle Scholar
  42. Zheng B, Marschner P (2017) Previous residue addition rate and C/N ratio influence nutrient availability and respiration rate after the second residue addition. Geoderma 285:217–224. doi: 10.1016/j.geoderma.2016.10.007 CrossRefGoogle Scholar

Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  1. 1.School of Agriculture, Food and WineThe University of AdelaideAdelaideAustralia

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