Abstract
There is limited information about the impact of residue properties on response of microbial activity to soil salinity. It is well established that salinity decreases soil microbial activity. However, most studies on soil respiration in residue-amended salt-affected soil only used one or two types of plant residues. Residues differ in decomposability which could influence the impact of salinity on soil respiration. The aim of this study was to investigate the impact of salinity on respiration in soil amended with residues differing in chemical composition (lignin concentration, water-soluble organic carbon and C/N ratio). Three experiments were conducted. In the first experiment, finely ground residues differing in chemical composition (shoots of wheat, canola, saltbush and kikuyu, sawdust, eucalypt leaves) were added at 2 % w/w to loam soils differing in salinity: electrical conductivity in a 1:5 soil; water extract (EC1:5) 0.1 (non-saline), 1, 2.5 and 3.3 dS m−1. As expected, cumulative respiration decreased with increasing soil EC, but the negative impact of salinity differed among residues. Based on the regression between cumulative respiration in percentage of the non-saline soil and EC1:5, it was calculated that cumulative respiration would be reduced by 20 % compared with the non-saline soil at EC1:5 0.3 dS m−1 in soil amended with the poorly decomposable sawdust or canola shoots (high C/N ratio, high lignin concentration), but at EC1:5 4 dS m−1 soil with easily decomposable saltbush shoots (low C/N ratio, low lignin concentration). In the second experiment, the C/N ratio of residues with high C/N but different lignin content (canola and sawdust) was adjusted to 20–80 by adding NH4SO4 to the residues prior to mixing them into the soils. In both residues, the decrease in cumulative respiration with increasing salinity was smaller when the C/N ratio was adjusted 20 or 40 compared to the original C/N (82 for canola, 114 for sawdust); cumulative respiration would be reduced by 20 % compared to the non-saline soil at EC1:5 3 (low C/N) compared to 0.7 dS m−1 (high C/N). In the third experiment, water-extractable organic carbon (WEOC) was partially removed by leaching from two residues with high WEOC concentrations (eucalypt leaves and saltbush shoots). Partial removal of WEOC reduced cumulative respiration in the saline soils, but increased the negative effect of salinity on respiration only with saltbush shoots. Compared to the non-saline soil, cumulative respiration was reduced by 20 % at EC1:5 4.5 dS m−1 with unleached saltbush shoots, compared to 1.5 dS m−1 with leached residues. It is concluded that the negative impact of salinity is greater in soils amended with residues with low decomposability, e.g. high C/N and lignin content compared to easily decomposable residues and that N supply is particularly important for adaptation of microbes to salinity.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig1_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig2_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig3_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig4_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig5_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig6_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00374-014-0955-2/MediaObjects/374_2014_955_Fig7_HTML.gif)
Similar content being viewed by others
References
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 42:119–128
Anderson JM, Ingram JSI (1993) Tropical soil biology and fertility: a handbook of methods, 2nd edn. C.A.B... International, Wallingford
Ashraf M, Foolad MR (2007) Roles of glycine betaine and proline in improving plant abiotic stress resistance. Environ Exp Bot 59:206–216
Ashworth J, Keyes D, Kirk R, Lessard R (2001) Standard procedure in the hydrometer method for particle size analysis. Commun Soil Sci Plant Anal 32:633–642
Baldock JA, Masiello C, Gelinas Y, Hedges J (2004) Cycling and composition of organic matter in terrestrial and marine ecosystems. Mar Chem 92:39–64
Baumann K, Marschner P, Smernik RJ, Baldock JA (2009) Residue chemistry and microbial community structure during decomposition of eucalypt, wheat and vetch residues. Soil Biol Biochem 41:1966–1975
Berg B, McClaugherty C (2008) Plant litter: decomposition, humus formation, carbon sequestration. Springer, Berlin
Bradstreet RB (1965) The Kjeldahl method for organic nitrogen. Academic, New York
Chowdhury N, Marschner P, Burns R (2011a) Response of microbial activity and community structure to decreasing soil osmotic and matric potential. Plant Soil 344:241–254
Chowdhury N, Marschner P, Burns RG (2011b) Soil microbial activity and community composition: impact of changes in matric and osmotic potential. Soil Biol Biochem 43:1229–1236
de Souza Silva CMM, Fay EF (2012) Effect of salinity on soil microorganisms. In: Hernandez-Soriano MC (ed) Soil health and land use management, 1st edn. Tech Publisher, Rijeka Croatia, pp 177–198
Ghollarata M, Raiesi F (2007) The adverse effects of soil salinization on the growth of Trifolium alexandrinum L. and associated microbial and biochemical properties in a soil from Iran. Soil Biol Biochem 39:1699–1702
Hagemann M (2011) Molecular biology of cyanobacterial salt acclimation. FEMS Microbiol Rev 35:87–123
Hatfield R, Fukushima RS (2005) Can lignin be accurately measured? Crop Sci 45:832–839
Hatton T, Ruprecht J, George R (2003) Preclearing hydrology of the Western Australia wheatbelt: target for the future. Plant Soil 257:341–356
Keeney DR, Nelson DW (1982) Nitrogen-inorganic forms. In: Page AL (ed) Methods of soil analysis. Part 2. Chemical and microbiological properties. Agronomy Monograph, Madison, WI, pp 643–698
Llamas PD, de Cara Gonzalez M, Iglesias Gonzalez C, Ruíz Lopez G, Tello Marquina J (2008) Effects of water potential on spore germination and viability of Fusarium species. J Ind Microbiol Biotechnol 35:1411–1418
Marschner P (2012) Marschner’s mineral nutrition of higher plants. Academic, Boston
Mavi MS, Marschner P, Chittleborough DJ, Cox JW, Sanderman J (2012) Salinity and sodicity affect soil respiration and dissolved organic matter dynamics differentially in soils varying in texture. Soil Biol Biochem 45:8–13
Nannipieri P, Giagnoni L, Renella G, Puglisi E, Ceccanti B, Masciandaro G, Fornasier F, Moscatelli M, Marinari S (2012) Soil enzymology: classical and molecular approaches. Biol Fertil Soils 48:743–762
Oren A (2001) The bioenergetic basis for the decrease in metabolic diversity at increasing salt concentrations: implications for the functioning of salt lake ecosystems. Hydrobiologia 466:61–72
Rayment G, Higginson FR (1992) Australian laboratory handbook of soil and water chemical methods. Inkata Press Pty Ltd, Melbourne
Rengasamy P (2006) World salinization with emphasis on Australia. J Exp Bot 57:1017–1023
Rietz D, Haynes R (2003) Effects of irrigation-induced salinity and sodicity on soil microbial activity. Soil Biol Biochem 35:845–854
Saxton K, Rawls WJ, Romberger J, Papendick R (1986) Estimating generalized soil-water characteristics from texture. Soil Sci Soc Am J 50:1031–1036
Setia R, Marschner P (2013) Carbon mineralization in saline soils as affected by residue composition and water potential. Biol Fertil Soils 49:71–77
Setia R, Marschner P, Baldock J, Chittleborough D (2010) Is CO2 evolution in saline soils affected by an osmotic effect and calcium carbonate? Biol Fertil Soils 46:781–792
Setia R, Marschner P, Baldock J, Chittleborough D, Verma V (2011a) Relationships between carbon dioxide emission and soil properties in salt-affected landscapes. Soil Biol Biochem 43:667–674
Setia R, Smith P, Marschner P, Baldock J, Chittleborough DJ, Smith J (2011b) Introducing a decomposition rate modifier in the Rothamsted carbon model to predict soil organic carbon stocks in saline soils. Environ Sci Technol 46:1624–1631
Shainberg I, Letey J (1984) Response of soils to sodic and saline conditions. Hilgardia, California 52:1–57
Shaw R, Hughes K, Thorburn P, Dowling (1987) A Principles of landscape, soil and water salinity—processes and management options. Part A. In: Landscape, soil and water salinity. Proceedings of the Brisbane Regional Salinity Workshop. Brisbane
Sinsabaugh RL (2010) Phenol oxidase, peroxidase and organic matter dynamics of soil. Soil Biol Biochem 42:391–404
Sumner ME, Naidu R (1998) Processes involved in sodic behavior. In: Rengasamy P, Sumner M (eds) Sodic soils—distribution, properties, management and environmental consequences, 1st edn. Oxford University Press, New York, pp 35–50
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 37:29–38
Warren CR (2013) High diversity of small organic N observed in soil water. Soil Biol Biochem 57:444–450
Wichern J, Wichern F, Joergensen RG (2006) Impact of salinity on soil microbial communities and the decomposition of maize in acidic soils. Geoderma 137:100–108
Wong V, Greene R, Dalal R, Murphy B (2010) Soil carbon dynamics in saline and sodic soils: a review. Soil Use Manag 26:2–11
Xu J, Tang C, Chen ZL (2006) Chemical composition controls residue decomposition in soils differing in initial pH. Soil Biol Biochem 38:544–552
Yan N, Marschner P (2012) Response of microbial activity and biomass to increasing salinity depends on the final salinity, not the original salinity. Soil Biol Biochem 53:50–55
Zarcinas BA, McLaughlin MJ, Smart MK (1996) The effect of acid digestion technique on the performance of nebulization systems used in inductively coupled plasma spectrometry. Commun Soil Sci Plant Anal 27:1331–1354
Acknowledgments
We thank the University of Adelaide for providing a postgraduate scholarship to H. Hasbullah.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Hasbullah, H., Marschner, P. Residue properties influence the impact of salinity on soil respiration. Biol Fertil Soils 51, 99–111 (2015). https://doi.org/10.1007/s00374-014-0955-2
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00374-014-0955-2