RESEARCH PAPER
Fractions of nitrogen (including 15N) and also carbon in the soil as affected by different crop residues
More details
Hide details
1
Faculty of Bioengineering and Animal Husbandry, Siedlce University of Natural Sciences and Humanities, B. Prusa 14, 08-110 Siedlce, Poland
2
Institute of Agrophysics, Polish Academy of Sciences, Doświadczalna 4, 20-290 Lublin, Poland
3
Faculty of Agriculture and Biotechnology, Jan and Jędrzej Śniadecki University of Technology in Bydgoszcz, prof. S. Kaliskiego Ave. 7, 85-796 Bydgoszcz, Poland
4
Research Group - Stable Isotopes, Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa, Poland
Final revision date: 2023-05-19
Acceptance date: 2023-05-29
Publication date: 2023-08-16
Corresponding author
Anna Siczek
Department of Soil and Plant System, Institute of Agrophysics, Polish Academy of Sciences, Poland
Int. Agrophys. 2023, 37(3): 265-278
HIGHLIGHTS
- Transformation of N and C compounds from faba bean and wheat residues was studied
- Soil Ntot, total hydrolysable-N, humic-N were higher in faba bean than wheat rotation
- 15N mainly cumulate in easily hydrolysable fraction of SOM
- Soil chemical profile differs between faba bean and wheat rotation and sampling terms
- Soil with faba bean residues richer in N than with wheat what reduce N fertilization
KEYWORDS
TOPICS
ABSTRACT
Returning crop residue can increase soil organic matter content, and residue quality has an influence over the rate of their turnover. However, there is a lack of information concerning the biochemical transformations of organic compounds of N and C present in the crop residues during subsequent crop growth. In this study, the contents of organic N and C fractions in soils obtained using acid and alkaline hydrolysis under two crop rotations (faba bean vs. wheat rotation) were investigated. Black fallow served as a control. The mean total N increased in the order: black fallow, wheat rotation, faba bean rotation, total C and SOM were higher in the cropped soils than in black fallow. Hydrolysable-N (1-step acid hydrolysis) reached 83.7% total N, amino acid-N and threonine+serine-N were the highest in faba bean rotation and the lowest in black fallow, ammonia-N and aminosugar-N were lower in black fallow than in cropped soils. Hydrolysable-N (2-step sequential fractionation) reached 85.3% total N and significant differences were noted between the cropped soils and black fallow, with respect to both the N and C contents. 15N was mainly accumulated in the N soluble and easily hydrolysable N compounds, and these fractions were greater in cropped soils than in black fallow. N in the humic compounds increased from black fallow to faba bean rotation. A PCA analysis showed that crop rotation and soil sampling terms had a substantial influence over cluster formation. An ANOSIM test revealed significant differences between the crop rotation and term treatments. The results indicated that soil with faba bean rotation is richer in N compounds than soil with wheat as a forecrop and this may result in a reduction in N fertilizers for the succeeding crop.
FUNDING
This work was supported by the National Science Centre in Poland (project number 2016/21/B/NZ9/03588, 2017-2022).
CONFLICT OF INTEREST
The authors declare no conflict of interest.
REFERENCES (47)
1.
Alvarez-Puebla R.A., Valenzuela-Calahorro C., and Garrido J.J., 2006. Theoretical study on fulvic acid structure, conformation and aggregation. A molecular modelling approach. Sci. Total Environ., 358(1-3), 243-254.
https://doi.org/10.1016/j.scit....
2.
Becher M., 2013. Organic matter transformation degree in the soils of the upper Liwiec River (in Polish). Dissertation, Siedlce University of Natural Sciences and Humanities, Poland.
3.
Becher M. and Kalembasa D., 2011. Fraction of nitrogen and carbon in humus horizons of arable Luvisols and Cambisols located on Siedlce upland (in Polish). Acta Agrophysica, 18(1), 7-16.
4.
Becher M., Kalembasa D., Kalembasa S., Symanowicz B., Jaremko D., and Matyszczak A., 2023. A new method for sequential fractionation of nitrogen in drained organic (peat) Soils. Int. J. Environ. Res. Public Health, 20, 2367.
https://doi.org/10.3390/ijerph....
5.
Bird J.A., Herman D.J., and Firestone M.K., 2011. Rhizosphere priming of soil organic matter by bacterial groups in a grassland soil. Soil Biol. Biochem., 43(4), 718-725.
https://doi.org/10.1016/j.soil....
6.
Blair G.J., Lefroy R.D.B., and Lisle L., 1995. Soil carbon fractions based on their degree of oxidation, and the development of a carbon management index for agricultural systems. Aust. J. Agr. Res., 46(7), 1459-1466.
7.
Boddy E., Hill P.W., Farrar J., and Jones D.L., 2007. Fast turnover of low molecular weight components of the dissolved organic carbon pool of temperate grassland field soils. Soil Biol. Biochem., 39, 827-835.
8.
Bremner J.M., 1965. Organic forms of nitrogen. In: Methods of soil analysis (Ed. C.A. Black). American Society of Agronomy, Madison, USA.
9.
Bruun S., Ågren G.I., Christensen B.T., and Jensen L.S., 2010. Measuring and modeling continuous quality distributions of soil organic matter. Biogeosciences, 7, 27-41.
https://doi.org/10.5194/bg-7-2....
10.
Coleman K. and Jenkinson D.S., 1996. RothC-26.3 – A Model for the turnover of carbon in soil. In: Evaluation of Soil Organic Matter Models (Eds D.S. Powlson, P. Smith, J.U. Smith). NATO ASI Series (Series I: Global Environmental Change), Springer, Berlin, Heidelberg,
https://doi.org/10.1007/978-3-....
11.
Drosos M., Vinci G., Spaccini R., and Piccolo A., 2020. Molecular dynamics of organic matter in a tilled soil under short term wheat cultivation. Soil Till. Res., 196, 104448.
https://doi.org/10.1016/j.stil....
12.
Ellerbrock R.H. and Kaiser M., 2005. Stability and composition of different soluble soil organic matter fractions – evidence from δ13C and FTIR signatures. Geoderma, 128(1-2), 28-37.
14.
FAO, 2017. Soil Organic Carbon: the hidden potential. Food and Agriculture Organization of the United Nations. Rome, Italy.
15.
Greenfield L.G., Gregorich E.G., van Kessel C., Baldock J.A., Beare M.H., Billings S.A., Clinton P.W., Condron L.M., Hill S., Hopkins D.W., and Janzen H.H., 2013. Acid hydrolysis to define a biologically-resistant pool is compromised by carbon loss and transformation. Soil Biol. Biochem., 64, 122-126.
16.
Hayes M.H., McCarthy P., Malcolm R.L., and Swift R.S., 1989. Structures of humic substances: the emergence of forms. In: Humic Substance II: In Search of Structure: Setting the Scene (Eds M.H. Hayes, P. McCarthy, R.L. Malcolm, and R.S. Swift). John Wiley and Sons, New York, USA.
17.
Hayes M.H.B., Mylotte R., and Swift R.S., 2017. Humin: its composition and importance in soil organic matter. Adv. Agron., 143, 47-138.
18.
Hayes M.H.B. and Swift R.S., 2020. Vindication of humic substances as a key component of organic matter in soil and water. Adv. Agron., 163, 1-37.
https://doi.org/10.1016/bs.agr....
19.
Haynes R.J., 2005. Labile organic matter fractions as central components of the quality of agricultural soils: An overview. Adv. Agron., 85, 221-268.
https://doi.org/10.1016/S0065-....
21.
Huygens D., Boeckx P., Templer P., Paulino L., Van Cleemput O., Oyarzún C., Müller C., and Godoy R., 2008. Mechanisms for retention of bioavailable nitrogen in volcanic rainforest soils. Nature Geosci., 1, 543-548.
https://doi.org/10.1038/ngeo25....
22.
Jackson O., Quilliam R.S., Stott A., Grant H., and Subke J.-A., 2019. Rhizosphere carbon supply accelerates soil organic matter decomposition in the presence of fresh organic substrates. Plant Soil, 440, 473-490.
https://doi.org/10.1007/s11104....
23.
Kalembasa S., 1991. Quick method of determination of organic carbon in soil. Polish J. Soil Sci., 24(1), 17-22.
24.
Kalembasa S., 1995. Application of 15N and 13N isotopes in soil science and agriculture chemistry research (in Polish). WNT, Warsaw, Poland.
25.
Kalembasa S. and Kalembasa D., 2016. Conversions and pathways of organic carbon and organic nitrogen in soils. In: Bioactive Compounds in Agricultural Soils (Ed. L. Szajdak). Springer, Cham.,
https://doi.org/10.1007/978-3-....
26.
Kayler Z.E., Kaiser M., Gessler A., Ellerbrock R.H., and Sommer M., 2011. Application of δ13C and δ15N isotopic signatures of organic matter fractions sequentially separated from adjacent arable and forest soils to identify carbon stabilization mechanisms. Biogeosciences, 8, 2895-2906.
27.
King A.E., Ali G.A., Gillespie A.W., and Wagner-Riddle C., 2020. Soil organic matter as catalyst of crop resource capture. Front. Environ. Sci., 8:50.
https://doi.org/10.3389/fenvs.....
28.
Kumar A. and Sharma M., 2014. Review of methodology for estimation of labile organic carbon in reservoirs and lakes for GHG Emission. J. Mater. Environ. Sci., 5(3), 653-660.
29.
Leavitt S.W., Follett R.F., and Paul E.A., 1996. Estimation of slow- and fast-cycling soil organic carbon pools from 6N HCl hydrolysis. Radiocarbon, 38(2), 231-239.
30.
Man M., Wagner-Riddle C., Dunfield K.E., Deen B., and Simpson M.J., 2021. Long-term crop rotation and different tillage practices alter soil organic matter composition and degradation. Soil Till. Res., 209, 104960.
https://doi.org/10.1016/j.stil....
31.
Meier U., 2001. Growth stages of mono- and dicotyledonous plants. BBCH Monograph, Federal Biological Research Centre for Agriculture and Forestry, Bonn, Germany.
32.
Mwafulirwa L.D., Baggs E.M., Russell J., Morley N., Sim A., and Paterson E., 2017. Combined effects of rhizodeposit C and crop residues on SOM priming, residue mineralization and N supply in soil. Soil Biol. Biochem., 113, 35-44.
https://doi.org/10.1016/j.soil....
33.
Owen A.G. and Jones D.L., 2001. Competition for amino acids between wheat roots and rhizosphere microorganisms and the role of amino acids in plant N acquisition. Soil Biol. Biochem., 33, 651-657.
34.
Paul E.A., Morris S.J., Conant R.T., and Plante A.F., 2006. Does the acid hydrolysis-incubation method measure meaningful soil organic carbon pools? Soil Sci. Soc. Am. J., 70, 1023-1035.
35.
Paul E.A., Follett R.F., Haddix M., and Pruessner E., 2011. Soil N dynamics related to soil C and microbial changes during long-term incubation. Soil Sci., 176(10), 527-536.
https://doi.org/10.1097/SS.0b0....
36.
Roberts P. and Jones D.L., 2008. Critical evaluation of methods for determining total protein in soil solution. Soil Biol. Biochem., 40(6), 1485-1495.
https://doi.org/10.1016/j.soil....
38.
Schulten H.R. and Schnitzer M., 1992. Structural studies on soil humic acids by Curie-point pyrolysis-gas chromatography/mass spectrometry. Soil Sci., 153, 205-224.
39.
Shirato Y. and Yokozawa M., 2006. Acid hydrolysis to partition plant material into decomposable and resistant fractions for use in the Rothamsted carbon model. Soil Biol. Biochem., 38(4), 812-816.
https://doi.org/10.1016/j.soil....
40.
Sollins P., Kramer M.G., Swanston C., Lajtha K., Filley T., Aufdenkampe A.K., Wagai R., and Bowden R.D., 2009. Sequential density fractionation across soils of contrasting mineralogy: evidence for both microbial- and mineral-controlled soil organic matter stabilization. Biogeochemistry, 96, 209-231. doi:10.1007/s10533-009-9359-z.
41.
Solomon D., Fritzsche F., Lehmann J., Tekalign M., and Zech W., 2002. Soil organic matter dynamics in the subhumid agroecosystems of the Ethiopian Highlands: evidence from natural 13C abundance and particle-size fractionation. Soil Sci. Soc. Am. J., 66, 969-978.
42.
Stevenson F.J., 1982. Organic forms of soil nitrogen. In: Nitrogen in agriculture soil (Ed. F.J. Stevenson). Madison: ASA-CSSA-SSSA, USA.
43.
Stevenson F.J., 1994. Humus Chemistry: Genesis, Composition, Reactions. 2nd Edition, Wiley, New York, USA.
44.
Tate K.R., 2017. Microbial biomass: a paradigm shift in terrestrial biogeochemistry. Singapore, World Scientific Publishing Company.
45.
Wick A.F., Ingram L.J., and Stahl P.D., 2009. Aggregate and organic matter dynamics in reclaimed soils as indicated by stable carbon isotopes. Soil Biol. Biochem., 41, 201-209.
46.
World Reference Base, 2014. World Reference Base for Soil Resources International Soil Classification System for Naming Soils and Creating Legends for Soil Maps. World Soil Resources Reports No. 106. update 2015, Rome: FAO.
47.
Yang S., Jansen B., Absalah S., Kalbitz K., Chunga Castro F.O., and Cammeraat E.L.H., 2022. Soil organic carbon content and mineralization controlled by the composition, origin and molecular diversity of organic matter: A study in tropical alpine grasslands. Soil Till. Res., 215, 105203,
https://doi.org/10.1016/j.stil....