10. Carbon-nitric turnover in agrocnoses of crop rotations
https://doi.org/10.31073/agrovisnyk201809-10
Demydenko O. V., Shapoval I. S., Bojko P. I., Velychko V. A.
Pages: 64-72.
Full article:
Key words: balance of organic carbon, capacity of balance, productivity, different crop rotations, correlation, factorial analysis.
Pages: 64-72.
Full article:
Abstract
The purpose. To determine normative parameters of typification of balance and content of organic carbon Corg in agrocnoses of different crop rotations, as components of methodology of agroecological assessment of their productivity at use of collateral production as organic fertilizers in conditions of modern climatic system of Forest-steppe of Ukraine. Methods. Generalization of results of long-term researches in field stationary experiment, statistical: dispersive, correlation, factorial, claster analysis of parameters of productivity, qualitative and quantitative clauses of balance of nitrogen, carbon. Results. At full leaving of collateral production in 7 – 10-field crop rotations balance of Corg was positive, and the maximal productivity coincided with high values of balance (+1,32 – 2,54 t/hectare) and capacity of balance (3,17 – 3,72 t/hectare). In 3 – 5-field crop rotations balance of Corg was less profitable (+0,56 – + 0,87 t/hectare), but also capacity of balance of Corg increased at the maximal productivity up to 4,01 – 4,12 t/ hectare. Direct correlation is fixed between capacity of balance of Corg and productivity of crop rotations. With growth of productivity of crop rotations proportionally grows both mineralization, and humufication of Corg. Capacity of balance in short crop rotations on the maximal parameters exceeds 4 t/hectare whereas at 7 – 10-field crop rotations the maximal value of capacity of balance is less 4 t/hectare. Conclusions. Ratio Corg to nitrogen in agrocnoses, irrespective of type of crop rotations, is in optimum limits (20 – 30:1), that creates optimum conditions for humifacation of collateral production and formation of humus. It is confirmed by balance calculations of nitrogen and organic carbon.Key words: balance of organic carbon, capacity of balance, productivity, different crop rotations, correlation, factorial analysis.
References
- Bazilevich N.I., Titljanova A.A. (2008). Bioticheskij krugovorot na pjati kontinentah: azot i zol'nye jelementy v prirodnyh nazemnyh jekosistemah. [Biotic cycle on five continents: nitrogen and ash elements in natural terrestrial ecosystems]. Novosibirsk: Izdv. SB RAS. 381 p. [in Russian].
- Golubyatnikov L.L., Mohov I.I., Yeliseyev A.V. (2013). Cikl azota v zemnoj klimaticheskoj sisteme. [Nitrogen cycle in the terrestrial climatic system]. Izvestiya RAS. Physics of the atmosphere and the ocean., Cikl azota v zemnoj klimaticheskoj sisteme. Vol. 49, No. 3. P. 255-270. [in Russian].
- Moiseev N.N., Aleksandrov V.V., Tarko A.M. (1985). Chelovek i biosfera. Opyt sistemnogo analiza i jeksperimenty s modeljami. [Man and the biosphere. Experience in system analysis and experiment with models]. Moskva: Nauka,. 272 p. [in Russian].
- Thornton P.E., Doney S.C., Lindsay K. et al. (2009). Carbonnitrogen interactions regulate the climate-carbon cycle feedbacks: results from an atmospheric general circulation model. Biogeosciences. V. 6. P. 2099-2120.
- Vitousek P.M., Howarth R.W. (1991). Nitrogen limitation on land and in the sea: How can it occur? Biogeochemistry. V. 13. P. 87-115.
- Krapivin V.F., Svirzev Yu.M., Tarko A.M. (1982). Matematicheskoe modelirovanie global'nyh biosfernyh processov. [Mathematical modeling of global biosphere processes]. Moskva: Nauka. 272 p. [in Russian].
- Friedlingstein P., Cox P., Betts R.A. et al (2006). Climate_carbon cycle feedback analysis: Results from the C4MIP model intercomparison. J. Climate. V 19. No. 22. P. 3337-3353.
- Canadell J.G., Pataki D.E., Gifford R. et al. (Canadell J.G., Pataki D.E., Pitelka L. Eds.) (2007). Saturation of theterrestrial carbon sink. Terrestrial ecosystems in a changing world. The IGBP Series. V. XXIV. N.Y .: Springer_Verlag. 59-73.
- Sabine C.L., Heimann M., Artaxo P. et al. (Field C.B., Raupach M.R. Eds.) (2004). Current statusand trends in global carbon cycle. SCOPE 62: The global carbon cycle. London: Island Press. P. 17-44.
- Kapshtyk M.V., Demydenco O.V. (2014). The ways to ecologically balanced development of agro ecosystems in the Forest-steppe zone of Ukraine. International Journal of Agricultural Research and Review: ISSN-2360-7971: Vol. 2 (8): P. 092-098, August.
- Denman K.L., Brasseur G., Chidthaisong A. et al. (Solomon S., Qin D., Manning M. et al. Eds.). (2007). Couplings between changes in the climate system and bio_geochemistry. Climate Change 2007: The Physical Science Basis. Cambridge: Cambridge Univ. Press. P. 499-588.
- Chimitdorzhieva E.O. (2011). Zapasy ugleroda v chernozjomah i kashtanovyh pochvah Zabajkal'ja i jemisija SO2. [Carbon stocks in chernozems and chestnut soils Transbaikalia and the emission of CO2]. Abstract diss. Cand. biol. sciences - Ulan-Ude. 21 p. [in Russian].
- Cox P.M., Betts R.A., Jones C.D. et al (Pearce R. Ed.). (2001). Modeling the vege_tation and the carbon cycle as interactive elements of the climate system. Meteorology at the millennium. N.Y.: Academic Press. P. 259-279.
- Blagodatsky S.A., Larionova A.A., Evdokimov I.V. (1992). Dejstvie mineral'nyh soedinenij azota na intensivnost' dyhanija i jeffektivnost' rosta mikroorganizmov v pochve. Pochvovedenie. [Effect of mineral compounds of nitrogen on the intensity of respiration and the efficiency of growth of microorganisms in soil]. Pochvovedenie. No. 9. P. 88-96. [in Russian].
- Zaehle S. Dalmonech D. (2011). Carbon_nitrogen interactions on global global scales: current understanding in the modeling climate biosphere feedbacks. Curr. Opin Environ Sustain. V. 3. P. 311-320.