09. Interaction of actual and admissible indexes of erosion-hydrological processes on a probable basis
https://doi.org/10.31073/agrovisnyk201908-09
Belolips'kyj V. O., Poluliah M. M.
Pages: 52-59.
Key words: basin, reservoir, hydropost, agrolandscape, soil, erosion, humus, criterion, expenditure of drainage, model.
Pages: 52-59.
Abstract
The purpose. To determine influence of interaction of actual and admissible indexes on development of erosion-hydrological processes with the purpose of their minimization on a probable basis. Methods. On laboratory-field, mathematical-statistical, topometric, morphological methods they studied erosion-hydrological situations on basin principle at different hierarchical levels (drainage basin natural boundary reservoir), interaction of actual and admissible indexes of erosion-hydrological processes. Results. By means of creation of hyper surfaces of response of combinations of components of agrolandscapes of reservoirs of basin of river Aydar and factors of formation of Qmax on hydroposts (Belolutsk, Kuriachovka, Starobelsk, Bakhmutovka) they analyzed interaction of actual and admissible indexes of erosion-hydrological processes on 1–50% level of probability. Such regularities were fixed: 1) at high plough up of reservoirs of Starobelsk and Bakhmut hydroposts (accordingly 65–75 and 70–80%) with use in ploughland of downslopes more than 18 — 40–55% expenditures of drainage of 10% probability are maximum (25–58 and 38–63 m3/s); 2) decrease of plough up of reservoirs of Kuriachovka hydropost up to 55–60% decrease the maximum expenditures of drainage of 10% probability up to 10–15 m3/s at use in ploughland of downslopes more than 1/ — 45–55% from reservoir; 3) high plough up of reservoir of Belolutsk hydropost (65–75%) are run a level by use in ploughland of slope lands more than 17 within the limits of 35–45% in formation of the maximum losses of drainage of 10% probability up to 16–36 m3/s. Such regularity of formation of the maximum losses of drainage is observed and at other probabilities of their development. Conclusions. Study of ratio of prognostic (admissible) and actual characteristics of combinations of components of agrolandscape (40–60% of ploughland, 35–40% of downslopes more than 1w, 0,3–0,5% of forest belts of cross arrangement on the background of humus 3,5–5,5% at the level of 10% probability of the maximum losses of drainage) testify to their objective effect and decrease of hydrological characteristics on 65–75% up to the level of low indexes of expenditures of drainage: 3–5 m3/s — Belolutsk, Kuriachovka, and 10–15 m3/s — Starobelsk, Bakhmutovka hydroposts.Key words: basin, reservoir, hydropost, agrolandscape, soil, erosion, humus, criterion, expenditure of drainage, model.
References
- Shvebs, G.I., Liseckij, F.N. (1989). Proektirovanie konturno-meliorativnoj sistemy pochvozashitnogo zemledeliya [Design of contour-reclamation system of soil conservation agriculture]. Agriculture, 2, 55-59. [in Russ.].
- Trifonova, T.A. (2005). Razvitie bassejnovogo podhoda v pochvennyh i ekologicheskih issledovaniyah [Development of basin approach in soil and ecological researches]. Soil science, 9, 32-39. [in Russ.].
- Wischmeier, W.H. Smith, D.D. (1978). Predicting Rainfall Erosion Losses. Agriculture Handbook, № 537. Washington, U.S. Departament of Agriculture.
- Van der Knijft, J.M., Jones, R.J.A., Montanarella, L. (2000). Soil erosion risk assessment in Europe. European Soil Bureau, 34, 8.
- Belolipskyi, V.O., Poluliakh, M.M., Druhov, O.N. (2016). Heoinformatsiina otsinka pryrodnoho potentsialu gruntiv baseinu r. Aidar [GIS assessment of natural potential of the soils of the basin of the river Aydar]. Bulletin of agricultural science. Special issue, Oct., 42-47. [in Ukr.].
- Belolipskyi, V.O., Baliuk, S.A., Poluliakh, M.M., Timchenko, D.O. (2018). Otsinka intensyvnosti eroziino-hidrolohichnykh sytuatsii za baseinovym pryntsypom (metodychni rekomendatsii ta analiz) [Assessment of the intensity of erosion-hydrological situations on the basin principle (guidelines and analysis)]. V.O. Belolipskyi (Ed.). Kharkiv. [in Ukr.].
- Bulygin, S.Yu. (2012). Pochvovodoohrannaya optimizaciya agrolandshaftov [Soil and water protection optimization of agrolandscapes]. Monograph. Kyiv: Agrarian science. [in Russ.].
- Tarariko, O.H., Hrekov, V.O., Panasenko, V.M. (2011). Okhorona ta vidnovlennia dehradovanykh gruntiv vidpovidno proektu Gruntovoi Dyrektyvy Yevrosoiuzu [Protection and restoration of degraded soils in accordance with the draft soil Directive of the European Union]. Bulletin of agricultural science, 5, 9-13. [in Ukr.].
- Kutsenko, M.V. (2012). Heosystemni osnovy rehuliuvannia eroziino-akumuliatyvnykh protsesiv: heomorfosystemnyi aspekt [Geosystem framework for the erosion and accumulation processes: geomorphically aspect]. Monograph. Kharkiv: KP «City printing house». [in Ukr.].
- Rehionalna prohrama okhorony rodiuchosti gruntiv na 2014–2020 rr. (2013). [Regional program of soil fertility protection for 2014-2020] Luhansk regional state administration, Department of agro-industrial development, Luhansk branch of the state institution «Institute of soil protection of Ukraine», Luhansk regional main Department of land resources of the State Committee of Ukraine on land resources, Luhansk state agricultural experimental station of the Institute of crop production V.Y. Yuryev. Luhansk. [in Ukr.].