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(1967)
Objaśnienia techniczne do projektu melioracji użytków zielonych obiektu Rzeka Mała Solec [The description of technical Project of land reclamation of the grassland Mała river
(1990)
Podstawy regulowania uwilgotnienia gleb dolinowych [Principles of moisture management for shallow water table soils
(2012)
Analysing water level strategies
Filip Bujakowski, T. Falkowski, Grzegorz Wierzbicki, K. Żukowska (2014)
Using hydrodynamic modelling to assess the impact of the development on hydrogeological conditions in a polygenic river valley marginal zoneAnnals of Warsaw University of Life Sciences - SGGW. Land Reclamation, 46
E. Querner, P. Jansen, J. Akker, C. Kwakernaak (2012)
Analysing water level strategies to reduce soil subsidence in Dutch peat meadowsJournal of Hydrology
(2016)
2016: Zanikanie torfowisk [Peatlands disappearance]. Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk, Poznań
(1981)
Model matematyczny procesu podnoszenia się zwierciadła wody gruntowej przy nawodnieniu podsiąkowym [Mathematical model of rising of ground water level by subirri
(2017)
Wpływ procesów osiadania i zanikania
K. Lipka, E. Zajac, V. Hlotov, Z. Siejka (2017)
Disappearance rate of a peatland in Dublany near Lviv (Ukraine) drained in 19th century
(2007)
Charakterystyka hydrologiczna Chojnowskiego Parku Krajobrazowego [The hydrological characteristic of the Chojnowski Regional Park
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A. Brandyk (2011)
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(1967)
: Obja ś nienia techni - czne do projektu melioracji u ż ytków zie - lonych obiektu Rzeka Ma ł a Solec [ The description of technical Project of land reclamation of the grassland Ma ł a river site ]
(2018)
Słowa kluczowe: rzeka nizinna, regulacja rzek, systemy nawodnień podsiąkowych, gleby organiczne i mineralne MS
AbstractThis paper involves a comparative analysis of cross-sectional changes at selected reaches of a lowland river, flowing through the areas of mineral and organic soils. The comparisons were made at the background of design and execution assumptions from the period 1967–1971. Main processes, responsible for the observed changes of riverbeds in mineral soils (silting, conservation works) and organic soils (subsidence, disappearance of the peat deposit), were identified. In case of organic soils, the decrease of cross-sectional area by approximately from 30 to 60% was estimated in comparison to the original project assumptions, and the subsidence of river banks reached even 0.5 m in relation to the level determined in 1967. In the area of mineral soils, more considerable variability of cross-sectional area was noted along with minor changes of river banks elevation, that resulted most likely from the performed maintenance works.
Annals of Warsaw University of Life Sciences, Land Reclamation – de Gruyter
Published: Dec 1, 2018
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