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- W220484542 abstract "Gully formation is a serious problem in crop production, landscape management and freshwater eutrophication. A recent spectacular example, the Somogybabod gully came into being in the early summer of 2010 after an extremely wet spring. Usually a very rapid process, especially on loess, gully development in this case was supported by improper land use, catchment management and previous piping. Piping and tunnel formation take place invisibly underground. When tunnel roofs collapse, rather deep gullies are exposed within few minutes—as it happened at Somogybabod. Although several active permanent and ephemeral gullies are found in the surroundings, only the Somogybabod gully attracted the attention of scientists because it was initiated under forest cover and, threatening houses, was also highlighted by the media. The aroused public interest could provide an opportunity to face and solve the problem. Instead of runoff mitigation, however, only the filling up of the gully was considered—no long-term solution without the control of surface hydrology and field-scale complex amelioration." @default.
- W220484542 created "2016-06-24" @default.
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- W220484542 date "2015-01-01" @default.
- W220484542 modified "2023-09-24" @default.
- W220484542 title "The Somogybabod Gully: Hidden Erosion (Piping) in the Somogy Hills" @default.
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- W220484542 doi "https://doi.org/10.1007/978-3-319-08997-3_12" @default.
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