2018
DOI: 10.1088/1755-1315/107/1/012016
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Trends of the gully erosion development in the territory of the Republic of Tatarstan

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Cited by 7 publications
(7 citation statements)
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“…Finally, mention should be made that the above-mentioned hydrological (a reduction in spring snowmelt-induced discharge) and sheet/rill/gully erosion intensity changes (a decrease in annual river load/yield) in the basins of the main studied plain rivers of the Ciscaucasia (the Kalaus River and the Kuma River), in river basins of the central part of the northern slope of the Greater Caucasus (the upper Terek River basin) and possibly the lowland part of the Kuban River basin, were similar in their common features to those previously described in many regions of the neighboring East European Plain [13][14][15][16][17][19][20][21]23,25,[27][28][29]71,73,83,84], in the Baltic countries (Estonia, Latvia, and Lithuania) [85], as well as in Eastern Scandinavia [86], Poland, Belarus, and in the north of Ukraine [87]. That is, it was a sizeable regional phenomenon for Eastern and Central Europe.…”
Section: Comparison With Neighboring Regions Of Europementioning
confidence: 65%
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“…Finally, mention should be made that the above-mentioned hydrological (a reduction in spring snowmelt-induced discharge) and sheet/rill/gully erosion intensity changes (a decrease in annual river load/yield) in the basins of the main studied plain rivers of the Ciscaucasia (the Kalaus River and the Kuma River), in river basins of the central part of the northern slope of the Greater Caucasus (the upper Terek River basin) and possibly the lowland part of the Kuban River basin, were similar in their common features to those previously described in many regions of the neighboring East European Plain [13][14][15][16][17][19][20][21]23,25,[27][28][29]71,73,83,84], in the Baltic countries (Estonia, Latvia, and Lithuania) [85], as well as in Eastern Scandinavia [86], Poland, Belarus, and in the north of Ukraine [87]. That is, it was a sizeable regional phenomenon for Eastern and Central Europe.…”
Section: Comparison With Neighboring Regions Of Europementioning
confidence: 65%
“…For instance, tendencies towards a decrease in the intensity of sheet/rill/gully erosion processes, the accumulation of their products, and also a reduction in river sediment load/concentration have been found over the last decades in many administrative regions and river basins of the forest-steppe and steppe zones of European Russia characterized by a relatively high degree of agricultural development. All of this was possible by using various approaches and methods, such as modeling [17,18], analysis of hydrological (suspended sediment load) data [19][20][21], stationary studies [22], field and remote monitoring [23][24][25], field research based on a variety of chronomarkers [26][27][28][29], and so on. Despite these and other numerous results, many of European Russia's regions are still "blank spots" regarding this field of research.…”
Section: Introduction 1problem Formulationmentioning
confidence: 99%
“…Therefore, if during 1963-1986 the average rates of dry-valley bottom sedimentation of washed-out soil material, using radiocesium as a chronomarker for sediment dating, were 0.92-1.81 cm per annum, then during 1987-2015 they were only 0.17-0.50 cm per annum, i.e., they reduced by at least 72-81%. It is noteworthy that in this part of the Republic of Tatarstan, where the basins of these rivers are located, almost 60% of the studied gullies almost completely stopped linear growth from 1960-1970 to 2009-2016 [77].…”
Section: Forest-steppe Zonementioning
confidence: 86%
“…ing 1987-2015 they were only 0.17-0.50 cm per annum, i.e., they reduced by at least 72-81%. It is noteworthy that in this part of the Republic of Tatarstan, where the basins of these rivers are located, almost 60% of the studied gullies almost completely stopped linear growth from 1960-1970 to 2009-2016 [77].…”
Section: Forest-steppe Zonementioning
confidence: 86%
“…Verkhneuslonsky municipal district of the Republic of Tatarstan (map-scheme) shows fragments of a map of the expositions and slopes of the relief of the Verkhneuslonsky district. The watershed faces the Volga valley with high steep slopes with angles of up to 65 degrees[7]. The plakar surfaces and the water surface of the Kuibyshev reservoir correspond to zero slope values.…”
mentioning
confidence: 99%