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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.7868/S0435428118030082</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-1377</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Современный тренд эрозионно-аккумулятивных процессов в малом распаханном водосборе, Республика Татарстан</article-title><trans-title-group xml:lang="en"><trans-title>Assessment of contemporary erosion/sedimentation trend  within a small cultivated catchment in the Republic of Tatarstan (European Russia)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шарифуллин</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Sharifullin</surname><given-names>A. G.</given-names></name></name-alternatives><email xlink:type="simple">AGSharifullin@kpfu.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Гусаров</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Gusarov</surname><given-names>A. V.</given-names></name></name-alternatives><email xlink:type="simple">avgusarov@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Голосов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Golosov</surname><given-names>V. N.</given-names></name></name-alternatives><email xlink:type="simple">gollossov@gmail.com</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Казанский (Приволжский) федеральный университет, Казань</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kazan Federal University, Kazan</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Казанский (Приволжский) федеральный университет, Казань; Московский государственный университет имени М.В. Ломоносова, географический факультет, Москва</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kazan Federal University, Kazan; Lomonosov Moscow State University, Faculty of Geography, Moscow</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>22</day><month>09</month><year>2018</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>93</fpage><lpage>108</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Шарифуллин А.Г., Гусаров А.В., Голосов В.Н., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Шарифуллин А.Г., Гусаров А.В., Голосов В.Н.</copyright-holder><copyright-holder xml:lang="en">Sharifullin A.G., Gusarov A.V., Golosov V.N.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/1377">https://geomorphology.igras.ru/jour/article/view/1377</self-uri><abstract><p>Анализ аккумуляции наносов в днищах долин первого порядка позволяет дать достаточно надежную количественную оценку общей интенсивности и временнóй изменчивости эрозионных процессов на сельскохозяйственных землях, подходящих практически вплотную к этим долинам. С использованием радиоактивного цезия-137 в качестве хрономаркера, а также усовершенствованных эрозионных моделей USLE и Государственного гидрологического института, изучение аккумулированных наносов в днище малой долины “Темева речка” (площадь водосбора – 1.13 км2 ), расположенной в северо-западной части Республики Татарстан (бассейн р. Мёша), показало заметное снижение темпов смыва почв с пахотной части водосбора за последние десятилетия. Так, если за период 1963–1986 гг. темпы аккумуляции в днище малой долины смытого со склонов водосбора почвенного материала составляли 0.92–1.81 см/год, то за период 1987–2015 гг. – 0.17–0.50 см/год, т.е. сократились как минимум в 3–5 раз. Причиной отмеченного уменьшения темпов смыва почв и аккумуляции наносов явилось сокращение объемов поверхностного стока со склонов в период снеготаяния, вызванное повышением температуры воздуха в весеннее время года, уменьшением глубины промерзания почв и снижением частоты выпадения экстремальных ливней со слоем 40–50 мм. Влияние хозяйственной деятельности на уменьшение темпов эрозионно-аккумулятивных процессов было, по всей видимости, несущественным, хотя некоторое изменение севооборотов с увеличением доли многолетних трав, очевидно, повлияло на снижение темпов смыва в теплое время года. Данная эрозионная тенденция и климатические причины, ее обусловившие, имели региональный характер и ранее выявлены в ряде регионов южной половины Европейской территории России.</p></abstract><trans-abstract xml:lang="en"><p>An analysis of sedimentation at first-order-valley bottoms allows the gathering of a sufficiently reliable quantitative evaluation of soil losses from a catchment area for two time intervals (1963–1986 and 1987–2015) and its temporal variability. The catchment studied (Temeva Rechka, 1.13 km2) is located in the River Myósha basin, the northwestern part of the Republic of Tatarstan, Russia. Combination of methods and approaches was used for estimation of sediment redistribution for the both time intervals, including detail geodetic survey of main morphological units of the catchment dry valley, large scale geomorphological mapping, caesium-137 technique for sediment dating in typical locations of the valley bottom, calculation of soil losses using modi fied version of USLE and State Hydrological Institute (Russia) models. In addition, available information about dynamics of some climate characteristics for the period 1950–2015 was collected from regional weather stations. LandSat images were applied for evaluation of possible land use changes. Crop management coefficients were calculated separately for the rainfall and snow-melt periods using available data about crop-rotation dynamics for the last 55 years. A significant decrease of average annual soil losses from the cultivated part of the Temeva Rechka catchment was found for the period 1987–2015 compared to the period 1963–1986. Such conclusion was mainly based on different sedimentation rates in the valley bottom: for the period of 1963–1986 the average sedimentation rates were 0.92–1.81 cm per year, while for the period of 1987–2015 these rates were only 0.17–0.50 cm per year. The main reason for this significant decrease was the reduction of surface runoff caused by climate warming in the region. The warming led to a reduction of soils freezing depth before the snow-melt period, and to a decline in frequency of extreme (rainstorm) precipitation (40–50 mm per a rainstorm). The influence of agricultural activity on the erosion and sedimentation rates changeabi lity was insignificant, although some regional variation of crop rotation including a increase in proportion of perennial grasses obviously caused a decline in soil losses during warm period of year. The same trend of erosion/sedimentation rates due to mostly climate changes was identified in some regions of the European Russiaʼs southern half.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>эрозия</kwd><kwd>наносы</kwd><kwd>цезий-137</kwd><kwd>балка</kwd><kwd>водосбор</kwd><kwd>изменения климата</kwd><kwd>промерзание почвы</kwd><kwd>талый сток</kwd><kwd>пашня</kwd><kwd>лесостепь</kwd><kwd>Русская равнина</kwd></kwd-group><kwd-group xml:lang="en"><kwd>erosion</kwd><kwd>sediment</kwd><kwd>caesium-137</kwd><kwd>dry valley</kwd><kwd>catchment</kwd><kwd>climate change</kwd><kwd>soil freezing</kwd><kwd>snowmelt runoff</kwd><kwd>cultivated</kwd><kwd>land</kwd><kwd>forest-steppe</kwd><kwd>Russian Plain</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">РНФ (проект  15-17-20006).</funding-statement><funding-statement xml:lang="en">The study was funded by the Russian Science Foundation according to  the research project No. 15-17-20006.</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Голосов В.Н., Острова И.В., Силантьев А.Н., Шкуратова И.Г. 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