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<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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 custom-type="elpub" pub-id-type="custom">geomorf-2008</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>О современном росте оврагов Таджикистана</article-title><trans-title-group xml:lang="en"><trans-title>On recent growth of gullies at Tadjikistan</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>Ахматов</surname><given-names>Х. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Akhmadov</surname><given-names>H. M.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Научно-исследовательский институт почвоведения МСХ Таджикской ССР</institution><country>Tajikistan</country></aff><pub-date pub-type="collection"><year>1979</year></pub-date><pub-date pub-type="epub"><day>20</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>51</fpage><lpage>55</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ахматов Х.М., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Ахматов Х.М.</copyright-holder><copyright-holder xml:lang="en">Akhmadov H.M.</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/2008">https://geomorphology.igras.ru/jour/article/view/2008</self-uri><abstract><p>Field studies and cartographic analysis allowed compiling a schematic map showing intensity of gullies' growth at Tadjikistan and recent state of gully erosion. The author outlined seven sites of most intensive gully erosion. Maximum values registered of gully growth are 82,5 m under undisturbed vegetation and 674,7 m per year at irrigated lands. Intensity of gullies' growth under natural conditions has been proved to follow vertical zonality, maximum value of the growth is registered at middle mountain zone, at irrigated lands most intensive growth is at valleys. Quantitative data are given for individual years and regions.</p></abstract><trans-abstract xml:lang="en"><p>Field studies and cartographic analysis allowed compiling a schematic map showing intensity of gullies' growth at Tadjikistan and recent state of gully erosion. The author outlined seven sites of most intensive gully erosion. Maximum values registered of gully growth are 82,5 m under undisturbed vegetation and 674,7 m per year at irrigated lands. Intensity of gullies' growth under natural conditions has been proved to follow vertical zonality, maximum value of the growth is registered at middle mountain zone, at irrigated lands most intensive growth is at valleys. Quantitative data are given for individual years and regions.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
