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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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.7868/S2073667320010049</article-id><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-6</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>ГИДРООПТИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>HYDROOPTICS</subject></subj-group></article-categories><title-group><article-title>Оценка влияния взвеси на спектральный показатель ослабления света в Телецком озере (Перевод на англ. яз.: Е.С. Кочеткова)</article-title><trans-title-group xml:lang="en"><trans-title>Evaluation of suspended matter effect on spectral light attenuation in Lake Teletskoye</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>Акулова</surname><given-names>О. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Akulova</surname><given-names>О. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Барнаул</p></bio><bio xml:lang="en"><p>Barnaul</p></bio><email xlink:type="simple">akulova8282@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>Букатый</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Bukatyi</surname><given-names>V. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Барнаул</p></bio><bio xml:lang="en"><p>Barnaul</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт водных и экологических проблем СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for Water and Environmental Problems, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>28</day><month>11</month><year>2021</year></pub-date><volume>13</volume><issue>1</issue><fpage>35</fpage><lpage>44</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Акулова О.Б., Букатый В.И., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Акулова О.Б., Букатый В.И.</copyright-holder><copyright-holder xml:lang="en">Akulova О.B., Bukatyi V.I.</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://hydrophysics.spbrc.ru/jour/article/view/6">https://hydrophysics.spbrc.ru/jour/article/view/6</self-uri><abstract><p>Представлены результаты измерений спектрального показателя ослабления света в диапазоне 400–800 нм по акватории Телецкого озера, полученные в ходе летней экспедиции (19–23 июня 2018 г.). В исследуемый период значения показателя ослабления (при натуральном основании логарифма) в различных точках отбора проб варьировались в пределах 0.2–4.4 м–1 в вышеуказанном спектральном диапазоне длин волн.Для оценки влияния взвеси на суммарный показатель ослабления рассчитан её относительный спектральный вклад, а также других основных оптически активных компонентов озёрной воды — жёлтого вещества, хлорофилла «а» и чистой воды. Спектральный вклад взвеси в показатель ослабления света на длине волны 430 нм находился в пределах 2.3–33.4 %, на длине волны 550 нм — 5.9–47.8 %. Для определения гранулометрического состава и счётной концентрации частиц взвеси использован метод оптической микроскопии. По данным измерений средневзвешенные радиусы частиц в пробах воды с поверхностного слоя озера находились преимущественно в интервале 0.5–0.8 мкм, концентрации — от 0.9∙106 см–3 до 3.3∙106 см–3. Распределения частиц по размерам аппроксимировались функцией Юнге с коэффициентом детерминации от 0.63 до 0.99.</p></abstract><trans-abstract xml:lang="en"><p>This study presents the results of the light attenuation coefficient measurements in the range of 400–800 nm in the waters of Lake Teletskoye, obtained in a summer cruise (19–23 June 2018). During the cruise in various locations, the attenuation coefficient values varied (to the base of natural logarithm) in the range of 0.2–4.4 m–1 within the stated wavelength range.The relative spectral effect of the suspended matter was calculated along with the other major optically active components of the lake water: yellow matter, chlorophyll-a and pure water to assess the contribution of suspension to the total attenuation coefficient. Suspended matter spectral contribution to light attenuation at 430 nm wavelength appeared in the range of 2.3–33.4 %, and at 550 nm — 5.9–47.8 %. Optical microscopy was used to determine the particle size distribution and the number concentration of suspended particles. According to the measurements, weight-average particle radii in the water samples varied primarily within the range 0.5–0.8 µm, while the concentrations differed from 0.9∙106cm–3 to 3.3∙106cm–3. Particle size distribution was approximated by the Junge function with a determination coefficient from 0.63 to 0.99.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>метод оптической микроскопии</kwd><kwd>спектральный показатель ослабления света</kwd><kwd>счётная концентрация взвеси</kwd><kwd>радиус частиц</kwd><kwd>распределение частиц по размерам</kwd><kwd>гранулометрический состав</kwd><kwd>функция Юнге</kwd><kwd>Телецкое озеро</kwd></kwd-group><kwd-group xml:lang="en"><kwd>method of optical microscopy</kwd><kwd>spectral light attenuation</kwd><kwd>suspended matter concentration</kwd><kwd>particle radius</kwd><kwd>particle size distribution</kwd><kwd>Junge function</kwd><kwd>Lake Teletskoye</kwd></kwd-group><funding-group><funding-statement xml:lang="en">This work was carried out as part of the state assignment of the IWEP SB RAS (project registration number AAAA-A17–117041210241–4).</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">Маньковский В.И., Шерстянкин П.П. 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