geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-179710.31857/S0435428120010034geomorf-1458Research ArticleМетодика научных исследованийScientific Research MethodsИспользование аэрофотосъемки и воздушного лазерного сканирования для выявления динамики экзогенных процессов как базы для оценки опасностиThe Use of Aerial Photography and Airborne Laser Scanning to Identify the Dynamics of Exogenic Processes as a Basis for Hazard AssessmentАрхиповаМ. В.ArkhipovaM. V.

Москва

Moscow

ВикторовА. С.VictorovA. S.

Москва

Moscow

ОрловТ. В.OrlovT. V.

Москва

Moscow

tim.orlov@gmail.comКазеевА. И.KazeevA. I.

Москва

Moscow

КапраловаВ. Н.KapralovaV. N.

Москва

Moscow

ТрапезниковаО. Н.TrapeznikovaO. N.

Москва

Moscow

Институт геоэкологии имени Е.М. Сергеева РАНРоссияSergeyev Institute of Geoecology RASRussian Federation20203006202001Геоморфология3448Copyright © Архипова М.В., Викторов А.С., Орлов Т.В., Казеев А.И., Капралова В.Н., Трапезникова О.Н., 20202020Архипова М.В., Викторов А.С., Орлов Т.В., Казеев А.И., Капралова В.Н., Трапезникова О.Н.Arkhipova M.V., Victorov A.S., Orlov T.V., Kazeev A.I., Kapralova V.N., Trapeznikova O.N.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/1458

Для участка трубопровода с активным развитием экзогенных геологических процессов (ЭГП) – оползней, эрозии и термокарста – определена их динамика на основе повторного лазерного сканирования. Участки развития ЭГП выявлены по материалам аэрофотосъемки и полевых работ. Проведено сравнение лазерного сканирования 2010 и 2011 гг. Определены изменения рельефа и объемы смещения грунтовых масс в результате развития ЭГП в полосе строительства трубопровода. Наиболее значительными являются изменения рельефа в пределах оползневого участка, также большие изменения отмечаются на участках прямых техногенных воздействий. Менее сильные изменения фиксируются в зонах сноса и накопления материала на оползневом участке; на участках развития эрозионных процессов и по периферии очагов термокарста отмечены понижения отметок высот. Было выявлено смещение материала с понижением высотных отметок в размере 3827 м3 и с повышением высотных отметок – 1890 м3.

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Using repeated laser scanning, we analyzed the dynamics of exogenic geological processes (EGP) such as landslides, fluvial erosion, and thermokarst, for a pipeline section with a high concentration of these hazards. Air-borne imagery and field works were involved in detecting foci of the EPG. We compared laser scanning data from 2010 to 2011 and estimated topography changes resulted from the geological hazard activity in the pipeline vicinity. Variations of the topography at the landslide area were the greatest as well as those at the section with intense industrial activity. Fewer changes were found in the zones of removal and accumulation of material within the landslide area. We also detected a decrease of height marks in the areas of fluvial erosion and thermokarst sinks peripheries. In particular, the removal of 3827 m3 of material in the upper part of the test area resulted to noticeable lowering of the surface, and accumulation of 1890 m3 of material caused the rise of surface height.

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The authors declare that there are no conflicts of interest present.