Aleksey Sidorchuk

ORCID: 0000-0002-6750-5463
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About
Contact & Profiles
Research Areas
  • Soil erosion and sediment transport
  • Hydrology and Sediment Transport Processes
  • Geology and Paleoclimatology Research
  • Marine and environmental studies
  • Hydrology and Watershed Management Studies
  • Soil and Environmental Studies
  • Climate change and permafrost
  • Aeolian processes and effects
  • Geological Studies and Exploration
  • Landslides and related hazards
  • Geological formations and processes
  • Aquatic and Environmental Studies
  • Water Resources and Management
  • Ancient and Medieval Archaeology Studies
  • Spacecraft Design and Technology
  • Archaeology and ancient environmental studies
  • Flood Risk Assessment and Management
  • Cryospheric studies and observations
  • Historical and Archaeological Studies
  • Methane Hydrates and Related Phenomena
  • Soil and Unsaturated Flow
  • Dam Engineering and Safety
  • Ecology and biodiversity studies
  • Plant Surface Properties and Treatments
  • Tree-ring climate responses

Lomonosov Moscow State University
2008-2024

Moscow State University
2006-2024

Novosibirsk State University
2018

Manaaki Whenua – Landcare Research
2004-2006

Cadre Research
2004

Crown Research Institutes
2002

Abstract. It has been well established that during the late Quaternary, Khvalynian transgression of Caspian Sea occurred, when sea level rose tens meters above present level. Here, we evaluate physical feasibility hypothesis maximum phase this extraordinary event (known as “Early transgression”) could be initiated and maintained for several thousand years solely by hydroclimatic factors. The is based on recent studies dating highest stage (well +10 m a.s.l.) to final period deglaciation,...

10.5194/hess-28-241-2024 article EN cc-by Hydrology and earth system sciences 2024-01-17

10.1016/s0341-8162(99)00029-6 article EN CATENA 1999-10-01

Abstract Empirical prediction equations of the form W = aQ b have been reported for rills and rivers, but not ephemeral gullies. In this study six experimental data sets are used to establish a relationship between channel width ( , m) flow discharge Q m 3 s −1 ) gullies formed on cropland. The resulting regression equation 2·51 0·412 ; R 2 0·72; n 67) predicts observed reasonably well. Owing logistic limitations related respective set ups, only relatively small runoff discharges (i.e. <...

10.1002/hyp.392 article EN Hydrological Processes 2002-02-28

Abstract The processes of sheet, rill and gully erosion on the slopes Russian Plain are controlled by same factors as elsewhere: cover, erodibility, erosivity landform. combination land‐use history variations in these bio‐physical produced a that is unique to this area. most eroded soils occur Non‐Black Earth area, especially where there soddy‐podzolic soils. Over entire Plain, 99 × 10 9 m 3 soil have been lost from since AD 1696. On arable land, layer <10 cm thick has 82% 10–20 removed...

10.1002/hyp.1391 article EN Hydrological Processes 2003-11-01

Abstract The process of gully erosion at the active stage is far from equilibrium; rather, shows characteristics a self‐organizing system that close to crisis. This qualitative description similar understanding open dynamic systems state selforganized criticality (SOC). We tried find quantitative attributes SOC in numerical simulations evolution with model. Three scenarios were used: (1) controlled by initial topography and texture, when discharge base level are constant; (2) constant lowers...

10.1002/esp.1334 article EN Earth Surface Processes and Landforms 2006-04-25

The Yamal Peninsula occupies the northern part of West Siberian Plain in Russia. This territory has rapidly developed due to exploitation several gas fields. At same time, is one most severely gullied landscapes Arctic. potential risk damage environment or structures and cost such damages are very high there. erosion cumulative by runoff above critical, calculated for each point at a catchment. Calculations take into account geomorphic, lithological, vegetation cover thresholds, realized...

10.3390/su12010260 article EN Sustainability 2019-12-28

Abstract Floodplain morphology is described in relation to channel pattern changes the past. The oldest segments of present-day floodplains were formed Late Valdai (Weichselian). Their inherited from large palaeomeanders (macromeanders) under extremely high discharge conditions. A map spatial distribution macromeander relics on East European Plain given. Various floodplain have a spectrum ages that may reflect only selected portions river history. most widespread morphological units...

10.1144/gsl.sp.1999.163.01.17 article EN Geological Society London Special Publications 1999-01-01

Abstract The Stavropol region of southern Russia is severely affected by human‐induced gully erosion. A lack detailed information on the different stages formation resulting from major agricultural expansion c . 100 years ago, an obstacle for management and containment these systems. In this study we combine measurements particle‐bound radionuclides ( 137 Cs, 210 Pb ex , 226 Ra, 232 Th 40 K) classical geomorphology to investigate reconstruct phases development a during last years. We believe...

10.1002/esp.1025 article EN Earth Surface Processes and Landforms 2004-03-01

Fractal dimensions of the more than 200 large river networks former USSR were calculated. We use term «fractal» as «a structure consisted parts which are in some sense alike to whole». River don't possess complete self-likeness – fractal dimension changes with change measurer unit and chosen length rivers. Therefore calculations fulfilled lying within limits 1–10 km. from 1.1 1.7, corresponds aggregate short rivers (1–10 km) consisting 20–80% total network length. Then all studied have...

10.15356/0435-4281-2014-1-3-14 article EN cc-by Geomorphology RAS 2015-02-21

Abstract Field experiments at Tiramoana station 30 km north of Christchurch, New Zealand using an erosion plot 16·5 m long, 0·6 wide, and with a slope 14–14·5° on rendzina soil aimed to measure the variability flow velocity aggregates transport rate in shallow overland flow. Discharge/cross‐section area ratio was used estimate mean velocity, high‐speed digital video camera image analysis provided information about sediment variability. Six runs 0·5–3·0 L s −1 discharges were supercritical...

10.1002/hyp.7006 article EN Hydrological Processes 2008-03-20
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