Use this url to cite publication: https://hdl.handle.net/20.500.14911/116356
O механизме вторичного загрязнения озер
Publication Type (CRIS)
Konferencijų tezės nerecenzuojamame leidinyje / Conference theses in non-peer-reviewed publication (T2)
Publication Type (eLABa)
Kitos konferencijos pranešimo tezės / Other conference presentation abstracts (T3)
VILNIUS TECH Research Priorities and Topics
Fizinių, technologinių ir ekonominių procesų matematiniai modeliai ir metodai / Mathematical models and methods of physical, technological and economic processes (FM03)
Lithuanian Intelligent Specialization
Energetika ir tvari aplinka / Energy and a sustainable environment (L102)
Author(s)
| Author | Affiliation |
|---|---|
Tarasyuk, Nikolay | Valstybinis mokslinių tyrimų institutas Fizinių ir technologijos mokslų centras |
Title
O механизме вторичного загрязнения озер
А. Моисеенкова, Н. Тарасюк
Title in other language
A mechanism of lakes secondary pollution
Is part of
Озерные экосистемы: биологические процессы, антропогенная трансформация, качество воды : материалы V международной научной конференции 12–17 сентября 2016 г., Минск – Нарочь = Lake ecosystems: biological processes, antropogenic transformation, water quality : materials of the V international scientific conference September 12–17, 2016, Minsk – Naroch : [abstract]
Published In
| Year | Start Page | End Page |
|---|---|---|
2016 | 331 | 333 |
Publisher
Минск : Издательский центр БГУ
Extent
p. 331-333
Science / Art Area
Technologijos mokslai / Technological sciences (T)
Field of Science / Art
Aplinkos inžinerija / Environmental engineering (T004)
Fizika / Physics (N002)
Abstract (en)
When the beginning of the temperature gr adient is positioned below the sediment surface in the absence of convective motions in a temperature stratified water column, a thin overlaying layer of sediments becomes also a significant obstacle to heat flux. This, in turn, must lead to the strengthening of the temperature gradient followed by buoyancy of the interstitial liquids. In this case, buoyancy itself inducing upward motions of the pore water in creases thermal diffusivity of the surface sediments and allows the upward movement of the beginning of the temperature gradient.
Resource Type (COAR)
TextConference outputConference proceedingsConference paper
Language
Rusų / Russian (ru)
Country
Baltarusija / Belarus (BY)
Owning collection
eLABa ID
19573614