Daily variation of CO2 exchange and photosynthesis intensity in surface water of Lake Baikal

2007 ◽  
Vol 413 (2) ◽  
pp. 402-405 ◽  
Author(s):  
V. V. Zavoruev ◽  
M. V. Panchenko ◽  
V. M. Domysheva ◽  
M. V. Sakirko ◽  
O. I. Belykh ◽  
...  
Keyword(s):  
Surface Water ◽  
Lake Baikal ◽  
Daily Variation ◽  
Co2 Exchange

scholarly journals Chemical composition of surface water in the main tributaries of Lake Baikal – the Selenga and the Barguzin Rivers

2019 ◽  
Vol 320 ◽  
pp. 012020
Author(s):  
Ts Zh Bazarzhapov ◽  
V G Shiretorova ◽  
L D Radnaeva ◽  
D Suocheng ◽  
A K Tulokhonov
Keyword(s):  
Chemical Composition ◽  
Surface Water ◽  
Lake Baikal

Peculiarities of Long-term Variability of Surface Water Inflow to Lake Baikal

2019 ◽  
Vol 44 (10) ◽  
pp. 652-658
Author(s):  
V. N. Sinyukovich ◽  
M. S. Chernyshov
Keyword(s):  
Surface Water ◽  
Lake Baikal ◽  
Water Inflow

Influence of atmospheric precipitation on the CO2 exchange with the water surface of Lake Baikal

2007 ◽  
Vol 415 (1) ◽  
pp. 740-743 ◽  
Author(s):  
V. M. Domysheva ◽  
M. V. Panchenko ◽  
D. A. Pestunov ◽  
M. V. Sakirko
Keyword(s):  
Lake Baikal ◽  
Water Surface ◽  
Atmospheric Precipitation ◽  
Co2 Exchange

Methane in the atmosphere and surface water of Lake Baikal

2021 ◽  
Author(s):  
Dmitriy A. Pestunov ◽  
Valentina M. Domysheva ◽  
Maria V. Sakirko ◽  
Artem M. Shamrin ◽  
Mikhail V. Panchenko
Keyword(s):  
Surface Water ◽  
Lake Baikal

Application of a Simple Cold Stub to the Direct Observation of Frozen Hydrated Sand

1973 ◽  
Vol 31 ◽  
pp. 212-213
Author(s):  
John M. Wehrung ◽  
Richard J. Harniman
Keyword(s):  
United States ◽  
Surface Water ◽  
Direct Observation ◽  
Controlled Study ◽  
Clay Particles ◽  
Organic Debris ◽  
Rock Formations ◽  
Water Tables ◽  
Permeable Rock ◽  
Natural Means

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.

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