scholarly journals On the relation between infrasound, seismicity, and small pyroclastic explosions at Karymsky Volcano

2007 ◽  
Vol 112 (B8) ◽  
Author(s):  
Jeffrey B. Johnson
Keyword(s):  
Karymsky Volcano

scholarly journals The 1996 Eruption of Karymsky Volcano, Kamchatka: Historical Record of Basaltic Replenishment of an Andesite Reservoir

2004 ◽  
Vol 45 (11) ◽  
pp. 2325-2345 ◽  
Author(s):  
PAVEL E. IZBEKOV ◽  
JOHN C. EICHELBERGER ◽  
BORIS V. IVANOV
Keyword(s):  
Historical Record ◽  
Karymsky Volcano

scholarly journals Explosions and periodic tremor at Karymsky volcano, Kamchatka, Russia

2004 ◽  
Vol 158 (3) ◽  
pp. 1151-1167 ◽  
Author(s):  
Jonathan M. Lees ◽  
Evgenii I. Gordeev ◽  
Maurizio Ripepe
Keyword(s):  
Karymsky Volcano

scholarly journals Degassing explosions at Karymsky Volcano, Kamchatka

1998 ◽  
Vol 25 (21) ◽  
pp. 3999-4002 ◽  
Author(s):  
Jeffrey B. Johnson ◽  
Jonathan M. Lees ◽  
Evgenii I. Gordeev
Keyword(s):  
Karymsky Volcano

scholarly journals Three-dimensional volcano-acoustic source localization at Karymsky Volcano, Kamchatka, Russia

2014 ◽  
Vol 283 ◽  
pp. 101-115 ◽  
Author(s):  
Colin R. Rowell ◽  
David Fee ◽  
Curt A.L. Szuberla ◽  
Ken Arnoult ◽  
Robin S. Matoza ◽  
...  
Keyword(s):  
Source Localization ◽  
Three Dimensional ◽  
Acoustic Source ◽  
Acoustic Source Localization ◽  
Karymsky Volcano

scholarly journals Leaching of trace elements from the rocks under action of organic acids

2017 ◽  
pp. 70-76
Author(s):  
A. V. Savenko ◽  
V. S. Savenko ◽  
A. V. Dubinin
Keyword(s):  
Crystal Structure ◽  
Trace Elements ◽  
Organic Ligands ◽  
Mass Ratio ◽  
Liquid Phases ◽  
Organic Complexes ◽  
Karymsky Volcano ◽  
Solid Liquid ◽  
Oxalic Acids ◽  
Acetic Acids

The experiments on studying leaching of trace elements (Li, Rb, Cs, Sr, Ba, V, Mn, Fe, Co, Ni, Cu, Tl, Y, La, Ce, Th, U) from unaltered ash of the Karymsky volcano (Kamchatka) under its interaction with 0.01 M solutions of oxalic, salicylic, tartaric, citric, and acetic acids at the different solid/liquid phases mass ratio were lead. Based on the obtained data it is drawn a conclusion that mobilization of trace elements occurs mainly as a result of demolition of crystal structure of rock-forming minerals, as well as (in case of oxalic acids) at reduction of Fe(III) and Mn(IV) oxyhydroxides to soluble Fe(II) and Mn(II) compounds. Organic complexes formation increases of the metals stability in solution and provides a possibility of achievement of much higher values of the dissolved forms concentration than for the lack of organic ligands.

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