Research Article

Geofluid Systems of Koryaksky-Avachinsky Volcanoes (Kamchatka, Russia)

Table 2

(a) Water chemical compositions of deep wells of the Koryaksky-Avachinsky volcanogenic basin, according to sampling data collected from 1970–2014. Wells: GK1, G1, K6, R3, R2, 53, E1, KO1, K5, and K6 (well positions shown in Figure ). GK1, G1: data from G. Ryabinin (pers. com., 2011); R2, R3 (A. Evtukhov et al., 1995), and E1: Kopylova G. (pers. com., 2011). The remaining samples were collected by A. Kiryukhin and T. Rychkova, and analyses were performed in the Central Chemistry Lab of the Institute of Volcanology FEB RAS. and : hydrogeochemical geothermometers (, Fournier, 1977; and , White, 1970).

##DataрНNa+K+ Ca2+ Mg2+SiO2Na/K

GK104.10.19707.5207219910507024115148
G114.04.19888.8502492910034504824247242
K617.11.19908.521241175251192446476598
K817.11.19908.31463581331259159823444348596
R305.06.19927.614412869166667167679271614075111
R215.03.19938.25186901430801101221143
E130.08.201112.168344102854736226
5305.07.20118.25124154283282235919586
GK128.07.20146.9606594173338713277805926105110
K0109.06.20148.226546053275975689026378074
K530.06.20148.91624115133637180039368191
K609.06.20147.21392375213375320805225105104

(b) Water chemical compositions (ppm) of hot and cold springs of the Koryaksky-Avachinsky volcanogenic basin, according to sampling data collected from 2011 to 2016, ##: denoted names, see Table for explanation; gas, l/s; water, kg/s. The samples were collected by A. V. Kiryukhin, and analyses were performed in the Central Chemistry Lab of the Institute of Volcanology FEB RAS. and , hydrogeochemical geothermometers ( = 1309/(5.19 − ) − 273, Fournier, 1977; and = 855.6/( + 0.8573) − 273, White, 1970)

##Data°CgasрНNa+K+ Ca2+Mg2+SiO2Na/K

K809.07.20101226.3107221405611861371044.9281139
K109.07.201010106.4687407850960101845.7257128
K209.07.201011156.28774591621267131945.0278134
K309.07.2010116.566736774796297825.4265126
IS25.09.2010480.107.478733116715029415136995.1273137
K725.09.20109778831128551370117904.4296132
K225.09.20107.487243102611351142814.9281126
IS28.07.2011390.076.98002811143231034012663.1359115
K129.07.20116.66783211564147692404.629192
K229.07.2011146.386641134802184120513.8322103
VD29.07.2011426.5429<0.367472238471112.1448143
C530.07.2011~10006.5911111131.0
K114.08.2012116.4661288155868831696.5240169
K814.08.2012126.477425202851698103805.4266125
K214.08.2012136.396021974921236988.0213136
IS14.08.2012466.681350153616291501137541.8499106
K106.08.20131215–206.5696339867106390946.9231134
K206.08.201313106.285743537313691091035.5263139
IS06.08.2013460.206.5852351003153373861061154.1309145
K307.08.2013136.5657345866106690956.9232134
K108.08.2014136.56643415450880101876.3243130
K208.08.2014146.279844138631262120915.4264132
IS08.08.20146.68053076915729419241015.3267138
C709.08.20142~10006.8522341122603.3
C509.08.20144~10006.75121020137.3
AV216610.08.20145.66231030127.122845
K205.08.2015146.46.406.381246935612821091564.5293164
IS05.08.20156.78681381287129394811731563.3350164
K105.08.20156.25623710658974811556.5238163
K103.08.20166.2555368650107079725.3269120
K203.08.20165.97484699611488105774.4295123
IS03.08.20166.365828131616232445102935.1275133
K704.08.20165.9682327342148690673.1360116
K804.08.20166105314486012104119865.0277129
VD03.08.201662361152394311252.7393150
CHD03.08.20164.626075250543.4343106
CHF04.08.20164.711123040246.324571
SH04.08.20168.5181111154861.3
C505.08.20166.7713103076.0
AV220006.08.20165.301410202