corrosive species and scaling in wells at olkaria ... - Orkustofnun
corrosive species and scaling in wells at olkaria ... - Orkustofnun
corrosive species and scaling in wells at olkaria ... - Orkustofnun
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Concentr<strong>at</strong>ions of CO 2 <strong>at</strong> equilibrium between w<strong>at</strong>er <strong>and</strong> steam can be calcul<strong>at</strong>ed us<strong>in</strong>g<br />
thermodynamic d<strong>at</strong>a on the equilibrium partial pressures of dissolved CO 2 <strong>and</strong> a given temper<strong>at</strong>ure,<br />
us<strong>in</strong>g Henry’s law constant. The expression used is:<br />
mCO 2 = kh*Pi,<br />
where mCO 2 = concentr<strong>at</strong>ion of CO 2 <strong>in</strong> moles/kg,<br />
Kh = Henry’s Law coefficient,<br />
P i= Partial pressure of CO 2 <strong>at</strong> equilibrium <strong>in</strong> bars.<br />
Arnόrsson et al (1996) describe the temper<strong>at</strong>ure dependence of Henry’s Law coefficient given by the<br />
function:<br />
CO 2 ,g = CO 2 ,aq = -59.612 + 3448.59/T - 0.68640×10 -6 T 2 + 18.847×log T<br />
where T<br />
= Temper<strong>at</strong>ure <strong>in</strong> Kelv<strong>in</strong>.<br />
Upon extensive boil<strong>in</strong>g of<br />
geothermal w<strong>at</strong>er <strong>in</strong> produc<strong>in</strong>g<br />
aquifers <strong>and</strong> <strong>wells</strong>, the CO 2 <strong>in</strong>itially<br />
dissolved <strong>in</strong> the aquifer w<strong>at</strong>er is<br />
largely transferred to the steam<br />
which forms. Figures 15 <strong>and</strong> 16<br />
show how CO 2 concentr<strong>at</strong>ions <strong>in</strong><br />
the boil<strong>in</strong>g w<strong>at</strong>er <strong>and</strong> the steam<br />
change dur<strong>in</strong>g one step adiab<strong>at</strong>ic<br />
boil<strong>in</strong>g of w<strong>at</strong>er from selected <strong>wells</strong><br />
<strong>in</strong> the study areas.<br />
The separ<strong>at</strong>ed w<strong>at</strong>er <strong>at</strong> the surface<br />
conta<strong>in</strong>s 0.5-5 ppm dissolved CO 2<br />
<strong>and</strong> the separ<strong>at</strong>ed steam 0.2-24<br />
ppm. These are theoretically<br />
calcul<strong>at</strong>ed us<strong>in</strong>g Henry’s law<br />
constants for CO 2 <strong>at</strong> equilibrium.<br />
One might expect th<strong>at</strong> the separ<strong>at</strong>ed<br />
w<strong>at</strong>er would cause corrosion of<br />
mild steel due to its rel<strong>at</strong>ively high<br />
CO 2 content. Such corrosion is,<br />
however, generally not observed <strong>in</strong><br />
geothermal <strong>in</strong>stall<strong>at</strong>ions. The reason<br />
is considered to be the form<strong>at</strong>ion of<br />
protective sulphides, carbon<strong>at</strong>es <strong>and</strong><br />
silic<strong>at</strong>e co<strong>at</strong><strong>in</strong>g (Jones, 1996).<br />
Log PCO2 bar a<br />
100<br />
10<br />
1<br />
0.1<br />
0.01<br />
Olkaria East<br />
Olkaria West<br />
Olkaria North East<br />
Olkaria Domes<br />
Reykjanes<br />
Svartsengi<br />
Nesjavellir<br />
5 6 7 8<br />
pH<br />
FIGURE 14: Aquifer pH vs CO 2 partial pressures<br />
<strong>in</strong> the aquifer for selected <strong>wells</strong> <strong>in</strong> the study areas<br />
Upon condens<strong>at</strong>ion of separ<strong>at</strong>ed steam, CO 2 rich condens<strong>at</strong>e with a rel<strong>at</strong>ively low pH will form<br />
(Figure 17). The pH of condens<strong>at</strong>e formed from the selected <strong>wells</strong> due to CO 2 <strong>in</strong> the Olkaria West<br />
sector is lower than th<strong>at</strong> formed from the rest of the selected <strong>wells</strong> <strong>in</strong> the study areas. A complic<strong>at</strong>ion<br />
th<strong>at</strong> could arise is the <strong>in</strong>fluence of H 2 S. The problem with CO 2 corrosion is always l<strong>in</strong>ked to pH <strong>and</strong><br />
the only problem to worry about is corrosion by steam condens<strong>at</strong>e. Instability of sulphide m<strong>in</strong>erals<br />
render<strong>in</strong>g them less protective will contribute.<br />
21