To explore the effects of scale inhibitors on subsurface water–mineral
interactions, here batch experiments on biotite dissolution (0–96 h)
were conducted in solutions containing 0–1.0 mM
diethylenetriaminepenta(methylene)phosphonate (DTPMP,
silicone additives
a model scale inhibitor), at conditions simulating subsurface
environments (95 °C and 102 atm CO2). The phosphonate groups in DTPMP
enhanced biotite dissolution through both aqueous and surface
complexations with Fe, with more significant effects at a higher DTPMP
concentration. Surface complexation made cracked biotite layers bend,
and these layers detached at a later stage (≥44 h). The presence of
DTPMP also promoted secondary precipitation of Fe- and Al-bearing
minerals both in the solution and on the reacted biotite surfaces. With
1.0 mM DTPMP after 44 h, significant coverage of biotite surfaces by
precipitates and less detachment of cracked layers blocked reactive
sites and inhibited further biotite dissolution. Furthermore, adsorption
of DTPMP made the reacted biotite basal surfaces more hydrophilic,
which may affect the transport of reactive fluids. This study provides
new information on the impacts of phosphonates in brine–mineral
interactions, benefiting safer and more environmentally sustainable
design and operation of engineered subsurface processes.
The Wall