Hydrocarbon production operations include water injection,
varying
stimulation approaches, and enhanced oil recovery techniques. These
treatments often affect reservoir formation, production, and injection
facilities. Such sorts of well operations cause the formation of organic
and inorganic scales in the near-wellbore region and various production
and injection structures. Downhole squeeze treatment is commonly used
as a control measure to prevent scale precipitation. A scale inhibitor
solution is introduced into a formation by applying a squeeze treatment.
The method allows scale inhibitors to adsorb on the internal rock
surface to avoid settling down the scale precipitates. Thus, the study
of adsorption of different types of inhibitors to prevent scale formation
on the reservoir rock through the execution of downhole squeeze treatment
is becoming necessary. This study incorporated different experimental
techniques, including dynamic adsorption experiments of chelating
agents employing a coreflooding setup, inductively coupled plasma-optical
emission spectrometry (ICP-OES) to inhibit the formation of iron-containing
scales in limestone rocks, and ζ-potential measurements targeting
determination of iron precipitation in varying pH environments on
calcite minerals. The influence of the inhibitor soaking time and
salt existence in the system on chelating agent adsorption was also
evaluated in the coreflooding experiments. The findings based on the
coreflooding tests reveal that the concentration of chelating agents
plays a significant role in their adsorption on carbonate rocks. The
treatments with 20 wt % ethylenediaminetetraacetic acid (EDTA) and
20 wt % diethylenetriaminepentaacetic acid produced the highest adsorption
capacity in limestone rock samples by inhibiting 84 and 85% of iron(III)
ions, respectively. Moreover, the presence of the salts (CaCl
2
and MgCl
2
) considerably decreased the adsorption
of 10 wt % EDTA to 56% (CaCl
2
) and 52% (MgCl
2
) and caused nearly 20% more permeability reduction, while more inhibitor
soaking time resulted in comparably higher adsorption and lesser permeability
diminution. The results of ζ-potential measurements showed that
the pH environment controls iron(II) and (III) precipitation, and
iron(III) starts to deposit from a low pH region, whereas iron(II)
precipitates in increased pH environments in calcite minerals.