Page 455 - Fundamentals of Enhanced Oil and Gas Recovery
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Microbial Enhanced Oil Recovery: Microbiology and Fundamentals                      443


                   10.12.6 pH
                   A broad range of pH can be observed in reservoirs. This factor is considered one of
                   the main environmental factors that affect the microbial growth [84]. Microorganisms
                   grow superbly under slightly alkaline condition [10] and at low pH values the micro-
                   bial activities will be adversely affected [84]. In general, the optimal pH range for
                   microbial growth is 4.0 9.0 [84,839]. However, there are evidences of withstanding
                   extreme pH values less than 2.0 at high temperatures by Sulfolobus [840]. Moreover,
                   Donaldson et al. [25] mentioned about isolation of microorganisms capable of growth
                   at pH values as low as 1.0 and as high as 12.0. Before injecting microorganisms to the
                   reservoir, the growth capability under the reservoir condition such as pH should be
                   confirmed as it is done in several laboratory studies [559,560,841]. The pH induces
                   some effects on enzymatic activities and many enzymes are sensitive to pH [84,833].
                   Jenneman and Clark [842] stated that the prevalent pH range in the oil reservoirs may
                   not hinder the microorganisms’ growth; however, the pH gradients can influence the
                   specific metabolic processes required for some certain MEOR processes. pH can indi-
                   rectly affect the microorganisms’ growth and metabolism by influencing the solubility
                   of toxic materials [25].


                   10.12.7 Lithology
                   In MEOR activities, it is necessary to inject the nutrients (and in some cases microor-
                   ganisms) in to the reservoir. The effects of rocks and clays on retentions of microbial
                   cells and nutrients are of importance through the transport process [25,629,843,844].
                   Several different minerals build the oil reservoir rocks. Sedimentary rocks are the most
                   common in oil reservoirs; however, hydrocarbons might be found in ingenious and
                   metamorphic rocks too [25,816]. Sandstones and carbonates including limestones and
                   dolomites are the main categories of sedimentary rocks in which hydrocarbons can be
                   found [25]. Fractured carbonate reservoir contains most of the world’s oil [793].In
                   this type of reservoirs, the matrix blocks are mixed to oil-wet. Carbonates and silicates
                   do not significantly retard the microbial activity but adsorptive capacity of clays and
                   some other minerals present in the reservoir rocks may interfere with microbial pro-
                   cesses [25]. There are charges on the rocks surfaces, which can adsorb the microor-
                   ganisms and prevent their transport. Amongst the clays, montmorillonite and
                   kaolinites are the greatest and the least ion exchange capacities, respectively, and illites
                   exhibit intermediate capacity [25]. Via swelling, clays absorb water, which impose
                   some limitations for microorganisms’ migration [25].


                   10.12.8 Porous Media and Microorganisms’ Size
                   Scrutinizing several field trials, Maudgalya et al. [23] stated that a minimum reservoir
                   permeability of 75 mD has been the most suitable for MEOR projects. The lower
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