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3.8 Risks  157

                                           P mud >P pf



                                Borehole             Borehole
                                  Pipe                 Pipe



                                                     Filter cake


                          Formation            Formation
                         (a)                   (b)

                         Figure 3.24  (a) Situation without filtercake and (b) stuck
                         pipe along the borehole wall in a permeable formation with
                         filter cake. (Modified after Schlumberger Oilfield Glossary
                         2009.)

                           overbalanced and the drilling mud forms a thick filtercake at the borehole wall.
                           The differential pressure presses the DCs into the filtercake, and if the contact
                           area is large enough the string gets stuck due to the high-contact forces. However,
                           overbalanced drilling may be necessary in permeable sediments, for example, if
                           gas influx needs to be kept out, but bears a high potential of differential sticking
                           (Figure 3.24a and b). Differential sticking mainly occurs during stagnancy of
                           rotary, for example, if a new pipe joint is added to the drillstring.
                         • Thermally induced stress on borehole wall and/or casing/cement (due to drilling
                           process): A mud which is colder (hotter) than the formation, will reduce (increase)
                           both pore pressure and hoop stresses (that are the tangential stresses on the
                           borehole wall). Consequently, cooling the mud should have beneficial effects on
                           borehole stability, whereas heating would have negative effects. As regards the
                           temperature/pore pressure coupling, this becomes negligible for rocks having
                           permeability greater than 10 µD (microDarcy).



                         3.8.4
                         Geological Risks

                         Geological risk arises from geological uncertainties or if the rock mechanical
                         reaction of certain lithologies to the drilling process is insufficiently considered.
                         In terms of well integrity as part of the well planning, the potential geologic risks
                         should be specified for each geologic unit of the well profile before drilling. Some
                         general risks as observed in different lithologies of boreholes are listed in Table 3.2.
                           Wells may encounter major unexpected structural geologic/stratigraphic changes
                         during drilling. Therefore, real-time correlation must be systematically planed in
                         advance, and must identify key marker beds and decision points. A systematic
                         and careful cutting sampling belongs to the key issues in recognizing changes
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