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    F I E L D D E V E L O P M E N T

    966 SEPTEMBER 1997

    Gas hydrate formation during deepwateroffshore drilling and production is a well-recognized operational hazard. In waterdepths greater than 1,000 ft, seabed condi-tions of pressure and temperature becomeconducive to gas-hydrate formation. In awell-control situation, although the kickfluid leaves the formation at a high temper-ature, it can cool to seabed temperature withan extended shut-in period. With highenough hydrostatic pressure at the mudline,

    hydrates could form in the blowout-preven-ter (BOP) stack and choke and kill lines, ashas been observed in field operations.

    The current practice in deepwater drillingis to suppress the hydrate-formation tem-perature by use of highly saline drilling flu-ids formulated from NaCl or other salts.This solution is applicable for the Gulf of Mexico but insufficient for the conditionsencountered in Norwegian deep waters. Atextreme water depths or extremely lowmudline temperatures, this thermodynamicinhibition alone may not be sufficient toprevent hydrate formation. Instead, the useof kinetic inhibitors or crystal modifiers, inconjunction with thermodynamic in-hibitors, may allow successful operations insuch an environment. The definition of kinetic inhibitors (to distinguish them fromthe classic thermodynamic inhibitors, suchas polar compounds and electrolytes)comes from the effect of the chemicals onthe nucleation and growth of natural gashydrates, both of which are time-depen-dent, stochastic processes.

    DEEPWATER DRILLING FLUIDS

    A literature review indicated that 20 to 23wt% NaCl/polymer drilling-fluid systems arethe most commonly used fluid formulationsfor deepwater drilling. Drilling with thesesystems has been successful in water depthsup to 7,500 ft. A major operator in the Gulf of Mexico drilled wells in water depths rang-ing from 2,000 to 7,500 using mainly 20wt% NaCl- and PHPA-based drilling fluids.They experienced an average of one or moregas kicks per well. In one incident, at a waterdepth of 2,900 ft, difficulties disconnectingthe BOP were suspected to have been caused

    by hydrate formation. It is clear that thehigher the density, the shallower the water

    depth where hydrates could exist, whichprompts the question of why it has been pos-sible to drill in water depths up to 7,500 ftwithout encountering hydrates. The follow-ing can be cited as a possible explanation:(1) good well-control procedures, (2) littleor no gas kicks encountered, (3) the gas kickis of very low-gravity gas (mostly methane),(4) the effect of metastability, (5) high circu-lation rates and short shut-down periods,and/or (6) the presence of other inhibitors

    that are unaccounted for.POLAR AND SURFACE-ACTIVE

    AD DI TI VE S

    Surfactants or alcohols are known todecrease the surface tension of water, whichwill enhance the rate of gas diffusion in thebulk water during hydrate formation.Hydrate-crystal growth is controlled by therate of gas diffusion from the bulk of thewater to the crystal surface. Consequently,the presence of these compounds in thewater results in a rapid hydrate growth.Anionic and nonionic surfactants werefound to cause a dramatic increase in the rateof gas consumption on hydrate formation.Alcohols and glycols are well-knownhydrate thermodynamic inhibitors. Alcoholsand glycols, when dissolved in aqueous solu-tions, normally hydrogen bond with thewater molecules and make it difficult for thewater molecules to participate in the hydratestructure. However, their effect on the kinet-ics of hydrate formation is somehow differ-ent. Results show that the addition of alco-hol or glycol actually enhances the rate of hydrate formation, meaning that the pres-sure of small amounts of polar compounds isworse than having none. One explanationfor this behavior was that polar moleculesact as templates for nucleation when theyexist at low concentration. Also, the pres-ence of drilling-fluid additives like ben-tonite, barite, and lignite, with their tremen-dous surface area, could provide a surface onwhich gas molecules could be adsorbed.This behavior could cause the physicalentrapment of gas in quantities larger thanthe amount of gas dissolved in the water.The adsorbed gas that is dispersed within the

    bulk water with the solid particles is readilyavailable for encapsulation in the hydrate

    structure. This probably explains earlierobservations about the increase in the rateand amount of hydrate formation in drillingfluids formulated with these additives.

    KINETIC INHIBITION AND

    CRYSTAL MODIFIERS

    The kinetic inhibition of gas hydrates gen-erally refers to the process by which thenucleation and growth of hydrate crystalsare altered (modified) by use of a low con-

    centration of mostly polymeric- and surfac-tant-based chemicals. The inhibitors maycause one or more effects: (1) delay theappearance of the critical nuclei (kineticinhibitor), (2) slow the rate of hydrate for-mation (crystal modifier), and/or (3) pre-vent the agglomeration process (crystalmodifier). These chemicals do not disruptthe thermodynamic equilibrium of thehydrates. Currently, there is no clear under-standing of how some of these chemicalsaffect the growth or the morphology of thehydrate. However, it is possible for thesechemicals to control the growth and theagglomeration of the hydrate crystals byadsorbing at the crystal/liquid interface. Ananalogous approach is used by the ice creamindustry to control the growth of the icecrystals. In both of these processes, mixing(shear) plays an important role in mechani-cally smoothing the texture of the slurry.

    Working with high-salinity drilling flu-ids, as in deepwater drilling, reduces theoptions in selecting a good kinetic inhibitorand crystal modifier. Another challengeworking with these inhibitors is their sur-face activity. Because of all the surface areaspresent in drilling fluids, unless theinhibitors have a specific affinity toward thehydrate surface, one most likely will haveto cover all the solid surfaces before theinhibitor starts to work. More work isrequired before suitable kinetic inhibitorsor crystal modifiers for drilling fluids canbe recommended.

    LABORATORY MEASUREMENTS

    A thermodynamic testing program was con-ducted in two stages. In the first stage, aque-ous solutions of selected thermodynamic

    inhibitors formulated in seawater as the basefluid were tested. This stage was necessary to

    HYDRATE CONTROL INDEEPWATER DRILLING

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    968 SEPTEMBER 1997

    F I E L D D E V E L O P M E N T

    establish a baseline for the best inhibitors tobe used in the subsequent drilling- and spot-ting-fluids formulations. In the second stage,drilling-fluid formulations and two solidsfree spotting fluids with the best combina-tions of the thermodynamic inhibitorsscreened in the first stage were tested.

    RESULTS

    The tests produced a number of conclusionscovering the suitability and performance of various fluid formulations. The followingare the generalized conclusions. The most common drilling fluids used in

    deepwater drilling are the 20 to 23 wt%NaCl/polymer systems. Drilling withthese systems has been successfullyachieved in water depths up to 7500 ft.

    On a weight basis, NaCl is the most effec-tive hydrate inhibitor followed by KCl,

    CaCl2, NaBr, sodium formate, and calci-um nitrate. Ethylene glycol had the best performance

    among the glycols tested in this work. Sodium formate increases the degree of

    suppression over that of NaCl but has thetendency to precipitate at low tempera-tures and high concentration.

    A drilling fluid formulation was formulat-ed from 5 wt% KCl+15 wt% NaCl+10wt% ethylene glycol that has a maximumhydrate suppression of 32.1F.

    Two new solids-free spotting fluids weredeveloped. The first fluid did not formhydrates under an extreme degree of sub-cooling, while the second suppressed thehydrate temperature by 45.4F.

    The synthetic drilling fluid with 30 wt%CaCl2 in the internal phase did not formhydrates under extreme subcooling.However, hydrates did form when the con-centration of CaCl 2 was reduced to 15 wt%.

    The organic phase of the syntheticdrilling fluid slightly suppresses thehydrate equilibrium temperature but, atthe same time, increases the rate andamount of hydrate formation resultingfrom the higher gas solubility.

    This article is a synopsis of paper SPE 38567, Hydrate Control During Deep- water Drilling: Over view and New DrillingFluids Formulations, by H. Ebeltoft,Statoil; M. Yousif, IITRI Westport Tech-

    nology Center; and E. Soergaard, NorskHydro, scheduled for presentation at the1997 SPE Annual T echnical Conferenceand Exhibition, San Antonio, Texas, 58October. Please read the full-length paperfor additional details, illustrations, and ref-

    erences. The paper from which this synop- sis was taken has not been peer reviewed.