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<br />- .. ~ • <br /> <br />7 <br />3,759,328 <br />horizontally separated patterns that each contain one <br />or more wells opening into a layer rich in water soluble <br />minerals can be operated as described in connection <br />with FIG. 2 to form horizontally expanding permeable <br />zones and produce shale oil. The sizes of the permeable <br />zones can bt monitored by means of acoustic, clccvo- <br />magnetic the like mcasuremenu of the esunu a( the <br />mbstantially void space and/or measurcmenu of the <br />volume of fluids that arc contained into caverru. Thc <br />horizontal expansi°n oC the eavcma tan be controlled <br />to provide an efficient recovery of oil Gom nonintcr- <br />sccting, generally vertically extensive zone6 that are <br />spaced w that undisturbed columns capable of sup- <br />porting the orcrburAcn art Icft between the depleted <br />zonct. <br />During the initial stages of tspanding a ruhble- <br />eentaining cavern m accordance wth the present pro- <br />cess, it is not necessary and is generally undesirable to <br />use a trmperatuct high enough [o decompou a pre- <br />dominant proportion of the fluid-contacud hear unsi- <br />tirc eaibonetc material. Il u preferable to keep the eav- <br />crn substantially full of aqueous liquid in which the car <br />boosts material is soluble. This unds to provide the <br />hest heat C<Onomy since ii minimizes the decomposi- <br />tion reaction (which is an endothermic reaction that <br />eomaumcs heal). In order to keep the cavem substan- <br />tially filled with aqueous liquid it is preferable w main- <br />tain [he pressure within the eavcrn abort the dec°mpo- <br />sition pressure of the brat atnsltivt rarbonatc material <br />at the temperature within the cavern. !n general the <br />pressure within the cavem cannot be kept high enough <br />. [o prevent such a decomposition during an oil recover- <br />ing stage. The retorting and hydr°carbon recovery is <br />preferably conducted at a [emperawre above about <br />500 F, and at the depths at which od shale is usually <br />encountered, [he pressure in the cavem cannot be h,gh <br />enough to prevent decomposition o! heat sensitive car- <br />bonate material at Such a temperature, without a dan- <br />ger of creating large eesle fractures which are extended <br />into lOCatlOns in which fracwres art undesirable. <br />When one or a plu slit}' of generally vertically extcn- <br />sivc permeable xoncs have been capandcd horizontally <br />t0 substantially the extent desired, the cir<ulaUOn of <br />fluid within throne zones or caverns u preferably ad- <br />justed to minimize the rate oChorizontal growth and/or <br />mazimixc Iht rate of oil rerovery. Such an adjustment <br />can be eKected by increasing [he temperature and/ot <br />dccrcasing the aqueous liquid content of the fluid <br />within the eavcrn. A higher temperature tends to in- <br />crease the rate of oil rrr.overy (particularly with re- <br />^pect to the gaseous eomponenu of shale of ). AJtema- <br />tively, a decrease in the aqueom liquid coots rat tends <br />to redur. r. the rate of dissolution of aoluhlc mineral. <br />Where the removal of solid material horn the oil shale <br />la confined to a removal of the fluid products of the py- <br />ralysi^ rcaeliun and/or the COs and water vapor pro- <br />duced by the decomposition of hw[ semitive carbon• <br />aces, the volume of the depleted oil shale unds to be <br />sufficient, relative to the volume of wlids that are re- <br />moved, to tcrminau the growth o(the permeable mne <br />(unlcv the od shalt is one Nat contains an exec ption• <br />ally large proporl5on °f heat scnsilive Carbonate min- <br />eral). The aqueous liquid conunt o(Iht tluid within the <br />eavcrn can be reduced by, for example, circulating m!} <br />ctantially dry steam, nr a mizturc o(e dry steam and <br />e.g„ carbon di°xid0. at a rate and tcmperawm et which <br />GU _+ .J r 70J r . rJ~ YJCJ <br />8 <br />aqueous liquid lift within thG eavcrn contains a rela- <br />tively high proportion of inert inorganic salute. <br />FlG. 3 shows downhole equipment of the type shown <br />in FlG. 1 arranged to et7e[t a downholc xpuation of <br />5 the gaseous and liquid phases of the fluid being pro- <br />duccd. particularly when the concentration o(heat sen- <br />sitive carbonalt material is relatively high, and/or the <br />temperature of the inflowing hot aqueous fluid u rela- <br />tively high, a significant amount of gquous carbon di- <br />10 oxide and water will be formod. However, to the extent <br />that it is feasible, it is desirable w produce a relatively <br />tool liquid phase fluid that con[ainrs a zignificanl pf0- <br />portion oC produced shale oil hydrocarbon. In [he ar- <br />rangement shown in FlG. 3, borehole 20 is equrppcd <br />13 with pipe strings 21, 22 and 2J. Some or all o[ such <br />pipes etc preferably thermally insulated, as indicated <br />by coatings 2A on pipes 21 and 22- pipe 21, through <br />which the hot aqueous fluid is inflowed, opens into the <br />borehole et a relatively shallow depth. Pipe 22 extends <br />20 to an intermediate depth and is used to outlow fluid <br />[he[ u relatively tool but is predominately gaseous. <br />Pipe 23 extends to a relatively deep depth, is preferably <br />equipped wish downhole pumping means (not shown), <br />and is uxd w outflow fluid that is predominately liquid. <br />23 'pet vertical xction of bo[chule between the ends of <br />pipcf 22 and 23 urvex as a downhole gravity of upara- <br />tion chamber. <br />Steam or a mix tore °C steam and hot aqueous liquid <br />(hot water) it inflowed through pipe 21. Thc inflowing <br />30 hottest and lightest gaz tends to remain above the <br />cooler and heavier gas and N situ generated carbon di- <br />oxide. The cooler gaits outflow through pipe 22 while <br />the hones and lighter inflowing gases tend to flow along <br />the walls of the cavem. Where desirable a rclaucely <br />33 light and cool gas, such as methane, hydrogen, etc., can <br />be maintained substantially static, or slowly injected, <br />through anA around the upper p°rtion of the borehole <br />and cavern. <br />Once the nibbled oil shale cavem has been estab- <br />40 lished and the heat sensitive minerals and water-soluble <br />carbonates removed as an aqueous solution, the hydro- <br />carboru (oil)can be recovered by suitable means such <br />az by contacting the nibbled oil shale within the tavern <br />with a pyrolyring fluid to effect decomposition o! the <br />43 kcrogens to hydrocarbon which a removed from the <br />formation. In recovering the hydr°carbons, the pyro- <br />lyzing fluid can be injected (FIG. !) via 7 and reeov- <br />ered via cubing g visa versa and in a dual sytem as <br />shown in FIG. 3 the pyrolyring fluid ouch as steam can ' <br />So be injected via mbing string 21 and the hydrocarbon ~ <br />recovcrcd vie 22 or the proccse can be revcrxd. <br />It is understood that various changes in the detailed <br />described to captain the invention can be made by per- <br />55 sons skilled in the tit within the scope o(the invention <br />as cxpsessed in the appended claims. - <br />1 claim az my mvcntion: <br />t 1. In a process for expanding a zone of pcrmeahility <br />within a subterranean oil Shale by forming a permeable <br />~ zone within a portion that eon[ains heat Xnsitive cu- <br />bonatc mineral and circulating hot aqueous ^uid within <br />the permeable zone, the improvement which com- <br />p(IXS: <br />irtflowing hot aqucoua fluid into contact with ssub- <br />63 Icrrancan portion of nil shalt that contains heat <br />unsitive carbonate mineral at a relatively shallow <br />depth, the tr.mpesatufc of acid inllowing fluid being <br />