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Publication numberUS2777679 A
Publication typeGrant
Publication date15 Jan 1957
Filing date20 May 1952
Priority date7 Mar 1952
Publication numberUS 2777679 A, US 2777679A, US-A-2777679, US2777679 A, US2777679A
InventorsFredrik Ljungstrom
Original AssigneeSvenska Skifferolje Aktiebolag
Export CitationBiBTeX, EndNote, RefMan
External Links: USPTO, USPTO Assignment, Espacenet
Recovering sub-surface bituminous deposits by creating a frozen barrier and heating in situ
US 2777679 A
Abstract  available in
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Claims  available in
Description  (OCR text may contain errors)

Jan. 15, 1957 LJUNGSTRGM 2,777,679

F. RECOVERING SUB-SURFACE BITUMINOUS DEPOSITS BY CREATING A FROZEN BARRIER AND HEATING IN SITU Filed May 20, 1952 4 Sheets-Sheet 1 1957 F. LJUNGSTROM 2,777,679

RECOVERING SUB-SURFACE BITUMINOUS DEPOSITS BY CREATING A FROZEN BARRIER AND HEATING IN SITU 7 Filed May 20, 1952 4 Sheets-Sheet 2 Q W i m I L 15, 1957 F. LJUNGSTROM 2,777,679

RECOVERING SUB-SURFACE BITUMINOUS DEPOSITS BY CREATING A FROZEN BARRIER AND HEATING IN SITU 4 Sheets-Sheet 3 Filed May 20, 1952 Jan. 15, 1957 F. LJUNGSTROM 2,777,679

RECOVERING SUB-SURFACE BITUMINOUS DEPOSITS BY CREATING A FROZEN BARRIER AND HEATING IN SITU Filed May 20, 1952 4 Sheets-$11961! 4 United tates RECOVERING SUE-SURFACE BITUIVHNOUS DE- POSITS BY CREATING A FRGZEN BARRIER Ab?) EATING 3N SITU Fredrik Linngstriim, Fislrebackskil, Sweden, assignor to Svenska Sldfierolie Aktiebolaget, (lrebro, Sweden, a joint-stock company of Sweden Application May 20, 1952, Serial No. 288,945

Claims priority, application Sweden March 7, 1952 Claims. (Cl. 262-3) My present invention relates to pyrolysis and gasifying of bituminous sub-surface deposits, such as oil shale, oil sand, tar sand and coal in situ, i. e. in place in the earth. Sub-surface deposits are in this connection to be understood to mean also non-consolidated sub-terraneous strata such as fuel-containing sand. According to the method set forth oil and/or gases are produced by directly heating parts of the fuel-containing deposits or layers. The loss of heat entailed by a pyrolysis in situ has in the methods hitherto proposed or employed been much increased by the losses of heat caused by the inevitable evaporation of water leaking in or otherwise penetrating into the deposits or layers. This drawback is particularly disturbing when the fuel-containing deposits or layers are interposed by porous layers or strata consisting of sand, decomposed limestone or other such geological formations which are aquiferous in the horizontal plane and usually because of the existence of vertical splits or fissures in the layers facilitate the access of water from the sides or from above. In this connection the economy of the heating process has proved to be largely depending on the horizontal extent of the field exposed to heating, the efliciency increasing with the size of the field which is to be explained by the fact that the penetration into the field of water from the surroundings decreases in the same degree as the area of the field increases.

in order to reduce the leakage of water into the field to be worked a drainage of the surroundings may be performed prior to the heating for example by pumping ofi subsoil water by means of a larger or minor number of drilled wells. in this way the hydraulic pressure and consequently the quantity of leakage water are obviously reduced.

One object of my invention is effectively to counter- 5 act leakage of water from the surroundings into the body of bituminous deposit the fuel-content of which is to be extracted.

A further object of my invention is to counteract a communication in the opposite direction, i. e. from the body of the deposit toward the surrounding so as so much as possible to prevent gases developed by the pyrolysis to escape from the heated body otherwise than through pro-determined collecting places.

Still a further object of my invention is to ensure when proceeding with methods working in situ and using superatmospheric pressure that said pressure is maintained in the body of deposit which is the object of the gasifying process.

Further objects and advantages of my invention will be apparent from the, following description considered in connection with the accompanying drawings, which forms part or" this specification, and of which:

Fig. l is a vertical section through different layers of geological formations including one fuel-containing layer and having members introduced there into adapted to carry out the method according to the invention; said ice figure being a section along line II of Fig. 2 which in turn is a plan view of the surface of the area in question.

Fig. 3 is a longitudinal section through a combined freezing and heating element.

Figs. 4 and 5 are vertical'sections through the geological formations with wells or holes penetrating the same and into which freezing elements constructed according to the invention are partly inserted.

Figs. 6 and 7 are diagrammatic plan views an area treated according to the method of the invention.

Fig. 8 is a perspective view of a geological formation under treatment according to the invention.

Fig. 9 is a vertical section through a series of geological layers in which a bituminous layer is being gasified by using a modification of the method according to the invention.

In the various figures corresponding parts are denoted by the same reference numerals.

Referring to the drawings, 1%) designates a surface overburden consisting of earth and gravel sand which in the embodiment illustrated rests on a layer of limestone 12. This latter is in turn located over a layer 14 of the bituminous geological formation such as oil-shale which is to be subjected to pyrolysis. Below the layer 14 is a layer 1% which is supposed to consist of non-aquiferous clay slate or clay. The transition between the layers 1- and 16 may be constituted by a thinner layer 13 comprising eroded or dismembered, for example sandcarrying clay slate. The sequence of layers just described is in general typical for alum slate formations at various places in the world because of their formation during the same geological periods. The sequence is, of course, given as an example only and may vary in each case in different ways, in particular if the bituminous deposit is of another type.

A pyrolysis of the shale layer 14 is in the embodiment presented in Fig. 1 performed by an electrothermal method. Holes or wells 19 are driven into the geological formation, and into said holes heating elements generally denoted by 29 are introduced. These elements comprise metal tubes 22 in which are placed one or a plurality of electric resistances 24. The clearance between the walls of the wells or holes 19 and the tube 22 may be filled with a granular material 22 facilitating the heat transfer, such as sand. The resistance 24 is at its lower end in electrical connection with the tube 22 and by wires 26, 28 joined in a circuit 36 for low tension alternating current of, for example, three-phase character. The clearance between the resistance 24 and the tube 22 is filled with quartz sand or a similar granular material in order partly to prevent the current from flashing over and partly to facilitate the transfer of the generated heat to the shale layer. By being constructed with coils having various pitches the resistance 24 may be given varying heat capacity, for example so as to supply more heat to the upper and lower portions of the bituminous layer 14 than to its intermediate portions. The gases developed by the supply of heat are collected by holes 34 from which tubes 36 extend to the surface. Between the lower end of the tube 36 and the wall of the hole 34 is a sealing flange 33 above which the tube is encased by a granular material 39. As will be seen from Fig. 2 each gas-collecting tube 36 may be surrounded by a large number of electric elements 21). This pyrolysis method is more fully described in co-pending patent application Serial No. 756,624, filed June 24, 1947, now Patent No. 2,732,915, to which reference is made for explanation of the method and the means required for carrying out the same.

One or a plurality of wells or holes 40 are drilled through the geological layers, said wells 'or holes 'encircling the area which is the object subjected to pyrolysis andwhicli'is'd'esignated in Fig. 2 by the zigzag-shaped 7 lines 41. According to the invention, freezing elements are introduced into the Wells or holes 40. Said claments may, as isillusfrated in Fig. 3, consist of a tube 412 en'- -tered by a narrower tube 44 forming a loop and being wound to the shape of a coil over a major or a minor portion 46 of its length. The tube 42 extends beyond.

the shale layer 14 into the layer 16 which in theillustrated example is assumed to be non-aquiferous. A liquid or gaseous cooling medium issupplied to the one shah ,Of the tube 44 through a pipe '48and escapes through the structed In the example illustrated the box or case has a bottom of water-tight material. 'The freezing elements should be located in, such a spaced relation from the area i of py'rolysis'as to permit the completion of its exploitation prior to developing such transfer of heat to the frozen barrier as will melt the ice. In this connection it may be mentioned that geological formations usually have a,

low heat transfer capacity due to which the progress of the heat is relatively slow.

Preferably the freezing coil is flexible so as to permit its easy insertion into the well or hole. As is illustrated in .Fig. 4'theloopis composed of tubular pieces 52 interconnected by flexible sleeves 54 made of rubber or simi-,

lar material. The flexibility of the freezing coil may also be obtained by winding its two shanks helicoidally, as is indicated at 5,6 in .Fig. 5. The heat transfer from the surroundin'gs tovthe loop is supported by the fact that the well whole 40 is filled with subsoil water which. when starting, the cooling operation is frozen to ice- Referring to Fig. 6, 5,8 denotes the barrier of frozen minerals andice surrounding and sealing the area subjected to pyrolysis andindicated by the zigzag-shaped full lines 41.- The pyrolysisis preferably performed so as to cause a front of heat to travel in the direction indicated 7 by the arrow 62, i. e. rows of heating elements 20 are.

switched in successively so as toreachthe temperature of pyrolysis in the fuel-containing layer approximately simultaneously along the individual lines 41; Ahead of the front of heat are successively one after the other sealing frozenbarriers 64, '66, 68, ina spaced relation such that the distance. between each of them is larger than the.

distance between the'heating' elements. When the front of heat has reached the barrier 64 the next following bar rier 66 takes over the task of encasing the field of. pyrolysis ahead of the heat front.

In accordance with the modification illustrated in Fig. 7. in front of. the area of pyrolysis there is provided a freezing front designated in the figure by the dot and dash zigzag-line 70 and travelling in the direction of the arrow 62 in the same manner as does the front of heat. In this way one isicapable of initially forming a frozen bodyof. the geological formations which subsequently is heated by starting the pyrolysis. The layers or strata to be subjected to pyrolysis and the layers existent above and below the same are thus initially cooled down to a ternperature. below the freezing point of the water contained therein, whereby. a more or less coherent frozen body is obtained which; subsequently is heated to gasification tern: peraturc, in the first instance by a travelling front of heat.

' In Figure 8=, 72 denotes a tight box or case of the-fuelcontaining. layer andadjacent layers, respectively, in which a. body 74;.forms. the object. of gasification. The

heated body may bothgatv thetop and atth e bottom; as

4 ll; 9 al siqssb bqua nd by b tumin r example non-consolidated geological formations. 7

In order to create the travelling freezing and heating fronts, the same wells or holes may be employed. Further the same elements 42'may' initially be used as freezing elements and subsequently as heating elements. The freezing elements illustrated in Figs. 4 and 5 will under their operation become surrounded by ice, as is mentioned above. In order to withdraw thema melting of the ice in the wells or holes 48 may be performed by electric heating or means of a gaseous or liquid hot medium which is introduced into the coiled pipes, which medium may be the same as the cooling medium. The quicker the melting is performed, the minor transfer of heat to the surrounding portions of the geological formations will be encountered. A nevi freezing of water in the wells or holes will occur if the temperature around the 'well or hcle is sufiiciently low. The freezing element upon release and retraction out of the well or hole may be transferred to a well or hole of the next now. When. the front of heat commences to approach the wells or holes 40 and the "ice in them melts, they are used for the insertion of heating elements or as holes for the escape of developed gas. If desired, athawing of the ice inthe wells or holes may, however, be performed prior-to the approach d the front of heat, for examplein order to use them for the supply or escape of gas.

face of the soil.

'Fig. 9 finally illustrates'an embodiment, where the bituminous deposit, such as oil-shale, is gasified by introducirzg oxygen or air into the same. driving a plurality of holes 76 down to the deposit and preferably to the vicinity of its bottom layer. holes '76 are inserted tubes 78 which at their lower end portion are sealed against the wall of thehole by means of a packing 80connected with the tubes. Further the clear-. ance between the pipe and the wall of the hole. is. filled with a granular material 82 such as sand. Through a row.

of such holes the combustion-supporting gas such as oxygen is supplied under a pressure such that the geological formations resting thereupon are lifted and a substantially horizontal space 84 is created, in the illustrated embodiment in the lower portion of the bituminous deposit;

Tests have established that within alum shale a space of the kind extends. to, a larger distance from the supply place, said distance amounting to 50 or metres, for

example. At a distance determined with respect hereto from the row of holes 76a second row of holes 86 is made into which tubes 88 are introduced and tightened with the same'means as above. exploited is surrounded with a sealingfrozen barrier by means of cooling elements arranged in the holes 40 ac-.

cording to any of the alternatives described above. Upon ignition of the fuel-containing deposit home or the other way, for example by means of electric heating elements or electric resistances located in thelower portion of the supply-tubes 78, the space 84 will cause a continuous gasi= fication in the deposit. The ignition of the deposit may also be performed by means of only the oxygen gas j supplied through the tubes 78, for-example by arapid increase of its pressure and the heating effect resultingthereof, or by oxidation with the oxygen. The developed gases flow to the collecting tubes 86 in which a corresponding superatmospheric pressure is maintained. By heat trans? fer the zone of gasification is enlarged upwards so that larger and larger portions of the deposit will be brought to .theternperature at which gases'are developed and pyrol ysis will take place. A method of this kind is described for example in the U. S. patent specification Serial No. 210,682, filed February 13,1951, now forfeited, which is referred to for explanation of itsdetails. In this case it is particularly important. that the space 84 outside the remotest. holes along the flanks of .thefront. of heat trayelling: from. one. row. of holes tothe' next. one be H For this purpose, a suitable salt may be introduced into the wells or holes from the sur- This may be done by.

Into the The field or area. to be prevented by the sealing barrier of ice from permitting the gases to escape otherwise than through the collecting pipes.

, In this alternative embodiment, too, the holes 76 and 86 may be employed for the supply of the combustionsupporting gas and the collecting of the gases developed from the deposit as well as initially creating the frozen box or case and the freezing front.

The cooling and/or heating elements may be wound up helically with loops not larger than to permit convenient transportation to the place of installation to be successively introduced into the wells or holes through straightening, if desired by being passed between a pair or system of rolls.

While several more or less specific embodiments of my invention have been shown, it is to be understood that this is for purpose of illustration only, and my invention is not to be limited thereby, but its scope is to be determined by the appended claims.

What I claim is:

1. A method of gasifying in situ and recovering bituminous sub-surface deposits which includes the steps of cooling a zone down to a temperature at least as low as the freezing temperature of water to create a barrier zone for a selected area to be treated, heating the deposit in said selected area to produce gaseous products while maintaining the barrier zone, wherein the selected area is heated along a portion thereof to produce a heat front and said heat front is caused to travel generally parallel to itself within said area, and said barrier zone includes a cold front generally parallel with said heat front travelling in spaced relation thereto in advance thereof, and wherein the heat front is maintained by heat supplied to boreholes, the barrier zone is maintained by refrigerant supplied to boreholes, and the boreholes in the barrier zone are successively thawed to remove ice therein prior to the approach of the heat front to provide for gas movement in the thawed boreholes as the heat and cold fronts advance.

2. A method of gasifying in situ and recovering bituminous material in a sub-surface formation, comprising forming a barrier zone in said formation adjacent a selected area to prevent ingress of water from adjacent areas by cooling said formation at said zone to a temperature at 3. A method of gasifying in situ and recovering bituminous material in a sub-surface bituminous formation, comprising forming a barrier zone in said formation be tween a selected area and a lateral area by introducing a cooling medium into said zone, cooling said barrier zone to a temperature at least as low as the freezing point of water to create said barrier which extends as a cold front between said selected area and the laterally adjacent area, heating said selected area along a portion thereof within said barrier zone to form a heat front to produce gaseous products from bituminousmaterial in said formation, causing said heat front to travel generally parallel to itself Within said selected area, and maintaining said cold front generally parallel to said heat front and travelling in spaced relation thereto in advance thereof, and removing gaseous products formed during heating to the surface.

4. The method as set forth in claim 2 in which the when the formation adjacent said apparatus is to be refrigerated, and said element including a heat generating resistance adapted to be inserted into said bore for supplying heat thereto when energized, whereby the formation may be selectively cooled or heated from the same bore hole without removal of the temperature control apparatus.

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Classifications
U.S. Classification166/285, 166/259, 166/60, 166/256, 175/12, 166/245
International ClassificationE21B36/04, E21B43/16, E21B36/00, E21B43/24
Cooperative ClassificationE21B36/04, E21B43/2401
European ClassificationE21B43/24B, E21B36/04