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The storage capacity of underground gas storages in the Czech republic

Klempa, Martin

Abstract

Sources of natural gas are in most cases located in remote areas far from the places where the gas is utilized, i.e. especially developed industrial countries to which it is transported via pipeline. However, transit gas pipelines, which are transporting extracted gas to the consumers, have a relatively limited peak capacity, the transit supplies essentially have a stable character and are not able to cover increased seasonal or peak demands for gas in gas distribution networks. The solution of this problem is the main task for underground gas storages (UGS) that through the operative regulation maintain stability and reliability of the entire gas system. This article provides a general list of options that can increase the storage capacity of natural gas in underground gas storages and focuses on factors that influence the options of an individual UGS.

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18 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 THE STORAGE CAPACITY OF UNDERGROUND GAS STORAGES IN THE CZECH REPUBLIC Jakub RYBA, Pe BUJOK, Ma in KLEMPA Ins i u e o Clean Technologies o Mining and U iliza ion o Raw Ma e ials o Ene gy Use, Facul y o Mining and Geology, VSB – Technical Uni e si y o Os a a, 708 00 Os a a Po uba, Czech Republic E-mail: jakub.[email p o ec ed]z ABSTRACT Sou ces o na u al gas a e in mos cases loca ed in emo e a eas a om he places whe e he gas is u ilized, i.e. especially de eloped indus ial coun ies o which i is anspo ed ia pipeline. Howe e , ansi gas pipelines, which a e anspo ing ex ac ed gas o he consume s, ha e a ela i ely limi ed peak capaci y, he ansi supplies essen ially ha e a s able cha ac e and a e no able o co e inc eased seasonal o peak demands o gas in gas dis ibu ion ne wo ks. The solu ion o his p oblem is he main ask o unde g ound gas s o ages (UGS) ha h ough he ope a i e egula ion main ain s abili y and eliabili y o he en i e gas sys em. This a icle p o ides a gene al lis o op ions ha can inc ease he s o age capaci y o na u al gas in unde g ound gas s o ages and ocuses on ac o s ha in luence he op ions o an indi idual UGS. Keywo ds: na u al gas, unde g ound gas s o age (UGS), s o age capaci y 1 INTRODUCTION Unde g ound gas s o ages (UGS) became a necessa y pa o he gas anspo sys em in all de eloped indus ial coun ies. Al hough he ini ial implemen a ions o hese new echnologies we e used mainly o co e he seasonal consump ion, hei posi i e in luence oday a ec s he whole anspo sys em due o an inc ease in consump ion and he necessi y o anspo gas o e inc easingly longe dis ances. Rela ion o gas anspo sys ems o he ope a ion o UGS allows o a ain he maximum capaci y o gas pipes o e he whole yea [1,2,3]. The achie emen o high u iliza ion ac o is ca ied o e o “supplying” gas ese oi s which could employ injec ion/p oduc ion wells a a highe deg ee due o he balanced egime and bene i om a o able de elopmen o exploi a ion egimes. Unde g ound gas ese oi s in hei ini ial s ages o de elopmen we e buil especially in deple ed ese oi s o hyd oca bons [4]. Howe e , deple ed ese oi s we e no always in he app op ia e p oximi y om he place o concen a ed gas consump ion. In hese cases, unde g ound s o ages o mos ly aqui e o ca e n ype [5,6,7] we e c ea ed. Fo he schema ic o e iew o UGS dis ibu ion in he Czech Republic, see Figu e 1. 19 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 Figu e 1. The scheme o dis ibu ion o UGS in he Czech Republic [8] A o al olume o gas in UGS ( ese oi laye s – s o age ho izons) can be di ided in o wo basic pa s – ac i e and passi e. The passi e pa is e e ed o as a basic illing, i.e. cushion gas. This pa consis s o gas ha is pe manen ly loca ed inside an unde g ound s o age bo h du ing he wi hd awal and a e i [9,10,11]. The ac i e pa is he ope a ional capaci y o gas i sel in UGS (so-called s o age capaci y), which is ope a i ely injec ed and consequen ly wi hd awn om he ese oi acco ding o he demand o cus ome s and o ade pu poses. To al s o age capaci y, he size o he ac i e and basic illing (cushion gas) belong o he basic pa ame e s o UGS. To al s o age capaci y di ec ly depends on he size o he po e olume o he ese oi laye s. I he s o age objec is he o iginal sou ce o hyd oca bons, he o al s o age capaci y is ela ed o i s ini ial olume. The olume o cushion gas, which main ains he necessa y p essu e le el o he p ese a ion o ope a ing pe o mance o ope a ing wells, has an impac on he e iciency and economy o UGS ope a ions. In case p ima y o edge wa e is p esen , cushion gas also main ains an app op ia e dis ance o con ac wa e – gas om hose wells. The olume o cushion gas depends especially on he cha ac e o a deposi and equi ed pa ame e s o UGS. Basic illing (cushion gas) gene ally makes 45 o 60 % o o al capaci y, he e o e ac i e illing mos ly makes 40 o 55 %. A ese oi s loca ed in he deple ed deposi s, i is aimed o he 1:1 a io. Fo aqui e ypes o ese oi s, he a io is usually 1:2 in a ou o basic cushion wi h ega d o speci ic hyd odynamic p oblems o his ype o unde g ound s o age. Due o he na u e o gas s o ing ac i i y, i is logically implied ha i is in he in e es o owne s o ope a e UGS a peak e ec i e le el, i.e. a maximum ope a ing pa ame e s wi h app op ia e in es men and ope a i e cos s. Economic ac o s ela ed o he pu chasing and selling o na u al gas will no be discussed in his a icle. Jus i ica ion comes ou om he ac ha he o iginal u iliza ion o s o age objec was mo i a ed mos ly by he needs o main ain balance in he dis ibu i e ne wo k, while he con empo a y and especially u u e u iliza ion is p edominan ly ocused on e iciency, lexibili y and a iabili y o s o ed olumes and signi ican ly highe dynamics o he p ocesses. The e o e, he jus i ied needs o e-e alua ing he cu en ly applied pa ame e s o indi idual s o age objec s a e becoming appa en . I can be de i ed om he cha ac e is ics o UGS ope a ion ha he s o age capaci ies should be as la ge as possible. They can be sligh ly inc eased e en du ing he long- e m ope a ion o he UGS by he in luence o “cycling” he gas (injec ion, p oduc ion), by he p ocess o he so-called “pu i ica ion” o collec o (yield o ine mine al pa icles eleased by he hea dila ion, p essu e s ain o e en ually u bulen il a ion om ock skele on) and u he by d ying he po e space o he ese oi which con ibu es o he spon aneous inc ease o s o age olumes [12,13,14]. Du ing he designing o UGS ope a ion (buil inside he deple ed o nea ly deple ed ese oi s o hyd oca bons), he alues o ope a ional p essu es (pmax, pmin) a e de i ed om he o iginal da a o he ese oi p essu es and hei ela ion o he hyd os a ic p essu e. These alues a e espec ed and, o inc ease sa e y du ing he ini ial ope a ion o UGS, hey a e usually sligh ly unde sized. A e he ansi ion o he egula cyclic ope a ion 20 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 ollowing he ca e ul analysis o all unde lying da a, especially limi ing ac o s (places o endange ed igh ness o ese oi , see Figu e 2) and long- e m expe ience om moni o ing, ield and labo a o y esea ch and modelling o he UGS ope a ion, i is possible o sugges and, a e he app o al o espec i e ins i u ions, o implemen inc ease o uppe ange o ope a i e p essu es a up o app ox. 10 % abo e he hyd os a ic p essu e ( ela i e o he gi en dep h le el) o o he p essu e o o iginal deposi . Figu e 2. Places o endange men o ese oi igh ness – geological (p ima y he me ici y) and an h opogenic in luences (seconda y he me ici y) 2 OPTIONS OF INCREASING STORAGE CAPACITIES The op ions o inc easing o al s o age capaci ies o na u al gas in UGS can be di ided in o wo g oups – “low” olume inc ease (A) and “medium o high” olume inc ease (B). 21 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 A. “Low” olume – inc ease in o de o i s millions o i s ens o millions m3, acco ding o he o al s o age capaci y o gi en UGS. “Small” olume inc ease is usually implemen ed a UGS u ilizing o iginal hyd oca bon deposi s o s o age pu poses o aqui e s uc u es in pe iod when he UGS has al eady ully p o ed i s unc ionali y, he consume ’s demand ises, gas ma ke s p edic posi i e de elopmen ( ega ding s o age) and “medium o high” s o age inc ease is no p epa ed o is impossible o implemen . The decisi e ac o o easibili y is he s o age s uc u e ( ese oi ’s laye o laye s). Fu he ela ed pa ame e s o connec ing gas pipelines and op ions o su ace echnologies a e conside ed as sui able. Capaci y pa ame e s o ope a ional wells, connec ing gas pipes and su ace echnology do no equi e any complex adjus men s, no any signi ican in es men in o new unc ional de ices (e.g. comp esso s). Ope a ing p essu es ange om below o iginal deposi p essu e o below hyd os a ic p essu e. This can be achie ed by: a) Only by inc easing o ope a ion p essu es (i.e. an inc ease in ope a i e maximum p essu e and/o by a dec ease in minimal ope a i e p essu e) wi h essen ially minimal inc ease in po e space olume. This me hod can be applied o he s o age s uc u es limi ed by li hology o ec onically. The e is no p ima y no edge wa e o i is e en ually p esen in a negligible amoun . The op ion o adding a new po e space o he p ocess o gas accumula ion is minimal. b) Inc ease in maximum (ope a ion) p essu es connec ed wi h he inc ease in po e space olume. This me hod o inc easing imp essing (ope a i e) p essu es is, in con as o he me hod a), addi ionally connec ed o he inc ease in olume o communica ing po es. I can be applied o he s uc u es wi h bedding o ou side wa e in he cases when hey hyd odynamically communica e wi h o he uni s (see e.g. UGS Lobodice). Via he inc ease in p essu e, he wa e is pushed away, and he new po e en i onmen is connec ed o he s o age p ocess. When assessing he op ions o inc easing ope a i e p essu e, i is necessa y o addi ionally (see poin a) analyse he impac on he unc ionali y o wa e sealing. E en in his case, i is possible (gi en he a ou able condi ions) o implemen an inc ease in he maximum p essu es a abou 5 - 10 % abo e he o iginal deposi p essu e o hyd os a ic p essu e (in ela ion o he gi en dep h le el). B. “Medium o high” olume – inc ease in he o de o ens o i s hund eds o millions m3, acco ding o he o al s o age capaci y o e alua ed s uc u es. “High o low” olume inc ease can be implemen ed in sui able a eas (mo e objec s uc u es) gi en he a ou able condi ions (s a e subsidies, EU subsidies, sui able in es o , long- e m inc ease in demand, p edic ed a ou able de elopmen a gas ma ke , a ou able geopoli ical de elopmen , e c.) acco ding o he long- e m p ojec plans o cons uc ion ( e e ed o as “s ages”). These “s ages” o inc easing ope a i e s o age capaci ies can be mul iple and can a y acco ding o he di e en scena ios, which a e adjus ed o a speci ic si ua ion in he gi en pe iod. “Medium o high” olume inc ease consis s o he connec ion o new s o age objec s (app op ia e ese oi ’s laye s) in he o e bu den o in he base o cu en ly u ilized ho izons, e en ually in he connec ion o new app op ia e s uc u es in he immedia e su oundings (see e.g. UGS Třano ice). A u he op ion is o signi ican ly inc ease ope a ion p essu es a objec s, whe e he “ ese es” ha e no been ully u ilized by achie ing limi p essu es so a . Implemen a ion o his in en is limi ed by he pa ame e s o su ace plan echnology and, ou side o i s s uc u es, by pa ame e s o connec ed gas pipeline sys ems which could ha e eached he limi s o hei capaci y. The adjus men o su ace plan echnology, connec ions and adding o ope a ion wells a e usually ine i able and equi e subs an ial in es men . Ano he op ion o inc easing he o al s o age capaci y o na u al gas ega ding he needs o he en i e coun y is ep esen ed by he cons uc ion o new s o age objec s (see UGS Dambořice). Howe e , he inc ease in s o age capaci y can be implemen ed only when he he me ici y ( igh ness) o s o age s uc u es is p ese ed. Gene ally, he he me ici y o UGS unde g ound pa is di ided in o p ima y he me ici y (o iginal) and seconda y he me ici y, caused by echnical ope a ions (i.e. he an h opogenic ac i i y o people) [14,15]. P ima y he me ici y is ela ed o he igh ness o deposi objec s, which is e idenced by he exis ence o p ima y deposi ap sa u a ed by hyd oca bons (he me ici y in he dimension o geological ime). In he case o o e -p essu ising du ing he p ocess o UGS de elopmen , i is necessa y o possess knowledge o he s uc u al sealing and he ex en o gas accumula ion a e p essu ising o he ese oi . These pa ame e s a e de e mined and con olled by specialized ese oi and enginee ing me hods – especially by modelling and obse a ion o so- called p/z cu es (deposi p essu e educed by he comp essibili y ac o ). Fo he assessmen o seconda y he me ici y, we obse e dis up ion o p ima y he me ici y by an h opogenic ac i i y and ha ei he di ec ly – by d illing and consequen inadequa e equipmen o wells (du ing hei ope a ion o a e hei liquida ion) o 22 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 indi ec ly – by excessi e inc ease in ese oi p essu e ( ela ed o he inc ease o o al olume o s o ed gas), which causes dis up ion o o iginal geological seals. The o e iew o a eas, whe e he igh ness o ese oi is endange ed, is shown in Figu e 2. I clea ly p esen s bo h geological in luences (caused by he bo de s o ese oi ) and in luences caused by human ac i i y (an h opogenic in luences). The issues o igh ness ela ed o he bo om hole equipmen and he su ace p oduc ion equipmen a e no discussed u he in his pape . Types o bounda y o a ese oi can be di ided in o aul bounda y, p ima y o edge wa e bounda y, acial change and ge ing on a di e en ock massi . Among an h opogenic in luences we so – impe ec implemen a ion o bo om hole equipmen o ope a ion o e en ually obse a ion wells (including cemen ing o p oduc ion casing), insu icien ly liquida ed old wells, he in luence o p essu e and empe a u e changes on he con ac o a collec o – cap ock o impe meable base, endange o geomechanical s abili y o ese oi due o he changes o ope a i e p essu es (cycling o pmax - pmin). 3 DETERMINATION OF FACTORS LIMITING AN INCREASE IN STORAGE CAPACITIES Among signi ican ac o s ha can a ec he easibili y o inc easing s o age capaci y, we may lis he ailu e o geomechanical s abili y o s o age objec , he possible dis up ion o igh ness o cap ock and unde lying impe meable seals and he ailu e o insula i e p ope ies o cemen a ion. These ac o s should be p io i ised and e alua ed by bo h ma hema ic modelling and by labo a o y esea ch o co esponding ock (d illing co es) o , e en ually, analogical samples. Labo a o y esea ch aimed a he objec i es lis ed abo e is enabled by op-quali y appa a us (especially om F ench company Vinci Technologies [16]) and i can also be conduc ed in he labo a o ies o he Depa men o Geological Enginee ing and he Ins i u e o Clean Technologies o Mining and U iliza ion o Raw Ma e ials o Ene gy Use. To de e mine an e ec i e po osi y and absolu e pe meabili y, i is possible o u ilize he au oma ic pe meame e and po ome e Co e al 700. To assess a phase pe meabili y (gas-wa e ), a mul iphase pe meame e FDS 350 o a mul iphase pe meame e BRP 350 (see igu e 3) can be used. The de e mina ion o pe meabili y (mul iphase) is possible o conduc a ock samples (co es) a diame e 2.54 (1") and 3.81 (1,5"), leng h up o 7.62 cm a equi ed p essu e dep essions (in o de o i s ens o MPa). The comp ession o he sample (co e) in a sealing slee e – which ep esen s la e al geos a ic p essu e, can each up o 35 MPa a laye ed deposi empe a u e up o 150 °C in appa a uses BRP 350 and FDS 350. By adjus ing he appa a us, i can be used o obse e he in luence o a cyclic e ec o ope a ing p essu es (pmax, pmin) du ing he cyclic ope a ion o UGS on he s abili y o ese oi ’s ock skele on, i.e. on he in luence on he impe meabili y o cap ocks. Long- e m in luence o laye wa e s on he quali y o cemen s one can be checked a “in si u” condi ions (p essu es up o 16 MPa, empe a u e up o 80 °C) di ec ly a he a ea o con ac ock-casing-cemen in he eac ion chambe s RK-1 o own cons uc ion (pa en no. 306 107). We can also use a es cell o samples ( unc ional sample eg. no. 101/06-12-2011_F) de eloped speci ically o his pu pose, which enables he simula ion o ese oi en i onmen a labo a o y-p epa ed samples. Cu en ly, he labo a o ies lis ed abo e a e conduc ing long- e m esea ch ocusing on he cycle ope a ion o UGS. The measu emen s can check he geomechanical p ope ies o ocks ha ha e a decisi e in luence on he conside a ions abou he u he de elopmen o s o age capaci ies and sa e ope a ion o UGS. This includes especially he esea ch o he in luence o cycling maximal (pmax) and minimal (pmin) ope a ing p essu es on geomechanical s abili y o ocks skele ons (s o age and seals) and de e mina ion o “p essu e” limi o in eg i y ailu e. 23 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 Figu e 3. Bench op Rela i e Pe meame e BRP 350 (Klempa, 2018) 4 CONCLUSIONS To da e, he e a e he ollowing UGS in he Czech Republic ( o loca ion see Figu e 1): UGS Třano ice, UGS Š ambe k, UGS Lobodice, UGS T donice, UGS Dolní Dunajo ice and UGS Háhe (innogy s. .o.); UGS Uhřice and Uhřice-jih (MND gas S o age a.s.); UGS Dolní Bojano ice (SPP Bohemia a.s.); and UGS Dambořice (Mo a ia Gas S o age a.s.). Based on he e alua ion o he exis ing de elopmen o na u al gas s o age in UGS, we can s a e ha he possibili ies o “low” olume inc ease in s o age capaci ies ha e been al eady pa ially implemen ed a he long- e m ope a ing ese oi s. I we eason conse a i ely abou a e age op ion o inc easing o al s o age capaci ies a 5 %, hen he ou come could be es ima ed a app ox. 154 million m3. A u he inc ease ia his me hod would equi e conduc ing a highe amoun o labo a o y esea ch. The expendi u es o conduc ing hese labo a o y simula ions and alida ing hese al e na i es a e incompa ably lowe han he p epa a ions o lis ed al e na i es “B”. Mo e p og essi e al e na i es o ype “B” ha e been al eady implemen ed a some a eas which include UGS T donice (connec ing new Sa ma ian ho izons) UGS Třano ice (connec ing new sepa a e deposi objec in immedia e su oundings); UGS Uhřice (connec ing new sepa a e deposi objec – Uhřice-jih); UGS Š ambe k (ins alling comp esso s a ion, o iginally he injec ion was ealized only ia he o e p essu e om dis ibu i e gas pipeline). The newes UGS Dambořice was pu in o ope a ion in 2017. The o e iew o indi idual UGS and hei echnical pa ame e s in he Czech Republic (si ua ion in 2016) is lis ed in Table 1 [17]. 24 GeoScience Enginee ing Volume LXV (2019), No. 3 h p://gse. sb.cz p. 18 – 25, ISSN 1802-5420 DOI 10.35180/gse-2019-0014 Table 1. Technical pa ame e s o indi idual UGS in he Czech Republic [17] Ope a o UGS S o age Capaci y Maximum wi hd awal capaci y Maximum injec ion capaci y mil. m3 mil. m3/day mil. m3/day innogy GS Háje 64 6.0 6.0 Dolní Dunajo ice 900 17.0 12.0 T donice 535 8.0 8.0 Lobodice 177 5.0 2.5 Š ambe k 500 7.0 7.0 Třano ice 530 8.0 6.0 To al 2 706 51.0 41.5 MND GS Uhřice 255 6.0 2.6 Mo a ia GS Dambořice 115 4.0 3.0 Czech Republic o al 3 076 61.0 47.1 SPP S o age, l d. (connec ion o Slo ak gas pipeline sys em) Dolní Bojano ice 576 9.0 7.0 I has been es ima ed ha by 2021 he o al s o age capaci y should each he alue o 3.7 billion m3 wi h daily wi hd aw capaci y o 79 million m3 in he Czech Republic. In compa ison o he cu en s a e, his would mean an inc ease in ope a i e olume by app ox. 0.7 billion m3. The o al s o age capaci y o UGS ep esen s mo e han 33 % o yea ly consump ion. I had been supposed ha a ound 2021 he capaci y o gas s o age (especially due o he new connec ed objec s) could each up o 40 % o yea ly gas consump ion [8]. E en o he gas companies had planned he cons uc ion o new gas s o age capaci ies in he Czech Republic. New UGSs we e supposed o be buil in Břecla a ea and in Rožná na Žďá sku. Howe e , he ealiza ion o hese p ojec s is hal ed, and i is p obable ha he p ognosis men ioned abo e will no be achie ed. Howe e , he equi emen s o inc easing s o age capaci y by indus ial companies o dis ibu ion companies can also be esol ed by s o ing gas in UGS si ua ed ab oad (see UGS ope a ed by MND a.s. in Ge many). The u ilisa ion o local s o age capaci ies o he needs o he Czech Republic was also o e ed by Uk aine. ACKNOWLEDGEMENT This a icle was w i en in connec ion wi h p ojec Ins i u e o clean echnologies o mining and u iliza ion o aw ma e ials o ene gy use - Sus ainabili y p og am. Iden i ica ion code: LO1406. 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