GEOTHERMALISMIN!THE!PROVINCE!OFVERONA...UniPd’! Fig.4aTromographand tromographic’...

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SGI Milan, Italy on the 1012 th September 2014 GEOTHERMALISM IN THE PROVINCE OF VERONA Lake Garda and Verona Province case studies Laura Agos*ni 1 , Collareda M. 3 , Castellaccio E. 4 , Dal Degan D. 4 , Antonio Galgaro 12 , Jacopo Boaga 1 1 Department of Geosciences – University of Padua, Padua (Italy) laura.agos*ni2@studen*.unipd.it 2 Ins*tute for Geosciences and Earth Resources, IGGCNR Padua, Italy 34 Geologists of Vicenza (Italy) and Verona 1. IntroducJon The presence of territories characterized by local temperature and heat flux anomalies, as the Southern Garda Lake and the Verona Province areas, is well known (Fig.1a;1b). They are found In the Po Plain, located in northern Italy between the Alpine and Apennine mountain ranges. The use of low and medium temperature geothermal resources enhances a sustainable development of the area, combined with significant energy and cost savings, as well as a substan*al reduc*on of greenhouse emissions into the atmosphere. To promote a proper use of geothermal energy through direct uses of heat and by coupling with heat pump systems it is essen*al to characterize the geothermal reservoirs involved, taking into account the local differences related to geological, hydrogeological and thermal features. 2.Tectonic and Structural CharacterisJc The rela*onship between tectonic structural characteris*c, and the presence of thermal fluids is not clear and for this reason we are studying: the difference between the chemicalphysical composi*ons of thermal groundwater of the two districts iden*fied from literature (districts A and B in Fig.1b); the presence of thermal contamina*on within the Lake Garda; the hydrothermal circuits for assessing the geothermal resource renewability. In the past authors such as Sighinolfi and Sorbini (Fig. 2) helped produce geochemical and hydrogeological models that are s*ll worthy of interest. The hydrogeological profile in the figure represents the thermal area of Caldiero called District A in Castellaccio e Zorzin, 2012. ( fig.2) Fig.1a –Map of temperatures and permeable rocks in the Po Plain with main hydrothermal systems. (Pasquale,Verdoya and Chiozzi, 2014) In evidence Verona’s Province (Fig.1 b) Fig.1b – Thermal district map of the Verona Province (Castellaccio and Zorzin 2012) 3. Geochemical and Geological data The groundwater geochemical characteriza*on obtained from the screening of available literature (Castellaccio & Zorzin 2012; Sighinolfi et al., 1982) shows the presence of different geochemical facies. The Piper diagram of the districts highlights the existence of calcium and magnesium bicarbonate waters differen*ated by their temperature level ranging between 24 and 31 °C for Caldiero groundwaters and 12 and 14°C for those belonging to the Lessinian mountains (Fig.3a). In the B district instead (Fig.3b), thermal waters, are divided into four groups according to their different temperature. In August 2013 Further analysis were carried out (put in evidence in Piper diagram, Fig.3a and 3b). At the end of september new isotopic geochemical data will be analyzed to complement previous studies. Fig. 2 – The hydrogeological background model of district A modified (Sorbini et al., 1984). 4.Methodology Seismic Sounding and Remote Sensing, passive seismic survey as HVSR (Horizontal Ver*cal Spectral Ra*o), analysis of satellite and terrestrial images LiDar) will be performed to improve the local knowledge of the geothermal resources. 5. Further developments In the research programme, some thermal analyses images have been performed to define the thermal characteriza*on of the districts and a detailed inves*ga*on about the characteriza*on of Caldiero thermal area with a tromograph (see Fig.4b). Terres*al thermography, seismic sounding and new geochemical analyses will be carried out in the lake area and the Verona Province to beder define the hydrothermal circuit of the thermal areas and to foresee a ra*onal and sustainable use of the resources. 6. References Antonelli R. e Stefanini S., 1983 Nuovi contribu* idrogeologici ed idrochimici sugli acquiferi dell’Alta Pianura Veronese. Mem. Sci. Geol., 35 (198283), pp.3567, figg.22. Castellaccio E. e Zorzin R. a cura di, 2012 Acque calde e geotermia della provincia di Verona. Aspej geologici e applicazioni Memorie del Museo Civico di Storia Naturale di Verona, 2. serie Sezione Scienze della Terra n. 8, anno 2012 Dal Degan D., 2000 Aspej geologici, idrogeologici e ges*onali sull’idrotermalismo nei complessi alluvionali e fluvioglacialia NordOvest della cida` di Verona. Alcuni Confron* con altri campi idrotermali del Veneto. Tesi di laurea inedita, a.a. 19992000, Universita` di Padova Gambillara R., Astori A., Massironi M., Mar*n S., 2003Neotedonica dell’area veronese: uno studio integrato fra microrilievo e remote sensing Mem. Sc Geol. di Padova Vol.55, pp. 1320. ISSN: 03918602 Patrizi G., 2002 – Sintesi dei risulta* dell’indagine idrogeologica, geochimica e geochimicaisotopica sugli acquiferi della Lessinia. Relazione inedita, Servin –Servizi Integra* Ges*onali Ambientali, Ravenna Piccoli G., Bella* R., Binoj C., Di Lallo E., Sedea R., Dal Pra’ A., Cataldo R., Gado G.O., Ghezzi G., Marchej M., Bulgarelli G., Schiesaro G., Panichi C., Tongiorgi E., Baldi P., Ferrara G.C., Massari F., Medizza F., Iliceto V., Norinelli A., DE VECCHI Gp., Gregnanin A., Piccirillo E.M., Sbedega G., 1977 Il sistema idrotermale euganeoberico e la geologia dei Colli Euganei. Mem. Is*tu* Geol. Mineral. Univ. Padova, 30 (1975 77), pp. 1266, figg. 97, tabb. 14., tav. 1,1 c. geol. color. (1:25.000) Sighinolfi G.P., Gorgoni C., Mar*nelli G., Sorbini L., 1982. Indagine geochimica preliminare sulle acque del sistema termale veronese. Energia geotermica, CNR, Progr. Fin. Energia, 3: 1320, Roma Thank to all authors of book “ Acque calde e geotermia della provincia di Verona. Aspej geologici e applicazioni” : Agos*ni Laura – laura.agos*ni.2@studen*.unipd.it, agoalb@*scali.it ; Castellaccio Enrico – ecastellaccio@*scali.it ; Collareda Madeo – [email protected] ; Dal Degan Davide – [email protected] Galadini Fabrizio – [email protected] ; Michelej Luca – [email protected] ;Monegato Giovanni – [email protected] ; Rogledi Sergio – [email protected] Scardia Giancarlo – [email protected] ;Zorzin Roberto – [email protected] ; Mincioj Giuseppe (Director of Museo of Natural Hystory of Verona) – [email protected] Fig.4.b Tromographic data in geological map. In evidence the Rocca hill and the Gazzo hill, whose origin is volcanic. Quaternary sediments Cenozoic limestones and marls Mesozoic limestones and dolomites Crystalline basement Faults Cold surface waters Thermal deep waters Adige R. meters 2000 1000 1000 2000 0 0 10 km NORD Map of thermal areas of Verona’s Province Fig.5 Image of Eastern Verona Province (LiDar Ministero dell’Ambiente e della Tutela del Territorio e del Mare) modified by A. Ninfo –Geosciences UniPd Fig.4a Tromograph and tromographic device for HVSR acquisi[on Fig.4.c Two examples of HVSR output of Giunone spa in Caldiero town. We can see a high peak when rock is compact and a large peak when rock is fractured such as near area volcanic (the Rocca hill and the Rocca hill in Caldiero see Fig.4b) Fig.3a – Chemical analysis of wells and springs district A. In evidence the close correla[on between analysis of Lessinian mountains cold waters and warm waters 2013 data Fig.3b – Analysis of district B. Thermal waters with different temperatures are highlighted. The chemical analysis of 2013 are marked in green (Castellaccio and Zorzin,2012 modified by L.Agos[ni)

Transcript of GEOTHERMALISMIN!THE!PROVINCE!OFVERONA...UniPd’! Fig.4aTromographand tromographic’...

Page 1: GEOTHERMALISMIN!THE!PROVINCE!OFVERONA...UniPd’! Fig.4aTromographand tromographic’ device’for’HVSR acquisi[on’ Fig.4.c Two’examples’of’HVSRoutputof’Giunone’ spa

 SGI  Milan,  Italy  on  the  10-­‐12th  September  2014      

GEOTHERMALISM  IN  THE  PROVINCE  OF  VERONA    Lake  Garda  and    Verona  Province  case  studies  

Laura  Agos*ni1,  Collareda  M.3,  Castellaccio  E.  4,  Dal  Degan  D.  4  ,  Antonio  Galgaro1-­‐2  ,  Jacopo  Boaga1    1Department  of  Geosciences  –  University  of  Padua,  Padua  (Italy)  laura.agos*ni2@studen*.unipd.it  

2  Ins*tute  for  Geosciences  and  Earth  Resources,  IGG-­‐CNR  Padua,  Italy  3-­‐4Geologists  of  Vicenza  (Italy)  and  Verona  

 

1.   IntroducJon  The   presence   of   territories   characterized   by   local   temperature   and   heat   flux  anomalies,   as   the   Southern  Garda   Lake  and   the  Verona  Province  areas,   is  well  known   (Fig.1a;1b).   They   are   found   In   the   Po   Plain,   located   in   northern   Italy  between  the  Alpine  and  Apennine  mountain  ranges.  The  use  of  low  and  medium  temperature  geothermal  resources  enhances  a  sustainable  development  of  the  area,  combined  with  significant  energy  and  cost  savings,  as  well  as  a  substan*al  reduc*on  of   greenhouse  emissions   into   the  atmosphere.   To  promote  a  proper  use  of  geothermal  energy  through  direct  uses  of  heat  and  by  coupling  with  heat  pump  systems  it  is  essen*al  to  characterize  the  geothermal  reservoirs  involved,  taking   into   account   the   local   differences   related   to   geological,   hydrogeological  and  thermal  features.    

 2.Tectonic  and  Structural  CharacterisJc  The   rela*onship  between   tectonic   -­‐   structural   characteris*c,   and   the  presence  of   thermal  fluids   is  not   clear   and   for   this  reason  we  are  studying:  -­‐  the  difference  between  the  chemical-­‐physical  composi*ons  of  thermal  groundwater  of  the  two  districts  iden*fied  from  

literature  (districts  A  and  B  in  Fig.1b);  -­‐  the  presence  of    thermal  contamina*on    within  the  Lake  Garda;  -­‐  the  hydrothermal  circuits  for  assessing  the  geothermal  resource  renewability.  -­‐  In  the  past  authors  such  as  Sighinolfi  and  Sorbini  (Fig.  2)  helped  produce  geochemical  and  hydrogeological  models  that  

are   s*ll   worthy   of   interest.   The   hydrogeological   profile   in   the   figure   represents   the   thermal   area   of   Caldiero   called  District  A  in  Castellaccio  e  Zorzin,  2012.  (  fig.2)  

Fig.1a  –Map  of  temperatures  and  permeable  rocks  in  the  Po   P la in   w i th   ma in   hydrothermal   sys tems .  (Pasquale,Verdoya  and  Chiozzi,  2014)  In  evidence  Verona’s  Province  (Fig.1  b)  

Fig.1b    –  Thermal  district  map  of  the  Verona  Province  (Castellaccio  and  Zorzin  2012)    

3.  Geochemical  and  Geological  data  The   groundwater   geochemical   characteriza*on   obtained   from   the   screening   of  available   literature   (Castellaccio   &   Zorzin   2012;   Sighinolfi   et   al.,   1982)   shows   the  presence  of  different  geochemical   facies.   The  Piper  diagram  of   the  districts  highlights  the   existence   of   calcium   and   magnesium   bicarbonate   waters   differen*ated   by   their  temperature  level  ranging  between  24  and  31  °C  for  Caldiero  groundwaters  and  12  and  14°C   for   those  belonging   to   the   Lessinian  mountains   (Fig.3a).   In   the  B  district   instead  (Fig.3b),   thermal   waters,   are   divided   into   four   groups   according   to   their   different  temperature.  In  August  2013  Further  analysis  were  carried  out  (put  in  evidence  in  Piper  diagram,  Fig.3a  and  3b).  At  the  end  of  september  new  isotopic  geochemical  data  will  be  analyzed  to  complement  previous  studies.  

Fig.   2   –   The   hydrogeological   background   model   of   district   A  modified  (Sorbini  et  al.,  1984).    

4.Methodology  Seismic  Sounding  and  Remote  Sensing,  passive  seismic  survey    as  HVSR  (Horizontal   Ver*cal   Spectral   Ra*o),   analysis   of   satellite   and   terrestrial  images  LiDar)  will  be  performed   to   improve   the   local   knowledge  of   the  geothermal  resources.  

5.  Further  developments  In  the  research  programme,  some  thermal  analyses  images  have  been  performed  to  define  the  thermal  characteriza*on  of  the  districts  and  a  detailed  inves*ga*on  about  the  characteriza*on  of   Caldiero   thermal   area   with   a   tromograph   (see   Fig.4b).   Terres*al   thermography,   seismic  sounding   and  new  geochemical   analyses  will   be   carried  out   in   the   lake   area   and   the  Verona  Province   to   beder   define   the   hydrothermal   circuit   of   the   thermal   areas   and   to   foresee     a  ra*onal  and  sustainable  use  of  the  resources.  

6.  References  Antonelli  R.  e  Stefanini  S.,  1983  -­‐  Nuovi  contribu*  idrogeologici  ed  idrochimici  sugli  acquiferi  dell’Alta  Pianura  Veronese.  Mem.  Sci.  Geol.,  35  (1982-­‐83),  pp.35-­‐67,  figg.22.  Castellaccio  E.  e    Zorzin  R.  a  cura  di,  2012  -­‐  Acque  calde  e  geotermia  della  provincia  di  Verona.  Aspej  geologici  e  applicazioni-­‐  Memorie  del  Museo  Civico  di  Storia  Naturale  di  Verona,  2.  serie  -­‐  Sezione  Scienze  della  Terra  n.  8,  anno  2012  Dal  Degan  D.,  2000  -­‐  Aspej  geologici,  idrogeologici  e  ges*onali  sull’idrotermalismo  nei  complessi  alluvionali  e  fluvioglacialia  Nord-­‐Ovest  della  cida`  di  Verona.  Alcuni  Confron*  con  altri  campi  idrotermali  del  Veneto.  Tesi  di  laurea  inedita,  a.a.  1999-­‐2000,  Universita`  di  Padova  Gambillara  R.,  Astori  A.,  Massironi  M.,  Mar*n  S.,  2003-­‐Neotedonica  dell’area  veronese:  uno  studio  integrato  fra  microrilievo  e    remote  sensing-­‐  Mem.  Sc  Geol.  di  Padova  Vol.55,  pp.  13-­‐20.  ISSN:  0391-­‐8602    Patrizi  G.,  2002  –  Sintesi  dei  risulta*  dell’indagine  idrogeologica,  geochimica  e  geochimica-­‐isotopica  sugli  acquiferi  della  Lessinia.  Relazione  inedita,  Servin  –Servizi  Integra*  Ges*onali  Ambientali,  Ravenna  Piccoli  G.,  Bella*  R.,  Binoj  C.,  Di  Lallo  E.,  Sedea  R.,  Dal  Pra’  A.,  Cataldo  R.,  Gado  G.O.,  Ghezzi  G.,  Marchej  M.,  Bulgarelli  G.,  Schiesaro  G.,  Panichi  C.,  Tongiorgi  E.,  Baldi  P.,  Ferrara  G.C.,  Massari  F.,  Medizza  F.,  Iliceto  V.,  Norinelli  A.,  DE  VECCHI  Gp.,  Gregnanin  A.,  Piccirillo  E.M.,  Sbedega  G.,  1977  -­‐  Il  sistema  idrotermale  euganeo-­‐berico  e  la  geologia  dei  Colli  Euganei.  Mem.  Is*tu*  Geol.  Mineral.  Univ.  Padova,  30  (1975  -­‐  77),  pp.  1-­‐266,  figg.  97,  tabb.  14.,  tav.  1,1  c.  geol.  color.  (1:25.000)  Sighinolfi  G.P.,  Gorgoni  C.,  Mar*nelli  G.,  Sorbini  L.,  1982.  Indagine  geochimica  preliminare  sulle  acque  del  sistema  termale  veronese.  Energia  geotermica,  CNR,  Progr.  Fin.  Energia,  3:  13-­‐20,  Roma  Thank  to  all  authors  of  book  “  Acque  calde  e  geotermia  della  provincia  di  Verona.  Aspej  geologici  e  applicazioni”  :  Agos*ni  Laura  –  laura.agos*ni.2@studen*.unipd.it,  agoalb@*scali.it;  Castellaccio  Enrico  –    ecastellaccio@*scali.it;  Collareda  Madeo  –    [email protected];  Dal  Degan  Davide  –    [email protected]  Galadini  Fabrizio  –    [email protected];  Michelej  Luca  –    [email protected]  ;Monegato  Giovanni  –  [email protected];  Rogledi  Sergio  –    [email protected]  Scardia  Giancarlo  –  [email protected]  ;Zorzin  Roberto  –    [email protected];      Mincioj  Giuseppe  (Director  of  Museo  of  Natural  Hystory  of  Verona)  –  [email protected]    

Fig.4.b   Tromographic   data   in   geological   map.   In  evidence   the   Rocca   hill   and   the   Gazzo   hill,   whose  origin  is  volcanic.    

Quaternary sediments

Cenozoic limestones and marls

Mesozoic limestones and dolomites

Crystalline basement

Faults

Cold surface waters

Thermal deep waters

Adige R.

meters

2000

1000

1000

2000

0

0 10 km

NORD

Map  of  thermal  areas  of  Verona’s  Province  

Fig.5   Image   of   Eastern  Verona   Province     (LiDar  Ministero  dell’Ambiente  e  della  Tutela  del  Territorio  e   del   Mare)   modified   by    A.   Ninfo   –Geosciences-­‐UniPd    

Fig.4a  Tromograph  and    tromographic  device  for  HVSR  acquisi[on  

Fig.4.c   Two   examples   of   HVSR   output   of   Giunone  spa   in   Caldiero   town.   We   can   see   a   high   peak  when  rock  is  compact  and  a  large  peak    when  rock  is   fractured  such  as  near  area  volcanic   (the  Rocca  hill  and  the  Rocca  hill  in  Caldiero-­‐  see  Fig.4b)  

Fig.3a   –   Chemical   analysis   of   wells   and   springs  district   A.   In   evidence   the   close   correla[on  between   analysis   of   Lessinian   mountains   cold  waters  and  warm  waters  2013  data  

Fig.3b   –   Analysis   of   district   B.   Thermal   waters  with  different  temperatures  are  highlighted.  The   chemical   analysis   of   2013   are   marked   in  green   (Castellaccio  and  Zorzin,2012  modified  by  L.Agos[ni)  

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