By Guidi, Francesco; di Cesare, Franco; Cippitelli, Giuseppe - IAASM
By Guidi, Francesco; di Cesare, Franco; Cippitelli, Giuseppe - IAASM
By Guidi, Francesco; di Cesare, Franco; Cippitelli, Giuseppe - IAASM
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JOURNEY THROUGH THE PAST<br />
CAVIAGA GAS FIELD<br />
<strong>By</strong> <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>; <strong>di</strong> <strong>Cesare</strong>, <strong>Franco</strong>; <strong>Cippitelli</strong>, <strong>Giuseppe</strong><br />
THE AUTHORS EXPRESS THEIR APPRECIATION TO DOCTOR RICCARDO COEN, FORMERLY<br />
EXPLORATION MANAGER WITH AGIP PETROLEUM IN HOUSTON, (TEXAS) FOR HIS<br />
INSIGHTFUL SUGGESTIONS.<br />
1. Inflammable Air Native from the Marshland<br />
Alessandro Volta, Italian physicist and inventor, known for his pioneering work in<br />
electricity, was the first scientist to study methane and to understand its origin. In 1774 he<br />
was a Professor of Physics at the Royal School of Como. While on his summer holidays, in<br />
1776, on Lake Maggiore, his boat went alongside the reeds near Angera. Volta began to<br />
poke the muddy bottom of the water with a stick and saw lots of gassy bubbles floating up<br />
to burst on the surface. He collected some samples of the marsh gas and <strong>di</strong>scovered it was<br />
inflammable. He called it inflammable air from marshlands. It was what we nowadays<br />
call methane.<br />
Fig 1:<br />
Alessandro Volta, born in Como, Italy, from a noble<br />
family on 1746 and <strong>di</strong>ed on 1827 at the age of 82.<br />
Prolific inventor he is well remembered for his<br />
invention of the electric battery and stu<strong>di</strong>es on<br />
methane.<br />
In 1800 he invented the “Voltaic Pile” which was the<br />
first “wet cell battery” that produced a reliable,<br />
steady current of electricity.<br />
For the first time, Alessandro Volta recognizes the source of this inflammable gas when he<br />
states: and it is very likely that this inflammable air originates from vegetables soaked and<br />
<strong>di</strong>ssolved in water.<br />
It is interesting to note that the first natural gas <strong>di</strong>scovery in Europe occurred in the little<br />
village of Caviaga, in the Po Valley, approximately 100 kms South-East of Como.<br />
As far as the current global forecast is concerned, the widely accepted assessment is that<br />
natural gas is the most important energy source in the world: the 2030 projections of BP’s<br />
Statistical Review clearly state oil continues to suffer a long run decline in market share, while<br />
gas stea<strong>di</strong>ly gains. (fig 2).<br />
1
Fig 2: BP Energy Outlook 2030<br />
Following the above brief historical introduction, the evolution of the gas industry in Italy<br />
will now be reviewed.<br />
___________________________________________<br />
2. Gas in Italy<br />
The Caviaga gas field has been the spark that allowed Italy to become an industrialized<br />
Country and overcome the painful and destructive wounds of WWII. The search and<br />
development of natural gas gained momentum and expanded from the little village of<br />
Caviaga, to the entire peninsula inclu<strong>di</strong>ng Sicily and the offshore Adriatic. Italy’s gas<br />
consumption soared rather quickly and the BP Statistical Review reports that in 2010 the<br />
country’s gas consumption (76.1 bcm or 2,700 bcf) was third in Europe behind the United<br />
Kingdom (93.8 bcm ore 3,300 bcf) and Germany (81.3 bcm or 2,870 bcf); ahead of France<br />
(46.9 bcm or 1,650 bcf). Italy’s gas production in that year has been of 7.6 bcm (270 bcf).<br />
In any case Italian gas industry has developed a good pipeline system with a grid of more<br />
than 33,000 km (20,500 miles) and the natural gas trade movement in 2010 amounted to<br />
75.34 billion cubic meters (2,660 bcf).<br />
2
Fig 3: Enrico Mattei (1906- 1962)<br />
Fig. 4: North Italy and Caviaga Village<br />
The Caviaga gas field was the first gas <strong>di</strong>scovery by Agip (July 15, 1944) in the Po Valley<br />
area while the WWII conflict was still being fought on the Italian peninsula. Agip’s<br />
President, Enrico Mattei (1906 – 1962), promptly realized the value and significance of the<br />
gas <strong>di</strong>scovery that would be instrumental, in the years to follow, in allowing Italy to enter<br />
the post industrial phase.<br />
The <strong>di</strong>scovery of the Caviaga gas field was not only the starting point for the development<br />
of O&G in Italy; it also was the initial milestone that propelled Agip into the international<br />
E&P arena where it evolved becoming a significant competitor<br />
In 1944 Agip drilled the Caviaga gas <strong>di</strong>scovery well, just a few kilometers south of Milan.<br />
The open flow production testing carried out in the Pliocene reservoir section reached<br />
100,000 cmd, which was highly encouraging. The testing results were in<strong>di</strong>cative of a<br />
potential of very high reserves which <strong>di</strong>splayed along with the first large gas deposit in<br />
Western Europe, an almost inexhaustible and then practically unknown source of power.<br />
Today natural gas is among the most widely used energy sources, because it is more<br />
environmentally friend than oil and also offers a higher yield, especially when employed<br />
to produce electrical power.<br />
The Caviaga gas field <strong>di</strong>scovery was made a few decades before gas was found in the<br />
Netherlands and in the Northern Sea: consequently Italy was able to break through the<br />
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European gas market at least 30 years ahead of the other European countries. In the early<br />
1970s Italy produced and consumed 14 bcm (almost 500 bcf) of natural gas a year, while<br />
gas production and consumption were insignificant in other European countries.<br />
3. The State of Exploration for Hydrocarbons in Italy in the Early Forties<br />
To place all the facts in the proper context we should examine how hydrocarbon<br />
exploration in Italy fared in the 1930s.<br />
4<br />
Fig. 5: Orso Mario<br />
Corbino<br />
….In Italy it was a few years after the<br />
WWI that the country’s own petroleum<br />
industry took its first tentative steps,<br />
triggered by the Sinclair scandal. A row<br />
had erupted after Mr. Orso Mario<br />
Corbino (1876 – 1937), Italian Minister<br />
for National Economy and Mr. Weach,<br />
Vice President for Exploration of<br />
Sinclair, a New York – based oil<br />
company, signed an agreement on 29<br />
April 1924, granting the American<br />
company exclusive rights to<br />
hydrocarbon exploration in almost the<br />
whole Sicily and a good part of<br />
Emilia/Romagna region. Following a<br />
ferocious press campaign mounted<br />
against the deal, Orso Mario Corbino<br />
and his official had to resign and the<br />
Sinclair agreement was revoked on<br />
January 1925. Not long after in 1926, the Italian Government, well<br />
aware of the <strong>di</strong>fficulties in supplying gasoline and <strong>di</strong>esel to the<br />
Italian market , founded the Azienda Generale Italiana Petroli,<br />
AGIP, with the mission to explore, produce and purchase any sort of<br />
hydrocarbon both in Italy and abroad in order to stock the domestic<br />
market. But exploration in the Italian Peninsula, geologically<br />
broken by so many orogenic movements, <strong>di</strong>d not achieve very much<br />
apart from fin<strong>di</strong>ng a few accumulations of oil the northern<br />
Apennines. It was therefore inevitable that the company would have either to look abroad. (<strong>di</strong><br />
<strong>Cesare</strong> - <strong>Gui<strong>di</strong></strong>).<br />
But domestic exploration activity was never abandoned and Agip geologists devoted the<br />
search of drilling opportunities targeting the northern Apennines where many natural<br />
gas shows and seeps had been mapped and exploited since the Middle Age.
Here many of these seeps are from the “Argilla Scagliose” unit, a sequence composed of argillites<br />
and calcareous and sandy flysch with a complex and, in some places, a chaotic structure. This unit<br />
overlies the Tertiary flysch of the Northern Apennines sequence and is overlain by Oligocene-<br />
Miocene and Pliocene clastics. Most nineteenth century Italian geologists assumed that the Argille<br />
Scagliose is itself the source of the petroleum seeps, while others favoured a deeper origin. Whatever<br />
their origin, oil and gas accumulations in the Northern Apennines, as a rule, were small in size and<br />
low in productivity, and their <strong>di</strong>scovery was mainly due to chance.<br />
5<br />
Fig. 6: <strong>Cesare</strong> Porro 1865-1940 (Porro)<br />
In 1921, <strong>Cesare</strong> Porro, an Italian petroleum<br />
geologist of wide international experience (was<br />
one of the most eminent petroleum geologists of<br />
his generation. His experience spanned the<br />
world from the East In<strong>di</strong>es to the United States<br />
where he <strong>di</strong>scovered the Salt Creek field in<br />
Wyoming) summarized the status of<br />
exploration in Northern Italy. In his opinion,<br />
the Argille Scagliose could be the source of<br />
petroleum but accumulations in economic<br />
quantities require a reservoir rock sealed in a<br />
trap; reservoirs, seals, and traps are all<br />
lacking in the Northern Apennine area ,but he<br />
thought these elements possibly could be<br />
present in the external part of the Apennine<br />
chain where tectonism was presumably less<br />
intense and where Pliocene clays could provide<br />
an effective cap rock. This “external Apennine”<br />
could be buried under the alluvial cover of the<br />
southern Po Plain where geophysical surveys<br />
could be used to identify possible traps.<br />
Encouraged by this geological model, regional<br />
gravimetric surveys were carried out by Agip,<br />
during the years 1927 to 1935 and later by SPI<br />
(a subsi<strong>di</strong>ary of the Standard Oil Company of<br />
New Jersey). Several tests were drilled on<br />
positive anomalies, but results were <strong>di</strong>sappointing. The se<strong>di</strong>mentary sequence of the Po Plain<br />
subsurface was found to be <strong>di</strong>fferent in thickness and facies from the sequence exposed in the<br />
Apennines: tectonism was found to have been greater than pre<strong>di</strong>cted and structural con<strong>di</strong>tions<br />
could not be reliably interpreted from the gravimetric survey. Furthermore, gas and oil shows were<br />
scanty. (Pieri)<br />
4. Gas Seeps in Caviaga<br />
Agip’s geological interest focused on areas where oil and gas seeps were detected:<br />
Attention of the Agip Geologists were addressed, as mentioned before, to oil and gas<br />
seeps and in Caviaga, a small town in the Cavenago d’Adda <strong>di</strong>strict, near Lo<strong>di</strong>, was highly<br />
graded for that reason. In this area the natural gas seeps had been noticed in the outskirts<br />
of town by local resident for a very long time: the methane, seeping from the subsurface,<br />
polluted the air so much that the area was called “Via Gas” (Gas road).
Fig. 7: Caviaga and “Via Gas” (Gas road)<br />
Fig. 8: Caviaga, Via Gas (Gas road)<br />
5. Agip In Italy<br />
Agip had been set in 1926 by the Italian Government to help Italy to enter the field of oil<br />
and gas exploration/development: In fact the Italian economy could not find enough<br />
private capital to finance oil research. While Agip had attained some significant results in<br />
Romania, Albania and Iraq, achievements in Italy had been scanty. In the Thirties Agip<br />
produced just 1,000 tons of oil per year (7,000 barrels/year) in Italy, against a consumption<br />
6
of some million tons and about ten million cubic meters of gas per year (35 million cubic<br />
feet).<br />
Such meagre results in spite of a remarkable commitment with the drilling of 15 wells per<br />
year, on average, were due to Italy’s complex geology and the lack, at this time, of<br />
adequate technique capable of defining the subsurface pattern. At this moment Agip<br />
geologists decided to utilize a new geophysical methodology i.e. the seismic reflection<br />
which had been proved to be very effective in the United States.<br />
6. Seismic in Po Valley<br />
However, these were years when German technology dominated Continental Europe and Agip<br />
geophysicists were used to receiving information about the efficiency of German seismic<br />
methodology. Agip first decided to send a technical mission to Germany, which lasted from 20 to 30<br />
July 1938 during which time the Italian scientists had access to top German technology. Yet the<br />
final report, despite the political ties between Italy and Germany <strong>di</strong>d not contain any enthusiastic<br />
recommendations, It was probably for this reason that Agip management <strong>di</strong>d not make any<br />
contracts with German companies and instead decided to compare the status of the German seismic<br />
technology with the United States’.<br />
Agip management succeeded in convincing the Italian Prime minister Benito Mussolini to approve<br />
a visit to the USA. The mission set off in December 193, and after having met all the geophysical<br />
companies and some petroleum companies active in the Unite States, the final recommendation was<br />
decidedly in favour of Western Geophysical. The final report of the mission was subject to<br />
considerable debate and not finalised until March 1939.<br />
In the meantime dark clouds were looming on the horizon. The declarations of Adolf Hitler were<br />
threatening everything and a ruinous fury was affecting the minds and souls of the nations.<br />
Despite impen<strong>di</strong>ng gloom, Agip succeeded in signing a contract with Western for a seismic crew to<br />
be utilized in the Po Plain…On June 10, 1940 the day Italy entered WWII, already underway<br />
without the US, the first American seismic crew from Western Geophysical started acquisition<br />
work near Lo<strong>di</strong>, a few km south of Milan. Four years later, after the seismic surveys had been<br />
completed, Agip’s Caviaga well, near Lo<strong>di</strong>, found what potentially was the first large European gas<br />
field. (<strong>di</strong> <strong>Cesare</strong> – <strong>Gui<strong>di</strong></strong>).<br />
Following letter from Agip, Mr. Egi<strong>di</strong>o Castelli, the Caviaga Podestà (The Chief Magistrate<br />
in a Commune, Collins), authorized to perform seismic surveys in the area, i.e. to explode<br />
mines in the territory of this community. The mines will be made up of dynamite or other explosive<br />
of the second category, in the amount of 1 to 50 kg per charge and they will be exploded in depth<br />
(Pallavera).<br />
And the Western Geophysical seismic survey started on June 10, 1940 (deep shooting).<br />
Two were the American technicians who had even the commitment to train the Italian<br />
technicians from Agip. In October 1940, i.e. 4 months after the seismic crew had arrived in<br />
Italy, following pressures from the American Embassy in Rome, which considered the US<br />
entry in war as near (On 11 December 1941, Germany and Italy declared war on the<br />
United States). Works went on and a structure was quickly traced out at Caviaga, being<br />
the first structure detected in the Po Valley. The reports of the time describe the Caviaga<br />
structure as a wide anticline stretching toward East-West for about 8 km (5 miles).<br />
7
7. Exploration in the Caviaga Structure<br />
The wild cat produced the first positive result on 15 July 1944, following a producing test<br />
in Lower Pliocene formation (prevailing sands with thin shale intervals) in the interval<br />
1.374 – 1403.5 m (4,508’ – 4,605’). War events prevented intensive and regular tests which,<br />
on the contrary were made in Caviaga 2 wells, on 1946.<br />
60 wells for production were drilled which <strong>di</strong>sclosed an average pay of more than 300<br />
meters (1,000’) of sands with an average permeability of 750 md.<br />
Produced reserves amount to 14 billion cubic meters (495 billion cubic feet). The ensuing<br />
exploration activity has made evident Caviaga being part of a number of structures laying<br />
in the Po Valley where they took their shapes and energy . (fig 13)<br />
Fig. 9: Caviaga gas field, top Miocene Unconformity<br />
8
Fig. 10: Caviaga Gas Field: top Lower Pliocene producing sands<br />
Fig. 11: Caviaga Gas Field: Longitu<strong>di</strong>nal depth Section<br />
9
Fig. 12: Caviaga Gas Field<br />
Caviaga 2 Well<br />
10
Fig. 13: Pliocene Structures in Western part of Po Plain<br />
8. Present Gas Exploration and Production in Italy<br />
Natural Gas in Italy has been mostly produced in Po Valley and Adriatic offshore. Total<br />
production is summarized in the enclosed <strong>di</strong>agram, prepared by Jerà, utilizing data as<br />
provided by Assomineraria (Association of Petroleum Companies operating in Italy) and<br />
by DGRIME (Department for Energy of the Ministry for Economic Development).<br />
11
25000<br />
20000<br />
15000<br />
10000<br />
5000<br />
Million cm produced per year<br />
0<br />
1951 1956 1961 1966 1971 1976 1981 1986 1991 1996 2001 2006 2010<br />
It is clear that there has been a sharp decrease in production from 1994 to 2010, passing<br />
from 20.6 billion to 7.9 billion.<br />
The recent Macondo blowout in Gulf of Mexico (April 2010) has had a very negative<br />
impact on the offshore petroleum exploration in Italy, notably in Adriatic Sea where the<br />
Legislative Decree No. 128, of June 29, 2010 has practically blocked all the activity. In the<br />
central and northern part of this Adriatic Sea, Agip in the years 1992 and 1994 had<br />
acquired two large regional seismic 3D surveys for approximately 13,000 sq km (5,000 sq<br />
miles). The largest in the world at that time. The interpretation of the data had in<strong>di</strong>cated<br />
the possible presence of many gas prospects.<br />
9. Bibliography:<br />
1. Assomineraria: L’Italia, Paese <strong>di</strong> Idrocarburi, 1999BP Energy Outlook 2030,<br />
London, January 2011<br />
2. BP Statistical Review of World Energy, June 2011<br />
3. BP Energy Outlook 2030, London, January 2011<br />
4. <strong>di</strong> <strong>Cesare</strong>, <strong>Franco</strong>; <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>: A story of two men and the beginning of<br />
the Italian oil Industry, First Break, February 2003, Volume 21<br />
5. <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>: Il Gigante della Val Padana (The Po Valley Giant) Eni’s<br />
Way, 1994<br />
6. <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>; <strong>di</strong> <strong>Cesare</strong> <strong>Franco</strong>: Caviaga a Sessant’anni dalla scoperta.<br />
Industria Mineraria 1-2, 2004<br />
7. <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>; <strong>di</strong> <strong>Cesare</strong>, <strong>Franco</strong>: The Birth of Agip in the Oil World<br />
Landscape, SPE Technical Bulletin 3/2008<br />
12
8. <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>; <strong>di</strong> <strong>Cesare</strong> <strong>Franco</strong>: Alfredo Giarratana a Technician at the<br />
Helm of Agip; SPE Technical Bulletin Special Issue 2009<br />
9. <strong>Gui<strong>di</strong></strong>, <strong>Francesco</strong>; <strong>di</strong> <strong>Cesare</strong>, <strong>Franco</strong>: Twenty First Century: a Natural Gas<br />
Economy, SPE Technical bulletin 3/2010<br />
10. I Giacimenti Gassiferi dell’Europa Occidentale, Roma Accademia dei Lincei,<br />
1959<br />
11. Pallavera, Ferruccio: Storia <strong>di</strong> Cavenago D’Adda, 1989<br />
12. Paoloni, Carlo: Storia del Metano, 1976<br />
13. Pieri, Marco: Cortemaggiore Field – Italy Po Plain, Northern Apennines,<br />
AAPG Special Volumes. Volume TR: Structural Traps VII, Pages 99 -1118 (1992)<br />
14. Pizzigallo, Matteo: L’Agip degli Anni Ruggenti (1926-1932), 1984<br />
15. Porro, Anna; Porro, Pietro: Vita <strong>di</strong> <strong>Cesare</strong> Porro, Geologo. 1985<br />
13