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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 />

3


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 />

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