The historical beginnings of petroleum science
$this->bbcode_second_pass_quote('', 'T')he history of petroleum science might be considered to have begun in the year 1757 when the great Russian scholar Mikhailo V. Lomonosov enunciated the hypothesis that oil might originate from biological detritus. Applying the rudimentary powers of observation and the necessarily limited analytical skills available in his time, Lomonosov hypothesized that “... 'rock oil' [crude oil, or petroleum] originated as the minute bodies of dead marine and other animals which were buried in the sediments and which, over the passage of a great duration of time under the influence of heat and pressure, transformed into ‘rock oil’.” Such was the descriptive science practiced in the eighteenth century by Lomonosov and Linnaeus.
The scientists who first rejected Lomonsov’s hypothesis, at the beginning of the nineteenth century, were the famous German naturalist and geologist Alexander von Humboldt and the French chemist and thermodynamicist Louis Joseph Gay-Lussac who together enunciated the proposition that oil is a primordial material erupted from great depth, and is unconnected with any biological matter near the surface of the Earth.
Thus both ideas were delivered with powerful pedigrees: the wrong biological notion having been put forward by the greatest Russian scientist of his time; and the abiotic proposition approximately a half century later by, respectively, two of the greatest German and French scientists.
Historically, the first scientific repudiation Lomonosov’s hypothesis of a biological origin of petroleum came from chemists and thermodynamicists. With the nascent development of chemistry during the nineteenth century, and following particularly the enunciation of the second law of thermodynamics by Clausius in 1850, Lomonosov’s biological hypothesis came inevitably under attack.
The great French chemist Marcellin Berthelot particularly scorned the hypothesis of a biological origin for petroleum. Berthelot first carried out experiments involving, among others, a series of what are now referred to as Kolbe reactions and demonstrated the generation of petroleum by dissolving steel in strong acid. He produced the suite of n-alkanes and made it plain that such were generated in total absence of any “biological” molecule or process. Berthelot’s investigations were later extended and refined by other scientists, including Biasson and Sokolov, all of whom observed similar phenomena and likewise concluded that petroleum was unconnected to biological matter.
During the last quarter of the nineteenth century, the great Russian chemist Dmitri Mendeleev also examined and rejected Lomonosov’s hypothesis of a biological origin for petroleum. In contrast to Berthelot who had made no suggestion as to where or how petroleum might have come, Mendeleev stated clearly that petroleum is a primordial material which has erupted from great depth. With extraordinary perception, Mendeleev hypothesized the existence of geological structures which he called “deep faults,” and correctly identified such as the locus of weakness in the crust of the Earth via which petroleum would travel from the depths. After he made that hypothesis, Mendeleev was abusively criticized by the geologists of his time, for the notion of deep faults was then unknown. Today, of course, an understanding of plate tectonics would be unimaginable without recognition of deep faults.



