
|
Information about Oil Shale in Jordan There are extremely large proven and exploitable reserves of oil shale in the central and north-western regions of the country. The proved amount of oil shale in place is reported by the WEC Member Committee to be 40 billion tons; proved recoverable reserves of shale oil are put at 4 billion tons, with estimated additional reserves of 20 billion tons. Jordanian shales are generally of quite good quality, with relatively low ash and moisture content. Gross calorific value (7.5 MJ/kg) and oil yield (8-12%) are on a par with those of western Colorado (USA) shale; however, Jordanian shale has exceptionally high sulphur content (up to 9% by weight of the organic content). The reserves are exploitable by opencast mining and are easily accessible.
The eventual
exploitation of what is Jordan's only substantial fossil fuel resource
to produce liquid fuels and/or electricity, together with chemicals
and building materials, would be favoured by three factors - the high
organic-matter content of Jordanian oil shale, the suitability of the
deposits for surface-mining and their location near potential consumers
(i.e. phosphate mines, potash and cement works). Oil Shale (Bituminous Marl) refers to sedimentary rocks mostly carbonates to chalk marl and shale contain immature organic matters, when it is heated to above 500°C, it produces oil and gas. The Jordanian oil shale are naturally bituminous marls of varying shade of brown, grey or black. The investigations of the potential of bituminous rocks as a possible source for producing oil by retorting or for generating electricity by direct combustion is of first priority for Jordan. Oil shale is the major indigenous fossil-fuel in Jordan: its predicted reserves, of about 5 x 1010 tons, should be sufficient to satisfy Jordan's energy-requirements for several centuries. Using the oil shale as the input fuel, a multipurpose production process (i.e. retorting, electricity generation, thermal water-desalination, chemicals production as well as mineral extraction) could achieve high utilization-factors of both its chemical and energy potentials.
Until a few years ago the development of Jordan's oil shale reserves would have been economically unviable because of the high extraction and processing costs of shale oil. However, a breakthrough in oil-from-shale technology has made the extraction and processing costs of shale oil competitive with conventional crude oil, particularly when taking into account the cost of exploration for conventional oil. The economic benefits for Jordan's economy and its balance of payments make the development of shale oil worthwhile. This will enable Jordan to, eventually, become self-sufficient in oil and to recoup its investment within an estimated period of 8-10 years. It will also save Jordan's balance of payments an estimated $1.622 bn, being Jordan's projected oil import bill in 2010. There will also be the added bonus that Jordan could become a net exporter of shale oil. This will enhance Jordan's oil security well into the next century.
Oilshale deposited mostly within the lower part of the Muwaqqar Chalk Marl Formation (Campanian-Maestrichtian). The Formation consists of limestone, marl, shales and phosphates.
Location There are 23 known surface and near surface deposits, eight of which namely El-Lajjun, Sultani, Jurf Ed-Darawish, Attarat Um El-Ghudran, Wadi Maghar, Siwaga, Khan El-Zabib and El-Thamad were investigated in different levels. The major deposits of commercial scale interest are located south of Amman in central Jordan and are easily accessible from the desert highway between Amman and Aqaba. These are: -
ElLajjun is located at about 100 kms south of Amman, between Qatrana and Karak city. Sultani is located at about 115kms south of Amman just adjacent to the desert highway. Jurf Ed- Darawish is located 145kms south of Amman and near Jurf EdDarawish town. Attarat Umm Ghudran is located approximately 35 kms east of Qatrana. Wadi El Maghar is located approximately 40 kms south east of Qatrana. El-Thamad is located 45km south of the capital Amman.
Natural Resources Authority (NRA) has carried out extensive geological studies to determine the oil shale reserves at El-lajjun, and Sultani deposits. In 1979, BGR evaluated oil shale deposits in central Jordan (El-Lajjun, Jurf Ed-Darawish, El-Hisa and Sultani deposits). In 1980, a prefeasibility study by Technoprom export to determine the feasibility of direct burning the oil shale in a 300-400MW conventional combustion unit. In 1986, the consortium concluded an undated prefeasibility study for a 50000 bb1/day retorting complex including CFB and upgrading units. In 1985, an agreement was signed with ChinaPetro Chemical International Company to carry a proving test in order to determine whether a Fushuntype retort is technically feasible for processing El-Lajjun oil shale. The test proved the technical viability of extracting shale oil from El-Lajjun oil shale. In 1987, Jordan Electricity and Ministry of Energy and Natural Resources commissioned direct combustion studies using Sultani oil shale deposit with BBC, Engineering Combustion Lummus Canada and Puro-Power (USA). The performance tests conducted on Sultani oil shale have demonstrated that Sultani oil shale is suitable as fuel. Jordanian oil shale kerogen was studied by solvent extraction with chloroform and two mixed solvents - methanol/acetone/chloroform (M/A/C) and CS2/N-methyl-2-pyrrolidinone (CS2/NMP). It was found that the extraction yield and the composition of the extracts are quite different in the case of different solvents. Such results suggest that Jordanian oil shale kerogen structure is characterized by three-dimensional networks cross-linked by covalent bonds and noncovalent bond intermolecular interactions. The nonpolar aliphatic and aromatic fractions are trapped or "protected" in these networks. The mixed solvents M/A/C and CS2/NMP have stronger ability to disrupt these noncovalent bond interactions and give higher extraction yields. This may explain why, as the extraction yield increases, the amount of nonpolar saturated and aromatic fractions also increases. |