Minerals Report - International Seabed Authority
Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority
Figure 4: Volume density of initial hydrocarbon resources ρV vs. effective capacity coefficient of the basin fill (Kec) For larger objects, it is described by the following equation: ITIPRHC = (e 1.3. 10 -4v – 1) In the second version, the following formula was applied: ρV = e 4.69. e 2.67Kec . Kec . 1.12, INTERNATIONAL SEABED AUTHORITY 492
Where the ITIPRHHc is in Mmtoe (1 t oil = 1,000 m 3 gas); V, in thousands km3; and Kec, is a fraction. The volume-statistical method enables us to give a firstapproximation estimate of hydrocarbon resources in frontier sedimentary basins or their larger parts, for which the theoretical possibility of petroleum generation and accumulation have been established and the sedimentary cover, volume and qualitative characteristics of petroleum potential can be estimated from the available geologic and geophysical data. In this case, the first version of the method is applied (figure 4). Not all reservoir rocks are interpreted as natural reservoirs. For example, permeable seams without component seals above them or thick reservoir units lacking intraformational seals and that are therefore easily drained by formation water are not considered as “effective porosities”. The proportion of natural reservoirs in a sequence or in the basin fill as a whole is characterized by an effective porosity coefficient and depends on the lithology of sedimentary sequences and units. This coefficient ranges in value from 0.001 to 0.3-0.45. The lowest values are usually characteristic of coarse-grained deposits of orogenic complexes; the highest are usually characteristic of biogenic and bioclastic limestones (reefs in particular). The objects of estimation in the volume-balance method of hydrocarbon resource evaluation are large self-regulated equilibrium petroleum–hydrodynamic systems, laterally extending through entire basins or the constituent regions, sags, petroleum accumulation zones, and vertically confined to certain lithostratigraphic units. The petroleumhydrodynamic system (PHDS) volume encompasses the total volume of natural reservoirs present in the object under consideration, and is filled with three interrelated components, oil, gas, and formation water. The ratio between the volume of oil and gas saturated reservoirs (pools) in place and the total PHDS volume is the concentration coefficient (oil, gas, or total hydrocarbon concentration, respectively). Based on a simplified version of the volume-balance method, in the absence of data on temperature, pressure, porosity, and other in-place conditions of pay zones, the initial total-in-place hydrocarbon resources are calculated using the following equation: INTERNATIONAL SEABED AUTHORITY 493
- Page 450 and 451: 3.2. Assumptions made for each kind
- Page 452 and 453: alloys or even manganese ore in the
- Page 454 and 455: ought the nickel price to a top. Th
- Page 456 and 457: Because the metal market economy is
- Page 458 and 459: 14. J. -P. Lenoble (1992), Future d
- Page 460 and 461: 31. J. Francheteau, D. Needham, P.
- Page 462 and 463: 48. J. -P. Lenoble (1996), Les nodu
- Page 464 and 465: 66. J. -J. Prédali and J. -P. Polg
- Page 466 and 467: classification system, Mr. Lenoble
- Page 468 and 469: To recapitulate the sizes and possi
- Page 470 and 471: proposed processing technologies an
- Page 472 and 473: international community is only jus
- Page 474 and 475: Part 2 ISSUES TO BE TAKEN INTO ACCO
- Page 476 and 477: The Secretary-General said that the
- Page 478 and 479: Mr. Nandan pointed out that the nex
- Page 480 and 481: problems would resurface, because i
- Page 482 and 483: prospecting would be more applicabl
- Page 484 and 485: dimensional seafloor massive sulphi
- Page 486 and 487: workshop, in relation to deposit ev
- Page 488 and 489: an economic perspective, including
- Page 490 and 491: sulphides and cobalt-rich ferromang
- Page 492 and 493: CHAPTER 13 PETROLEUM POTENTIAL AND
- Page 494 and 495: structure and filled with sediments
- Page 496 and 497: Basin groups are subdivided into ty
- Page 498 and 499: during the late Mesozoic-Cenozoic s
- Page 502 and 503: ITIPRHC = Vnr φHC γ 103 (Mmtoe),
- Page 504 and 505: Table 1: Offshore (deepwater) initi
- Page 506 and 507: Speaking about particular geographi
- Page 508 and 509: World Ocean, including areas off no
- Page 510 and 511: Table 4: Largest oil and gas discov
- Page 512 and 513: The extremely harsh environment bro
- Page 514 and 515: In other regions of the world, enco
- Page 516 and 517: REFERENCES 1. L.G. Weeks (1971), Ma
- Page 518 and 519: SUMMARY OF PRESENTATION AND DISCUSS
- Page 520 and 521: Dr. Vysotsky said that estimates of
- Page 522 and 523: In Southeast Asia, Dr. Vysotsky spo
- Page 524 and 525: Philippines, and possibly Brazil. W
- Page 526 and 527: and we shall encounter severe deple
- Page 528 and 529: In the 1960's scientists discovered
- Page 530 and 531: Figure 2. Worldwide locations of kn
- Page 532 and 533: methane by bacteria in an anoxic en
- Page 534 and 535: It has been assumed that the struct
- Page 536 and 537: identification of gas hydrate in ma
- Page 538 and 539: ottom simulating reflections (BSR)
- Page 540 and 541: Figure 6: Interpretative plot of hy
- Page 542 and 543: floor have indicated the presence o
- Page 544 and 545: of free gas below the BSR is usuall
- Page 546 and 547: sediment and to provide an indicati
- Page 548 and 549: 6. Harvesting methane hydrates -Som
Where the ITIPRHHc is in Mmtoe (1 t oil = 1,000 m 3 gas); V, in thousands<br />
km3; and Kec, is a fraction.<br />
The volume-statistical method enables us to give a firstapproximation<br />
estimate of hydrocarbon resources in frontier sedimentary<br />
basins or their larger parts, for which the theoretical possibility of<br />
petroleum generation and accumulation have been established and the<br />
sedimentary cover, volume and qualitative characteristics of petroleum<br />
potential can be estimated from the available geologic and geophysical<br />
data. In this case, the first version of the method is applied (figure 4).<br />
Not all reservoir rocks are interpreted as natural reservoirs. For<br />
example, permeable seams without component seals above them or thick<br />
reservoir units lacking intraformational seals and that are therefore easily<br />
drained by formation water are not considered as “effective porosities”.<br />
The proportion of natural reservoirs in a sequence or in the basin fill as a<br />
whole is characterized by an effective porosity coefficient and depends on<br />
the lithology of sedimentary sequences and units. This coefficient ranges<br />
in value from 0.001 to 0.3-0.45. The lowest values are usually characteristic<br />
of coarse-grained deposits of orogenic complexes; the highest are usually<br />
characteristic of biogenic and bioclastic limestones (reefs in particular).<br />
The objects of estimation in the volume-balance method of<br />
hydrocarbon resource evaluation are large self-regulated equilibrium<br />
petroleum–hydrodynamic systems, laterally extending through entire<br />
basins or the constituent regions, sags, petroleum accumulation zones, and<br />
vertically confined to certain lithostratigraphic units. The petroleumhydrodynamic<br />
system (PHDS) volume encompasses the total volume of<br />
natural reservoirs present in the object under consideration, and is filled<br />
with three interrelated components, oil, gas, and formation water. The<br />
ratio between the volume of oil and gas saturated reservoirs (pools) in<br />
place and the total PHDS volume is the concentration coefficient (oil, gas,<br />
or total hydrocarbon concentration, respectively).<br />
Based on a simplified version of the volume-balance method, in the<br />
absence of data on temperature, pressure, porosity, and other in-place<br />
conditions of pay zones, the initial total-in-place hydrocarbon resources<br />
are calculated using the following equation:<br />
INTERNATIONAL SEABED AUTHORITY 493