Oil and gas

uses/properties/intro

oil market

source rocks

transport

reservoir rocks

seal rocks

traps

exploration

production

environmental

uses

properties

plastics

fertilisers

energy production

API - American Petroleum Index

hydrocarbons and other organic compounds

index of how heavy a crude oil is

use examples

50s

30s-40s

below 15

average constituents of fuel

lightest chains

shortest hydrocarbons

most volatile

heaviest and longest chains

need cracking for commerical

heavy and dark

bitumin

mostly liquid

solid

gas-liquid

construction

coal

road surfaces

planes tend to use kerogen

measurement of oil is in barrels like whiskey barrels

Source rocks generate oil and gas

contain organic-rich materials

how are oil and gas generated?

types of kerogen

type 1

type 2

type 3

algae

phyto and zooplankton

terrestrial plants

once oil and gas are generated they start to migrate upwards towards surface

they can only migrate through porous rocks

e.g. organic rich mudstones

must contain at least 1% total organic carbon by weight

often sedimentary but not always

seal rocks stop migration of oil and gas out of reservoir rock

often halites, anhydrite

must be impermeable, no pores so fluids can't move

geophysics seismic magnetic airborne

must have anticline structure to trap oil and gas

global warming by burning fossil fuels produces CO2

diesel, fuel, hydrocarbons

cycloalkanes, alkanes, arenes

compounds with SON

refineries are designed for specific oil compositions

different oils different composition based on organic material derived from and changes over time

based on specific gravity index

hard to process, lots of waste

more energy to produce light chains

not energy efficient or cost effective

ideal for refinaries

clear

starts to evaporate at very low temperature

easier to extract and more commercial uses

disel in trains and ships - heavy oil

gasoline - petrol - lighter/shorter

bitumen for roads is longest

90 million barrels a day

renewables starting to replace additional oil we use every year

current oil price 85 dollars a barrel

companies can influence price

free market - oil sold and traded, price controlled by supply and demand

best 5-10% TOC to generate larger volume of oil

potential begins with first life

oil and gas production controlled by rate of organic productivity vs organic matter degradation

destruction

preservation

burial

production

mostly generated by algae and bacteria

lacking oxygen

generally close to land

shallow, warm water

close to rivers - bring nutrients

most organic matter eaten, oxidised on surface

enclosed basin no ocean currents to sweep away source rock

low oxygen preserve organic matter

algae die and fall to seabed

aerobic organisms can't survive

animals can't eat organic matter

can't carry out degradation

sediment deposition

not too much as this dilutes organic content

moving rock away from oxygen is better to reduce bacteria

oil shales

oil and gas

gas - coals

lipid rich

lipid rich

marine source rocks

humic

organic matter maturation

maturation

increases overburden pressure causing temperature to increase

temp determines organic matter products

must be buried deep enough for temp to be hot enough to generate oil

temp increases with depth due to heatflow from centre of earth

40-80 kerogen window- anerobic and abiotic breakdown of organic matter

oil window 100 to 150 degC breakdown C bonds and form short chains

gas window 150-200 depleting H

over 200 - overmature

lose H2O, CH4, Co2, O

peak oil C used to make hydrocarbons

can be generated for longer once C starts to run out

metagenesis

diagenesis

metagenesis

low O:C atomic ratio, high H:C atomic ratio

high O:C atomic ratio, low H:C atomic ratio

drives

pressure drives explusion of generated hydrocarbons

buoyancy, gravity, less dense than surrounding fluid

travel as microscopic bubbles of oil and gas

some reaches surface and evaporates

oil displaces water

bigger pores better, more space for oil to fill

levels of porosoity

secondary porosity controlled by diagenesis (compaction, dissolution, cementation)

primary porosity controlled by settling and energy at deposition

permeability

ability of oil to flow between pores

click to edit

sandstone/limestone

can't be too compacted or cemented

fractured granite/basalt

impossible to fracture - ductile

biggest reservoirs sealed by salt

most reservoirs sealed by mudstone

microporosity

structural or stratigraphic convex-up

gas less dense than oil so rises up

water below - everything in subsurface contains water

oil-water contact

gas-oil contact - contacts controlled by buoyancy - flat

drilling wells to provide view of the subsurface

routine borehole length > 8km

oil and gas fields

upstream, downstream, new energies

oil spills