Keywords Flashcards
accuracy
A set of measurements is accurate if there is only a small systematic uncertainty associated with them. A systematic uncertainty is due to a systematic error which affects each measurement taken in the same way. A representation of the degree of similarity between the true value of a given parameter and a measurement of that parameter.
exponent
also known as the index of power, an expoent is a symbol or number placed above and after another symbol or number to denote the power to which the latter is to be raised.
magnitude
the numerical value of a quantity. magnitude does not take account of any direction associated with the quantity or of whether the quantity has a positive or negative value.
order of magnitude
the approximate value of a numerical quantity expressed as the nearest power of ten.
power of 10
A notation for representing a number as a larger or a smaller number multiplied by a power of ten. For example, in powers of ten notation, 1.234 can be written as 1.234 × 10^3 or 12.34 × 10^2 or 0.123 4 × 10^4 or 123 400 × 10^−2. When the decimal number is below 10, but greater than or equal to 1, for example, 1.234 × 10^3, then this is also known as scientific notation.
precision
a measurement has a high precision if the random uncertainty associated with it is small. a series of high precision measurements will only show a small scatter; low precision measurements will show a larger scatter in the measured values.
prefixes (for units)
a unit prefix is a specifier that immediately precedes and is joined to units of measurement to indicate multiples or fractions of the units, eg kilometre, 100 metres.
scale
a set of divisions used for measurements, as on a ruler. scales are used on the axes of a graph to allow data to be plotted at points corresponding to specific values. for example each cm of the scale on the axis may represent one year, or ten degrees.
scientific notation
A notation that represents any number by expressing it as a number equal to or greater than 1, but less than 10, multiplied by a power of ten. Thus 1.30 × 10^3 is in scientific notation (because 1.3 is between 1 and 10), but 0.130 × 10^4 and 13.0 × 10^2 are not.
significant figures
Uncertainties in measurements mean that measured values should be quoted only with a certain number of digits, and this number of digits is known as the number of significant figures. For example, 10.2 cm is quoted to three significant figures (abbreviated to 3 sig figs) and this means that there is some uncertainty in the final digit (perhaps the value is 10.3 cm or 10.1 cm) but the other two digits are certain. The larger the number of significant figures quoted for a value, the smaller is the uncertainty in that value
si units
An abbreviation for the Système Internationale d’Unités (International System of Units). SI units are used by scientists all over the world to make measurements according to agreed standards. Examples of SI units are the kilogram for mass, the metre for length, and the second for time.
bed
a layer of sedimentary rock within the earth’s crust (the plural, beds, is synonymous with strata)
bedload
sedimentary grains that are transported by rolling along the bed of a river etc by flowing water or air.
cementation
the process of mineral growth in the spaces between the grains of a sediment or sedimentary rock. the resulting cement (commonly quartz or calcite) holds the grains together. cementation is very effective in lithification of sandstones.
chemical weathering
the breakdown of rocks at the earths surface by the chemical action of acidic waters, eg the dissolution of limestones and the decomposition of feldspars to clay minerals. contrast physical weathering.
cleavage
(in rocks) the property of a rock that enables it to split along parallel, planar surfaces. it is developed by the alignment of mica under pressure during low-grade regional metamorphism.
(in minerals) planes of weakness within a mineral along which it tends to break. the planes are related to the arrangement of atoms in the minerals structure.
contact metamorphism
the metamorphism of rocks baked at their contact with a body of magma. affected zones of rock are narrow or localized in extent and occur at relatively shallow depth. contrast regional metamorphism.
crystal
a solid with a definite geometric form reflecting the regular arrangements of its constituent atoms.
deposition
(earth science): the buildup of sediment which occurs on a surface when sediment can no longer be carried, either in solution or as solid grains that are in suspension or part of the bedload.
(chemistry): the direct conversion of a gas (vapour) into a solid without passage through a liquid phase.
dissolved load
material formed by chemical weathering of rocks and carried within a river, stream, lake, sea, etc as dissolved chemicals.
dyke
a narrow vertical sheet of igneous rock which has been intruded into older rocks
erosion
the wearing away of the earth’s surface by the mechanical removal of rock and mineral fragments due to action of flowing water, ice, or wind, and the abrasive action of moving debris or glaciers.
evaporite
a sedimentary rock formed in hot climates by evaporation of salty water to precipitate salts such as the minerals halite (common salt) and gypsum. evaporites may form in enclosed coastal settings.
foliation
the layering in metamorphic rocks formed by banding of minerals or the parallel alignment of platy minerals. a characteristic texture of regionally metamorphosed rocks that is caused by pressure during deformation.
fossil
any evidence of ancient life, usually preserved in sedimentary rocks
fragmental texture
the characteristic appearance of a rock composed of broken fragments of various materials.
igneous rocks
a rock formed by the solidification of molten rock material.
limestone
a sedimentary, composed largely of calcium carbonate (calcite) that if formed typically by the accumulation on the ocean floor of the shells or skeletal remains of marine organisms.
lithification
the collective term for the processes of compaction and chemical change that transform loose sediment into rock.
lustre
the surface appearance of a mineral that depends on the way it reflects light. typical terms used to describe a mineral’s lustre include: glassy, resinous, metallic.
magma
molten (liquid) rock.
metamorphic rocks
a rock that has had its texture and/or mineral composition changed by the action of heat and/or pressure (usually both). a metamorphic rock can be derived from a sedimentary rock, and igneous rock, or a pre-existing metamorphic rock. metamorphic rocks have an interlocking crystalline texture and often display some form of mineral banding or alignment.
mica
a sheet silicate material found in many igneous, sedimentary and metamorphic rocks. muscovite is a pale-coloured variety (silvery-grey) that contains little iron or magnesium. biotite is a dark-coloured variety (dark brown to black) that contains applicable iron and/or magnesium.
mineral
a solid object, formed by natural processes , whose chemical composition lies within narrow limits such that each consituent atom fits together with its neighbours in a regular three-dimensional pattern. because of this, each typ eof mineral forms a crystal with a characteristic shape
ore minerals
minerals which contain useful materials in sufficient abundance that it can be economically viable to mine them
partial melting
the incomplete melting of a rock, during which the minerals with the lowest melting temperatures produce a liquid with a composition different from that of the original unmelted rock. an important cause of magmatic diversity
physical weathering
the mechanical breakdown of rocks into smaller fragments by physical processes at the earths surface such as frost shattering, penetrating roots, thermal expansion and contraction.
pluton
a large (km sized or more) body of igneous rock that was intruded into older rocks
regional metamorphism
the metamorphism of vast volumes of rock, accompanied by deformation that occurs mainly during mountain building at subduction zones and zones of continental collision. regionally metamorphosed rocks are characterized by minerals that have grown in alignment as a result of deformation pressure.
rock cycle
a conceptual system that links the ways in which rocks are continually being created and destroyed by geological processes operating at and below the earths surface.
saltation
a form of bedload transport involving sedimentary grains bouncing along the bottom and ricocheting off other grains
schist
a metamorphic rock with an appearance dominated by highly reflective, crudely aligned flakes of platy minerals, such as mica. schist is formed by regional metamorphism.
sedimentary bedform
the three-dimensional shape of the surface of sedimentary beds, eg ripples or dunes, which relates to the physical conditions under which the sediment has been transported.
sedimentary rock
a rock formed from sediment laid down at the earths surface that has subsequently undergone lifithication by processes such as compaction and cementation. sedimentary rocks usually have a fragmental texture, with individual grains cemented together. some other sedimentary rocks are formed by biological processes (eg coral reefs) or chemical processes (eg evaporites)
silicate minerals
minerals that contain silicon and oxygen
sill
a narrow horizontal sheet of igneous rock that has been intruded into older rocks
slate
A fine-grained metamorphic rock that breaks along smooth, flat, parallel surfaces. Slate is formed by metamorphism at relatively low temperature and pressure of fine-grained, clay-rich sediments. The platy metamorphic minerals in slate (e.g. mica) grow in parallel alignment from clay minerals in response to pressure during deformation.
sorting (of sediments)
A measure of the range of grain sizes present in a sediment or a sedimentary rock. If many grains fall within a narrow range of sizes, the sediment is said to be well sorted. If a wide range of grain sizes is present, a sediment is said to be poorly sorted. The degree of sorting can help to indicate the environment in which a sediment was deposited.
strata
Layers of sedimentary rock. (The singular, stratum, is synonymous with bed.)
suspended load
Sedimentary grains that are transported within flowing water or air, rather than by moving along the sedimentray bed (bedload).
texture
(Of a rock) The description of the particles a rock is made from and of the relationship between them. Texture can be fragmental, when individual mineral grains or rock fragments are cemented together (as in a sedimentary rock) or crystalline, where minerals have grown together so that one crystal interlocks with another (as in an igneous rock or a metamorphic rock).
transportation
The movement of sedimentary material in flowing water, air or ice.
weathering
The degradation of rocks due to physical, chemical or biological action.
ammonite
A member of an extinct group of marine molluscs with a chambered, spiral shell. Ammonites were confined to the Mesozoic.
background radiation
The naturally occurring level of radioactivity at any location.
basalt
A dark-coloured, fine-grained igneous rock, formed as a result of the rapid cooling of mafic magma at the Earth’s surface. Basalt and its intrusive equivalent, gabbro, are the principal components of the oceanic crust. It contains the minerals pyroxene, plagioclase feldspar, and sometimes olivine.
best-fit curve
A curve, or line, drawn on a graph of data on a graph so as to give the best representation of the data as a whole. It need not necessarily go through any of the data points and is drawn in such a way that there are approximately the same number of data points above and below the line.
bivalve
A member of a class of molluscs that has a shell with two valves. In most bivalves, one valve is the mirror image of the other.
brachiopods
Members of the group of marine animals possessing a shell with two valves of dissimilar shape and size. Brachiopods were much more abundant in the Palaeozoic and Mesozoic than today.
corals
Members of a group of marine animals which secrete a calcium carbonate skeleton below anemone-like soft tissue.
daughter isotope
An isotope produced by the radioactive decay of another isotope (the parent isotope).
echinoderms
A type of entirely marine animals with skeletons composed of many interlocking calcite plates. Among echinoderm groups are sea-urchins (echinoids), crinoids and starfish.
eons
The largest unit into which the geological timescale is divided. Earth history consists of two Eons: the Precambrian (or Cryptozoic (hidden life)) and the Phanerozoic (visible life).
eras
Major division of geological time, based on fossil characteristics in sedimentary rocks. The Phanerozoic Eon is also divided into three Eras: Palaeozoic, Mesozoic and Cenozoic.
fault
A plane along which adjacent rocks have moved.
fractional cystallisation
The process by which early-formed crystals become separated from the magma in which they crystallised to leave a magma with different composition. An important cause of magmatic diversity. Compare with partial melting.
gabbro
A coarse-grained, intrusive igneous rock, with the same chemical composition as basalt, formed by the slow cooling of basaltic magma at depth within the Earth. Gabbro and its extrusive equivalent, basalt, are the principal components of the oceanic crust.
gastropods
Members of the group of animals with an unchambered shell which typically coils in an asymmetrical spiral.
granite
A coarse-grained intrusive igneous rock composed largely of interlocking crystals of three types of mineral: quartz, feldspar and mica. It often occurs as large plutons.
graptolites
Extinct (Palaeozoic) marine colonial organisms with individuals housed in tiny cups arranged along one or more branches. Their fossils can look at first sight like lines drawn in pencil on a rock, hence the name meaning ‘writing on rock’.
half-life
The time taken for the number of atoms of a radioactive isotope to be halved by the action of radioactive decay.
isotope
An isotope of a given element has the same number of protons, the same number of electrons, but different numbers of neutrons. An isotope is often written as ‘element- mass number’ (for example, lead-235) or, alternatively, the mass number is written as a superscript to the left of the symbol for the chemical element (for example, 235Pb).
normal fault
A steeply inclined fault in which the movement has predominantly involved the rocks above the sloping fault plane having moved down, relative to the rocks on the other side of the fault plane. Usually associated with tensional deformation (stretching).
nucleus
(Plural: nuclei)
In chemistry and physics, the core of an atom. It contains nearly all of the atomic mass and is positively charged. With the exception of the hydrogen nucleus, which is a single proton, nuclei consist of protons and neutrons.
palaentology
The scientific study of fossils.
parent isotope
An isotope which undergoes radioactive decay, producing a daughter isotope.
periods
Periods Unit of geological time (a subdivision of Era) based largely on the presence of specific fossils in sedimentary rocks. Most geological Periods span several tens of millions of years.
principle of fauna succession
The principle that strata contain particular assemblages of fossils in a definite succession, with each stage in this succession representing a particular span of geological time
principle of superposition
The principle that, because younger sediments are deposited on older sediments, an individual rock layer is younger than the one beneath it and older than the one above it. Unless the strata have been disturbed or overturned, the oldest layer lies at the bottom.
radioactive decay
The spontaneous transformation of one isotope (the parent isotope) into another isotope (the daughter isotope), accompanied by the emission of some energy.
radioactivity
The spontaneous transformation of one isotope (the parent isotope) into another isotope (the daughter isotope), accompanied by the emission of some energy.
reverse fault
A steeply inclined fault in which the movement has predominantly involved the rocks above the sloping fault plane having moved up, relative to the rocks on the other side of the fault plane. Usually associated with the rocks being compressed sideways.
stratigraphic column
The sequence of geological time divisions (Eons, Eras and Periods) arranged in chronological order, with the oldest at the base
stratigraphy
The study of strata and their relationships in time and space. Sequences of strata have long been used to establish a generalized geological succession — the stratigraphic column — made up of geological eras and periods, which when given absolute dates forms the geological time-scale.
trilobite
A member of an extinct marine group of arthropods confined to the Palaeozoic. Trilobites had an external skeleton, divided lengthways into three lobes, that was shed periodically during growth.
unconformity
The absence of strata from a particular time interval in a certain region, due either to non-deposition, or to erosion of any sediment that had been deposited. The term also refers to the actual contact between unconformable rocks. An unconformity is often recognized by a difference in the angle of layering in adjacent sets of strata.
uniformitarianism
The concept, fundamental to geology, that geological processes which operate today also operated in the past. It is the basis of the frequently quoted maxim ‘the present is the key to the past’.
absolute plate motion
The movement of a tectonic plate relative to a fixed reference point such as a mantle plumes.
abyssal plain
The part of the ocean floor that lies between 4 km and 6 km below the surface. Abyssal plains are generally flat and they make up the major part of the ocean floor.
active continental margin
A type of convergent plate margin where oceanic lithosphere is subducted beneath a continental margin, such as exists along the west coast of South America. (See also ocean/continent subduction zone.)
asthenosphere
A weaker, more easily deformed region of the mantle that is below the lithosphere.
bathymetry
The measurement of depth of water in seas, essentially the topography of the seabed.
biomodal distribution
A distribution of data that exhibits two distinct peaks (i.e. has two modes).
body waves
A seismic wave that travels through the interior of the Earth. There are two types of body wave: a P wave and an S wave.
conservative plate boundary
A type of plate boundary where the plates move laterally past each other without convergence or divergence.
continental drift
The movement of continents over the surface of the Earth through geological time.
convergent plate boundary
A type of tectonic plate boundary where the plates move towards each other, also known as a subduction zone.
core
The central part of the Earth, composed mainly of iron. The outer core is liquid, the inner core is solid.
cross section
A representation of a vertical slice through the Earth to show an aspect of the subsurface.
crust
The upper seismic layer of the Earth. The crust has a relatively low density and low seismic wave speeds. It is about 7 km thick under oceans (oceanic crust), and 20–80 km thick (averaging 35 km) under continents (continental crust).
divergent plate boundary
A type of tectonic plate boundary where the plates move apart from one another, also known as a mid-ocean ridge (or spreading centre).
earthquake magnitude
A quantitative measure of the size of an earthquake, obtained from the amount of energy released.
epicentre
The point on the Earth’s surface directly above the focus of an earthquake.
focal depth
The depth of the focus of an earthquake below the Earth’s surface.
focus
The location (point of origin) of an earthquake. This is usually well below the Earth’s surface. (Plural = foci)
fracture zone
A liner deep sea fault that transects and displaces a mid ocean ridge.
full spreading rate
In plate tectonics, the rate at which two points lying either side of an oceanic ridge crest diverge.
GPS
Global Positioning System. A system of fixing the location of a point on the Earth’s surface with reference to a configuration of satellites.
graben
A fault edged, downthrown block of crust that forms a linear valley.
half spreading rate
In plate tectonics, the rate at which a single point on one side of a ridge moves away from the oceanic ridge crest.
hotspot
A volcanic area above a shallow region of anomalously hot mantle.
hotspot track
A chain of active and extinct volcanoes that have formed on a moving plate above a stationary hotspot.
hydrothermal circulation
The circulation of hot fluids in the vicinity of a magma body for example at a mid-ocean ridge.
hypsometric plot
A histogram showing the relative proportions of the Earth’s surface area at different altitudes and depths.
inclined seismic belt
An inclined zone of earthquakes (also known as a Wadati Benioff zone) extending several hundred kilometres into the Earth at a subduction zone. A Wadati–Benioff zone defines the position of a cold subducted slab of lithosphere.
island arc
The chain of volcanic islands on the overriding plate at a subduction zone where two plates of oceanic lithosphere converge. An island arc lies parallel to an ocean trench. (See also ocean/ocean subduction zone.)
lava
Molten igneous rock (magma) that flows over the Earth’s surface. The term lava flow can also be used to describe the body of rock formed after the molten lava has cooled and solidified.
lithospheric plate
An area of lithosphere, the edges of which are defined by a seismic zone. This is usually abbreviated to plate. Also known as a tectonic plate.
mantle
The layer of the Earth between the crust and the core .
mantle plume
A localised area of anomalously hot mantle that rises due to buoyancy. Mantle plumes may give rise to hotspots when they melt at shallower levels.
mid-ocean ridge
A broad ridge a few thousand kilometres across and 2– 3 km high on the ocean floor, extending for many thousands of kilometres. Mid-ocean ridges do not always lie in the centres of oceans. A mid-ocean ridge is a divergent plate boundary.
ocean/continent subduction zone
A type of convergent plate margin where oceanic lithosphere is subducted beneath a continental margin, such as exists along the west coast of South America. (See also ocean/continent subduction zone.)
ocean/ocean subduction zone
The chain of volcanic islands on the overriding plate at a subduction zone where two plates of oceanic lithosphere converge. An island arc lies parallel to an ocean trench. (See also island arc.)
orogeny
The processes and/or sum of events during which a mountain belt is formed, e.g. the Caledonian Orogeny. An orogeny usually involves the convergence of lithospheric plates, causing folding, faulting, metamorphism and igneous activity. Also referred to as continental collision.
plate boundary
The edge of a tectonic plate, where it interacts with a neighbouring plate.
plate tectonics
The theory that the Earth’s surface is composed of a number of lithospheric plates that can move around. It combines evidence for continental drift with the mechanism of sea-floor spreading, so providing an explanation that links previously unrelated features of the Earth, such as the distribution and shape of mountain belts, the location of seismic zones, volcanism and the shape of the ocean floor.
polarity of subduction
The direction of subduction at a convergent plate boundary.
pyroclastic flow
A flow of materials from a pyroclastic eruption down the side of a volcano.
seismic waves
A wave in the Earth, generated by an earthquake (or an explosion).
seismogram
A paper record of ground motion due to a seismic wave recorded by a seismometer. Sometimes referred to as a seismic trace or seismograph.
seismology
The study of earthquakes.
seismometer
An instrument that measures and records motion of the ground surface.
slip
The relative displacement to the two sides of a fault plane which were originally coincident.
SONAR
An acoustic survey system which uses the reflection of high frequency sount waves from a surface to image its surface. Frequently deployed from ships to map out the surface of the seabed. (An acronym derived from sound navigation and ranging.
subduction
The process by which an oceanic lithospheric plate sinks beneath another plate of either oceanic or continental character.
subduction zone
A region of the Earth where oceanic lithosphere subducts (sinks) beneath the edge of another lithospheric plate at a convergent plate boundary.
surface waves
A seismic wave that travels at and near the surface of the Earth.
s wave (shear wave)
A type of seismic wave; the slower type of body wave. This is a transverse wave in which the rock moves at a right angle to the direction of wave motion.
tectonic plates
An area of lithosphere, the edges of which are defined by a seismic zone. This is usually abbreviated to plate. Alo known as a lithospheric plate.
topography
Used in this context to describe the range and distribution of elevation of the surface of the Earth.
trench (submarine)
An elongate depression on the ocean floor that runs parallel to an active continental margin or to an adjacent chain of volcanic islands (island arc). Oceanic trenches are up to 11km deep, typically 50-100km wide and may be thousands of kilometres long.
triangulation
Locating a point with reference to three survey points at a known distance of separation.
tsunami
Ocean waves caused by movement of the ocean floor by an earthquake under the ocean. Tsunami can travel great distances across an ocean. They have a small wave height in the deep ocean, but increase in height significantly when they reach a coast, and can be very destructive.
vector
An arrow that contains information about direction and magnitude. Vectors of tectonic plate motion show both direction and speed which is normally indicated by length.
volcanic ash
Fine (<2mm) solid particulate material erupted from a volcano.
volcano
A naturally occurring vent or fissure at the Earth’s surface through which molten, solid and gaseous materials erupt.
watadi beniof zone
An inclined zone of earthquakes extending several hundred kilometres into the Earth at a subduction zone. A Wadati–Benioff zone defines the position of a cold subducted slab of lithosphere.
anthropocene
A proposed epoch relating to significant human impact on the geology and ecosystems on Earth
aquifier
Undeground, water-saturated permeable rock or unconsolidated materials
assimilation
The conversion of nutriment into a useable form that is incorporated into the tissues and organs or an organism. Examples of assimilation include photosynthesis in plants in which CO2 and water are converted into carbohydrates, or nitrogen fixation by bacteria in which gaseous N2 is converted into ammonia. Animals assimilate food by eating plants or each other.
atmosphere
A layer of gases surrounding a planet or other body held in place by the gravity of that body
atom
An atom is the smallest constituent unit of matter that has the properties of a chemical element; each chemical element is characterised by a different type of atom. Atoms are roughly 10–10 m across.
biogeochemical cycle
A pathway (or pathways) by which a chemical substances moves through both the living (biosphere) and non-living (lithosphere, atmosphere, and hydrosphere) components of Earth. They occur because chemical elements on Earth are recycled, unlike energy.
biomass
The amount of living material, usually in some area or volume. If quantified, marine biomass is often expressed in grams of carbon per unit area of sea-surface (or unit area of sea-bed, in the case of benthic ecosystems), i.e. gC m–2. Biomass is also used to refer to the matter of which an individual organism is composed.
biosphere
The part of the Earth inhabited by life.
carbonate counter pump
A sub-cycle of the carbon cycle, whereby carbon dioxide (CO2) reacts with water to form carbonic acid and bicarbonate. The carbonate pump allows the ocean to take up much more CO2 than if CO2 just dissolved in water
carbon cycle
The global transfer of carbon between various carbon reservoirs in the environment, involving both living organisms (biological cycle) and the non-living environment, such as soil, water, rocks and air (geochemical cycle).
carbon footprint
The amount of carbon dioxide (or carbon dioxide equivalent for other greenhouse gases) released into the atmosphere as a result a particular acivity.
closed system
A physical system in which no matter is exchanged with its surroundings.
condensation
The process whereby a substance changes from a gas to a liquid, e.g. water changes from water vapour to liquid water.
decomposition
The gradual disintegration of dead organic matter. Some decomposition occurs through physical factors such as wind and water, but it is mostly achieved by bacteria. See detritivore.
denitrification
A process, facilitated by microbes, in which nitrate is reduced through a series of intermediate products to ultimately form nitrogen gas (N2)
discharge
The flowing of a liquid (or gas) from where it has been confined.
eutrophication
The enrichment of an environment, often a water body, with nutrients. It can refer to the enrichment of an environment with excessive amounts of nutrients.
evaporation
The process whereby a substance changes from a liquid to a gas, e.g. liquid water evaporates to form water vapour.
evotranspiration
The sum of both the evaporation from the soil and other surfaces and transpiration from plants, which describes the process by which water is transferred from land and water surface to the atmosphere.
fixation
The process in which a substance is changed from the gaseous or solution phase, into a useable stable form, as in carbon dioxide fixation or nitrogen fixation.
flow
The movement of a substance in a continuous stream or current.
flux
A process of flowing or change.
gas exchange
The biological process by which gases move passively by diffusion across a surface. Gas exchange occurs between the air and cells inside a leaf in plants, and between air and blood in the lungs as examples.
hydrosphere
The part of the Earth that includes water, either in or on the surface of the Earth (including the oceans, rivers, lakes, ice), together with water in the atmosphere.
lithosphere
The rigid outer layer of the Earth, which includes the crust. It is made up of plates that may be oceanic, continental or both.
nitrate
The anion NO3− found in compounds such as sodium nitrate NaNO3 or potassium nitrate (saltpetre) KNO3.
nitrification
The aerobic process in which ammonia is oxidised to nitrite and nitrate by the nitrifying bacteria.
nitrite
The anion NO2-, found in compounds such as sodium nitrite NaNO2 or potassium nitrite KNO2
nitrogen fixation
The conversion of nitrogen gas (N2) into ammonia (NH3) or other nitrogen-containing molecules that can be used by living organisms (the reverse process to dintrification).
organic carbon
Carbon in compounds found in living things or the remains of living things. For example, plants produce simple organic carbon compounds through photosynthesis.
organic carbon pump
The biologically-driven transformation of carbon dioxide into organic carbon materials, their deposition into deep sea waters and sediments in the ocean, and their decomposition at depth
percolation
The process of a liquid slowly passing through a filter or porous material.
phases (chemical)
Physically distinctive forms of matter, such as a solid, liquid or gas.
photosynthesis
The process whereby plants utilise carbon dioxide, water and light energy from the Sun to manufacture organic compounds (carbohydrates).
pool
In a global cycle (e.g. water or carbon), pools provide a means of classifying cycled material by the type of location, irrespective of its real geographical location. For example, pools in the carbon cycle include the plants and fossil fuel deposits.
precipitation
A collective term referring to all the forms in which water can fall from the atmosphere onto the Earth’s surface (as rain, snow, sleet or hail).
pump
In biogeochemical cycles, a pump describes a process which drives fluxes and the name often indicates the main driver of the pump (i.e. a biological pump includes reactions driven by lifeforms).
reservoir
In a global cycle (e.g. water or carbon), reservoirs provide a means of classifying cycled material by the type of location, irrespective of its real geographical location. For example, reservoirs in the water cycle include the atmosphere, the oceans, ice and snow.
residence time
The average length of time that a molecule remains in a particular reservoir.
run-off
Something that drains or flows off, such as rain that flows off land into streams.
solution pump
Also known as the solubility pump this is the absorption or release of CO2 by water, following changes in solubility of gaseous CO2
store
In a global cycle (e.g. water or carbon), stores provide a means of classifying cycled material by the type of location, irrespective of its real geographical location. For example, reservoirs in the water cycle include the atmosphere, the oceans, ice and snow.
system
This is the part of the world in which there is a particular interest. In biology it is often a set of components working together as parts of an interconnecting network. In the context of a chemical reaction, it could simply be the contents of a reaction mixture.
terrestrial
Related to land or the planet Earth, but also refers to organisms that live on land or processes that occur on land instead of in water.
water cycle
The continuous circulation of water on Earth between ocean, atmosphere, land, biological organisms, etc. It involves water changing its state between solid (ice), liquid (water), and gas (water vapour).
autotroph
An organism that makes its own carbon-based material starting with carbon dioxide. An autotroph is also known as a primary producer. Almost all plants are autotrophs; they convert carbon dioxide into carbon based material by photosynthesis.
carnivores
An organism that obtains its carbon-based materials by consuming living or recently killed animals, either in whole or in part, i.e. a type of heterotroph.
carrion
The decaying flesh of dead animals.
commensalism
An association between two species in which one benefits and the other derives neither benefit nor harm.
community
Considered as a whole, the various populations of organisms (micro-organisms, plants and animals) that inhabit a particular area, and interact together.
competition
An interaction between organisms or species in which both the organisms or species are harmed. Limited supply of at least one resource (such as food, water, and territory) used by both can be a factor.
consumers
An organism that cannot manufacture its own carbon-based materials starting from carbon dioxide and therefore feeds on other organisms. Also known as a heterotroph. Compare with producer.
dcomposers
An organism which breaks down dead organisms through decomposition, including fungi and bacteria.
detritivores
Animals that feed primarily on detritus, i.e. organic debris from plants and animals.
ecosystem
All the (interdependent) communities of organisms in a particular geographical area, plus the physical environment that they inhabit.
ecosystem balance
A state of dynamic equilibrium within an ecosystem in which genetic, species and ecosystem diversity remain relatively stable, subject to gradual changes through natural succession.
food chain
A linear sequence of organisms in which each organism (or group of organisms) is food for the next member in the sequence.
food web
A schematic representation of the feeding interactions within an ecosystem or community. Food webs contain multiple food chains and one organism can have more than one food source, thereby linking food chains together.
guild
A guild is any group of species that exploit the same resources, or who exploit different resources in related ways.
habitat
The physical and biological environment in which an organism lives.
herbivores
An organism that obtains its carbon-based materials by consuming living plant (or fungal) material, i.e. a type of heterotroph.
herbivory
The act of eating plants and a herbivore is an animal that eats plants
heterotroph
An organism that cannot manufacture its own carbon-based materials starting from carbon dioxide and therefore feeds on other organisms. A heterotroph is also known as a consumer. Compare with autotroph.
individual
A single, separate organism distinguished from others of the same kind.
mutualism
An association between two species in which both partners confer some benefit.
omnivores
Organisms which obtain their food from both other animals and plants.
parasitism
A non-mutual association between species, where one species, the parasite, benefits at the expense of the other, the host, often without killing the host. The parasite is often much smaller than its host.
population
A group of organisms belonging to the same species which live in a defined place.
predation
One animal feeding upon another.
primary consumer
An organism that obtains its carbon-based materials by consuming another organism either whole or in part, either living or dead, and is the first heterotrophic species in a food chain. These organisms consume plant material.
primary producer
An organism that makes its own carbon-based material, starting from carbon dioxide. A producer is also known as an autotroph. Almost all plants are producers; they convert carbon dioxide into carbon based material by photosynthesis.