CSET Science, general interdisciplinary foundations - independent foundations study materials
CSET Science, general interdisciplinary foundations - independent foundations study resources

CSET Science, general interdisciplinary foundations - independent foundations key terms

CSET Science, general interdisciplinary foundations - independent foundations · Get comfortable with the vocabulary.

Atomic number

The number of protons in the nucleus of an atom, which uniquely identifies the element. In a neutral atom it also equals the number of electrons.

Related: Mass number, Isotope
Mass number

The total count of protons plus neutrons in one atom's nucleus. It is a whole number written as a superscript beside the element symbol and differs between isotopes.

Related: Atomic number, Isotope
Isotope

One of two or more atoms of the same element that have equal proton counts but different neutron counts, so they differ in mass while sharing nearly identical chemical behaviour.

Related: Mass number, Relative atomic mass
Relative atomic mass

The weighted average mass of an element's atoms compared with one-twelfth the mass of a carbon-12 atom, taking natural isotopic abundance into account. It is dimensionless and rarely a whole number.

Related: Isotope, Mole
Aufbau principle

The rule that electrons occupy the lowest-energy available orbitals first when an atom is built up, giving the familiar 1s 2s 2p 3s filling order and the ground-state configuration.

Related: Electron configuration, Hund's rule
Electron configuration

The arrangement of an atom's electrons among its shells, subshells and orbitals, usually written with superscripts such as 1s2 2s2 2p6. It governs chemical behaviour and position in the periodic table.

Related: Aufbau principle, Hund's rule, Valence electrons
Hund's rule

The statement that electrons fill degenerate orbitals singly, with parallel spins, before any pairing occurs. It explains the unpaired electrons in nitrogen and the paramagnetism of many transition-metal ions.

Related: Electron configuration, Aufbau principle
Restoring force

A force directed toward equilibrium, often proportional to displacement over an explicitly specified linear range; its direction determines the sign in the oscillator equation.

Natural angular frequency

The angular frequency of free oscillation in the chosen ideal model, measured in radians per second and related to period by omega = two pi divided by period.

Damping

Transfer of oscillator energy to other forms through mechanisms such as friction or electrical resistance, changing amplitude and potentially the observed response frequency.

Albedo

The fraction of incident radiant energy reflected by a surface or planetary system, defined for a specified spectral and averaging context.

Top-of-atmosphere energy balance

Accounting for incoming sunlight, reflected sunlight and emitted thermal radiation across the planetary outer boundary; an imbalance represents energy accumulation or loss.

Radiative feedback

A response to a perturbation that changes energy flows and thereby amplifies or reduces the initial temperature response, depending on the process and sign.

Monomers

Small, single units that join end to end in long chains, such as amino acids forming proteins or nucleotides forming nucleic acids. Their structure determines the properties of the polymer built from them.

Related: Condensation reaction, Polymer, Hydrolysis
Polymer

A large molecule made of many similar subunits linked in sequence, such as starch from glucose or a protein from amino acids. Its behaviour depends on chain length, branching and folding.

Related: Monomers, Condensation reaction
Condensation reaction

A joining reaction in which two molecules bond and a small molecule, usually water, is released. It builds glycosidic, peptide and ester bonds when smaller units are assembled into larger biological molecules.

Related: Hydrolysis, Glycosidic bond, Peptide bond
Hydrolysis

A splitting reaction in which a water molecule is used to break a bond between subunits. Digestion of starch, proteins and lipids depends on it, and it reverses condensation.

Related: Condensation reaction, Glycosidic bond, Peptide bond
Glycosidic bond

The bond formed between the hydroxyl groups of two monosaccharides with the loss of water. Its orientation, alpha or beta, changes whether a polysaccharide coils or forms straight strands.

Related: Condensation reaction, Starch, Cellulose
Starch

A storage polysaccharide of alpha-glucose found in plant cells, made of amylose and amylopectin. It is compact, insoluble and easily hydrolysed to release glucose for respiration.

Related: Glycosidic bond, Reducing sugar
Cellulose

A structural beta-glucose polysaccharide forming straight chains associated into strong plant-wall microfibrils. Most animals lack their own cellulase enzymes, while some obtain cellulose digestion through symbiotic microorganisms.

Related: Glycosidic bond, Hydrogen bond
Reducing sugar

A sugar with a free carbonyl group able to donate electrons, so it reduces copper(II) ions to a brick-red precipitate when heated in Benedict's reagent. All monosaccharides and most disaccharides qualify.

Related: Starch, Hydrolysis
Peptide bond

The covalent link formed between the amino group of one amino acid and the carboxyl group of another, releasing water. It is rigid and planar, which constrains how a polypeptide chain can fold.

Related: Condensation reaction, Primary structure, Hydrolysis
Primary structure

The exact sequence of amino acids in a polypeptide, held by peptide bonds. It is coded by DNA and ultimately determines the three-dimensional shape and function of the protein.

Related: Peptide bond, Secondary structure, Tertiary structure
Isostasia

Estado de equilibrio gravitatorio de masas litosféricas respecto al material subyacente, interpretado mediante diferencias de espesor y densidad sin exigir un océano de magma.

Related: Sial, Sima, Litósfera
Discontinuidad sísmica

Superficie interna donde la velocidad de las ondas sísmicas cambia bruscamente, delimitando capas terrestres; las principales son Mohorovičić, Gutenberg y Lehmann.

Related: Moho, Núcleo terrestre, Ondas sísmicas P y S
Moho

Discontinuidad de Mohorovičić, límite entre la corteza y el manto donde las ondas P aceleran de forma brusca; su profundidad varía entre unos 5 y 70 km.

Related: Discontinuidad sísmica, Corteza continental, Manto
Ondas sísmicas P y S

Ondas elásticas generadas por un terremoto: las P son longitudinales y atraviesan sólidos y fluidos; las S son transversales y no se propagan por líquidos.

Related: Discontinuidad sísmica, Núcleo terrestre, Sismógrafo
Núcleo terrestre

Región central de la Tierra, dividida en núcleo interno sólido y externo líquido, compuesta mayoritariamente por hierro y níquel; genera el campo magnético terrestre.

Related: Ondas sísmicas P y S, Geodinamo, Manto
Manto

Región entre corteza y núcleo, compuesta principalmente por rocas silicatadas y mayoritariamente sólida; puede deformarse y transportar calor en escalas geológicas.

Related: Sima, Convección mantélica, Moho
Litósfera

Capa externa rígida de la Tierra formada por la corteza y la parte superior del manto; está fragmentada en placas que se desplazan sobre la astenosfera.

Related: Astenosfera, Placa tectónica, Isostasia