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Research draft

weathering

vr.tr.weathering · ACT.ACT

Enable an agent to recognise weathering, assess how it is altering exposed rock or mineral material, and judge appropriate investigation or intervention.

Thing Registry Activities and processes

Research draft, second pass

A second pass drafted this model: the structure a model of this thing needs, and what is known about it in the world. The line under this one says how the second half was obtained - researched against sources, or recalled without web access, in which case nothing here was read anywhere and every claim is a lead to verify. Unreviewed either way.

recalled by Codex without web access - no source was read

Researched by: Codex

Purpose and description

Enable an agent to recognise weathering, assess how it is altering exposed rock or mineral material, and judge appropriate investigation or intervention.

Weathering is the physical disintegration and chemical alteration of rocks, minerals, and other materials at or near Earth's surface through interaction with water, air, organisms, and changing environmental conditions, without requiring transport of the resulting material.

It can be Identify a candidate weathering occurrence and distinguish it from transport, staining or inherited alteration.; Compare competing mechanism explanations against material, exposure and product evidence.; Select measurements that separate alteration extent, current activity and changes in material performance.; Track weathering fronts, surface change and product formation through time.; Evaluate whether drainage, exposure reduction or another intervention addresses the supported mechanism.; Refer consequences involving slope stability, structural integrity or water chemistry to the appropriate neighbouring model..

Distinguishing features

A weathering instance requires evidence of material disintegration or alteration; exposure to rain, sunlight or temperature variation alone is insufficient.

Weathering can produce loosened or altered material without transporting it; subsequent removal is recorded as erosion even when both processes occur together.

Physical weathering is supported by fragmentation or cracking without requiring mineral transformation, whereas chemical weathering requires evidence of dissolution or chemical change.

Biological presence counts as a weathering contribution only when an organism's activity can be connected to material disruption or alteration.

Inherited alteration must be distinguished from currently active weathering using exposure history, fresh alteration features or observations through time.

Scope

+ Physical disintegration and chemical alteration occurring in place

+ Biological contributions to physical and chemical weathering

+ Susceptibility associated with mineral composition, texture, fractures and exposure

+ Weathering products, alteration profiles and changes in material properties

+ Evidence for active mechanisms, progression and consequences

+ Monitoring and management of weathering in natural rock and mineral-based built materials

- Erosion, sediment transport and deposition as processes in their own right

- Regional soil formation and soil classification beyond their weathering components

- Metamorphism and hydrothermal alteration outside the adopted surface-process boundary

- Atmospheric weather and climate systems except as exposure conditions

- General deterioration of polymers, coatings and other manufactured materials

- The social and health concept of weathering

Characteristics

Parent material and reference condition
Rock or mineral identification linked to mineralogy, texture and a comparatively unweathered reference Weathering cannot be assessed reliably without distinguishing original material properties from subsequent changes.
Supported weathering mechanisms
Physical disintegration; chemical alteration or dissolution; coupled processes; unresolved, with biological contributions recorded separately Mechanism attribution determines which measurements and interventions are relevant.
Exposure and access pathways
Connections to water, air, organisms and salts through surfaces, pores and fractures Reactants and stresses must reach susceptible material for the proposed process to operate.
Weathering extent
Alteration depth in mm or m, affected volume fraction, or a named material-specific grading scheme Extent identifies how much material is affected without assuming that surface appearance represents the interior.
Material-property change
Change relative to a stated reference in porosity, permeability, strength or mineral composition, with method-specific units Visible alteration and functional deterioration need not progress together.
Progression rate
Surface recession in mm/year, mass change in g/m²/year, or reaction flux in mol/m²/year, with measurement period and attribution Different rate measures capture different processes and must not be treated as interchangeable.
Present activity
Active during observation; episodically active; no activity detected during observation; unresolved An extensively weathered material may show little measurable change during the current observation period.
Weathering products and their fate
Links to residual fragments, secondary minerals, dissolved constituents and their retention or export Products help identify mechanisms and connect weathering to neighbouring transport and soil processes.

Also called

rock weatheringtafonispace weatheringBrunificationsilicate weatheringchemical weatheringphysical weatheringhoneycomb weatheringspheroidal weatheringbiological weatheringhaloclastywedging

Where this came from

wikidata · CC0 1.0

Drafted structure

Bundle to layer to finding to question, as the second pass will find it: 6 bundles · 11 layers · 16 findings · 26 questions.

Weathering identity and boundaries Establishes the intended sense of weathering and identifies the material transformation being modelled.

The name can cover different subjects, while geological weathering often occurs alongside processes that must be distinguished from it.

Sense and instance

Defines the geological process sense and the evidence needed to recognise an occurrence.

Alteration in place

Record the affected parent material and evidence that it has disintegrated or changed chemically at the weathering location.

  1. Does this registry entry intend geological weathering, and what operational definition will be used? definition
  2. What observation demonstrates disintegration or chemical alteration rather than exposure alone? measurement

Adjacent processes

Separates weathering from transport and other forms of material alteration.

Process partition

Attribute local alteration, material removal and inherited changes separately, allowing them to coexist in one observed setting.

  1. Which observed changes occurred in place, and which reflect erosion or imported deposits? boundary
  2. What evidence separates surface weathering from earlier hydrothermal, metamorphic or manufacturing-related alteration? provenance
Mechanisms and biological contributions Organises explanations for material breakdown and records evidence for interacting mechanisms.

Similar cracks, pits or colour changes can arise through different processes and do not establish a mechanism by themselves.

Physical disintegration

Examines fragmentation caused by stresses acting within or on the parent material.

Stress and fracture evidence

Assess candidate processes such as freezing, salt crystallisation, thermal effects and root growth using evidence of both the required conditions and resulting damage.

  1. Which candidate stress process fits the crack geometry, material properties and recorded exposure conditions? measurement
  2. What observation would distinguish the leading explanation from another process capable of producing similar fractures? measurement

Chemical and biological alteration

Examines dissolution, mineral transformation and organism-mediated changes.

Reaction and organism attribution

Connect mineral depletion, secondary products or dissolved constituents to plausible reactions, recording biological involvement as a contribution rather than an automatically separate mechanism.

  1. Which mineral losses, secondary phases or dissolved constituents support the proposed chemical reaction? measurement
  2. What evidence connects organisms to chemical alteration or physical disruption rather than simple occupation of an already weathered surface? boundary
Susceptibility and exposure Relates the material's properties to the environmental conditions that permit weathering.

Weathering behaviour depends on both susceptible material and access to the relevant reactants or stress cycles.

Parent material controls

Records composition and internal structure that influence reaction and fragmentation.

Minerals, texture and pathways

Identify susceptible mineral phases, grain relationships, pores and fractures, distinguishing pre-existing features from those produced by weathering.

  1. Which mineral phases and textural features are preferentially altered or disrupted? measurement
  2. Which pores and fractures predate weathering, and which developed as alteration progressed? provenance

Environmental forcing

Records local water, temperature, chemical and biological conditions over relevant timescales.

Effective exposure history

Characterise conditions experienced at the material surface and within accessible pores, including episodic exposure and changes in shelter or drainage.

  1. What wetting, drying, temperature and solution-chemistry conditions reach the affected material? measurement
  2. How have burial, excavation, shelter, drainage or pollution changed the material's exposure history? provenance
Alteration state and progression Assesses weathering extent, products and change through time.

A weathered appearance does not establish alteration depth, present activity or a reliable weathering rate.

Profiles and products

Describes spatial variation from exposed surfaces into less altered material.

Weathering front and residues

Record alteration gradients, rinds, residual fragments and secondary phases without assuming a uniform or sharply bounded front.

  1. How do mineral composition, strength or porosity vary with depth and along fractures? measurement
  2. Which surface or pore-filling products formed locally, and which were deposited from elsewhere? provenance

Activity and rate

Separates accumulated weathering from change demonstrated during an observation period.

Rate with attribution

Specify the measured quantity, reference area or volume, observation interval and uncertainty, separating weathering signals from transport and measurement artefacts.

  1. What repeated measurement demonstrates current progression, over what interval and above what detection limit? measurement
  2. How are abrasion, sediment removal, moisture changes and external deposition excluded or accounted for in the reported rate? boundary
Consequences and response Connects diagnosed weathering to material consequences and justified next actions.

An agent needs to distinguish observable alteration from consequential change and choose actions appropriate to the supported mechanism.

Functional consequences

Assesses how alteration affects the material in its natural or built setting.

Property and product effects

Relate weathering to measured changes in strength, permeability or constituent release, leaving downstream hazard assessment to the relevant models.

  1. Which measured property changes or released constituents matter for this material's setting and use? measurement
  2. What evidence warrants referral for slope, structural, conservation or water-quality assessment? action

Investigation and intervention

Selects monitoring or treatment based on mechanism evidence and evaluates the result.

Mechanism-matched response

Choose an investigation or intervention that addresses a supported weathering process, with explicit success measures and consideration of altered moisture or salt movement.

  1. Which additional observation would most reduce uncertainty before choosing an intervention? action
  2. How will monitoring determine whether the intervention reduced alteration or instead redistributed moisture, salts or damage? action
Evidence and external alignment What the world already says about this thing, gathered so the model can be checked against it.

A model that cannot be lined up against existing standards, identifiers and practice cannot be adopted by anyone who already uses them.

Reported evidence

Findings from the breadth pass, kept separate from the structural claims.

Check these first

Recalled without web access and unsourced; every item is a lead to verify.

  • The registry supplies no sense; the geological meaning is assumed and should be checked against the originating entry.
  • Biological weathering overlaps physical and chemical weathering rather than forming a mutually exclusive mechanism.
  • Weathering rates and severity measures depend on material, mechanism, climate, and timescale; no universal numerical range is appropriate.
  1. Which of these check these first hold for the sense of weathering this model covers, and on what evidence? provenance

Kinds and varieties

Recalled without web access and unsourced; every item is a lead to verify.

  • Physical or mechanical weathering
  • Chemical weathering
  • Biological weathering, acting through physical or chemical processes
  1. Which of these kinds and varieties hold for the sense of weathering this model covers, and on what evidence? provenance

Real-world use

Recalled without web access and unsourced; every item is a lead to verify.

  • Assessing rock durability for foundations, slopes, tunnels, and construction stone
  • Explaining soil formation and the development of regolith
  • Conserving stone buildings, monuments, and archaeological remains
  • Interpreting landscape development and sediment production
  • Studying mineral nutrient release and carbon cycling
  1. Which of these real-world use hold for the sense of weathering this model covers, and on what evidence? provenance

Failure modes and hazards

Recalled without web access and unsourced; every item is a lead to verify.

  • Weathering can weaken rock masses and contribute to slope instability and rockfall.
  • Salt crystallization, freezing water, and mineral alteration can cause stone to crack, flake, or disintegrate.
  • Dissolution can enlarge voids in soluble rock and contribute to ground instability.
  • Oxidation of exposed sulfide minerals can generate acidic drainage and mobilize metals.
  • Laboratory accelerated-weathering results may poorly predict field durability when exposure conditions and mechanisms differ.
  1. Which of these failure modes and hazards hold for the sense of weathering this model covers, and on what evidence? provenance

Regional variation

Recalled without web access and unsourced; every item is a lead to verify.

  • Warm, wet environments commonly favor chemical alteration, although mineralogy, drainage, and exposure duration strongly influence outcomes.
  • Cold regions can experience substantial frost weathering where moisture and suitable freezing conditions coincide.
  • Coastal and arid environments often experience salt weathering where salts accumulate and undergo crystallization cycles.
  1. Which of these regional variation hold for the sense of weathering this model covers, and on what evidence? provenance

Neighbouring kinds and how to tell them apart

Recalled without web access and unsourced; every item is a lead to verify.

  • erosion - Weathering breaks down or alters material in place; erosion involves its removal by agents such as flowing water, wind, or ice.
  • soil formation - Weathering supplies and alters mineral material; soil formation also includes organic matter accumulation, biological activity, redistribution, and horizon development.
  • metamorphism - Metamorphism transforms rock under changed temperature, pressure, or fluid conditions, generally within Earth's crust; weathering concerns alteration under near-surface environmental conditions.
  • mass wasting - Mass wasting is downslope movement driven by gravity; weathering can prepare or weaken the material without moving it downslope.
  • weathering hypothesis - The public-health sense concerns cumulative physiological effects of chronic social adversity; this description covers geological weathering.
  1. Which of these neighbouring kinds and how to tell them apart hold for the sense of weathering this model covers, and on what evidence? provenance

What the second pass must settle

  • Does vr.tr.weathering specifically denote geological weathering, given the missing definition and its ACT / ACT.ACT classification?
  • Does an existing Vercy world model already own this geological concept, requiring a registry link rather than a separate publication?
  • Which disciplinary definitions should govern the boundary with hydrothermal alteration, soil formation and weathering of manufactured mineral materials?
  • Which weathering grades and rate measurements are valid for each material and setting, and which comparisons would be misleading?
  • What evidence standards should distinguish biological causation, coupled mechanisms and inherited alteration when direct observations are unavailable?