Soil Geochemistry: Principles and Concepts for Mineral Exploration, Exams of Geochemistry

An overview of soil geochemistry, focusing on its application in mineral exploration. It covers essential principles and concepts, including soil formation, sampling methods, and anomaly detection. The material is structured to guide exploration geologists in understanding how soil geochemistry can be effectively used to identify mineral deposits. Topics include considerations prior to sampling, soil development, anomaly formation, and methods of analysis. It also discusses sampling configurations, such as grid, profile, ridge, spur, and contour sampling, along with regional and semi-regional lag sampling techniques.

Typology: Exams

2025/2026

Available from 12/17/2025

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Exploration Geochemistry – Basic Principles & Concepts
Soil geochemistry / selective extractions / soil gases © ioGlobal Pty Ltd
Exploration Geochemistry – Basic
Principles & Concepts
Soil Geochemistry
Dr. David Lawie
ioGlobal
www.ioglobal.net
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Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

Exploration Geochemistry – Basic © ioGlobal Pty Ltd

Principles & Concepts^ Soil Geochemistry

Dr. David Lawie

ioGlobal www.ioglobal.net

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Outline

Considerations prior to startingScale of samplingSoils and Soil DevelopmentSites for Hosting Anomalies Within SoilsSampling ProtocolsMethods of Analysis & ChallengesAnomaly FormationSome Final Comments

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

From CRC-LEME newsletter

Soil

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

Consideration Prior To Embarking on a Soil Survey^ What elements to analyse for (target, pathfinder, regolith control)Extraction and instrumental finishNature of the soil substrate – residual/transportedSoil profile development, what depth or horizon to sampleLocal variations due to topography, drainage, parent materialOptimum size of sample and whether to sieve or notSpatial configuration of the sampling (square or offset grid, tightspacing along widely spaced lines)QC – Need to monitor the accuracy and representivity of data © ioGlobal Pty Ltd

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Prospect Scale - Grid

From Rose, Hawkes and Webb 1979

Prospect scale profilesampling to follow upgeophysical anomalies

10 ×

target width either side

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Prospect Scale - Profiles^ Prospect scale profile sampling tofollow up egg, geophysical anomalies 10 ×

target width either side

Don’t Do This

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

Prospect Scale – Contour Sampling © ioGlobal Pty Ltd

Courtesy Simon Gatehouse

Good for initial reconnaissance oflarge area which has not beenpreviously sampled Relevant where have:

Strongly and deeply dissectedterrainDrainage divides have a poorchance of intersectingmineralisationLogistical difficulty: poor accessinto streams and ridgesbecause of terrain. Speed & Safety: contours often easier tonavigate than ridges in extremetopography

Upper most B horizon tomaximise dispersionCompositing rate variable

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Semi Regional – Lag Sampling

Swept from the surfaceSieved to 2–6 mmData may be normalised to Fe contentSample grids at 500m by 500m have beenused

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Regional Soil Data – As in soil

Geological Control

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Regional Scale – Soils combined with

other surficial data

ZOOM 2

Levelled Cu Data – Nth America

ZOOM 1

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

Always Occur: © ioGlobal Pty Ltd

Weathering of parent materialAddition and partial decomposition of organic matterFormation of structural units

(Profile)

Depending on Environment

Leaching and acidificationClay eluviation (washing of clay from upper horizons)Podzolisation (transport of DOC and Fe & Al from upper h)Leaching of Si relative to Fe and AlReduction (ferric to ferrous)SalinisationErosion

Soil Formation

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

Soil development is initiated by the weathering of thebedrock and the incorporation of organic matter.These processes produce: © ioGlobal Pty Ltd

dissolved matter (bases, silicic acid, Fe, Al etc.); dispersed colloidal particles (e.g. silica, etc.): hydroxyls (Fe, Al, etc.): organic complexes; and, fine particulate matter (clay, clay-sized particles, etc.)

Profile Development

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

++

    • ++ +++ + + O + + ++ A1 A2 B C R

Bedrock

Parent material derivedby weathering

Horizons of illuviation(accumulation ofmaterial bydepositionor precipitationfrom percolatingwater).

Some soils show intensely gleyed layers(Horizon G of hydromorphic soils; G mayappear directly beneath A), or layers ofcalcium carbonate (Horizon C

Ca^

of

Organic debris only partially decomposedDark-colored horizon, organic (humus)rich; mixed with mineral matter.Light- Brown to orange-brown horizons.Accumulation of clay minerals or of ironand organic matter; compact blocky,prismatic structure. calcareous soils).

colored horizon of maximum eluviation. Prominent in some soils, faint or absent inothers. Generally loose structure.

Idealised Soil Profile Horizons of maximumbiological activity, ofeluviation (removal ofmaterials suspendedor dissolved in water),or both.

The Solum (the genericsoil developedby soil-formingprocesses)

Modified from Rose, Hawkesand Webb 1979

Exploration Geochemistry – Basic Principles & ConceptsSoil geochemistry / selective extractions / soil gases

© ioGlobal Pty Ltd

Major Soil Groups of the World

FOOD AND AGRICULTURE ORGANISATION OF THE UNITED NATIONS