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ASTM D5754 −95 (Reapproved 2006) is a standard guide for displaying the results of chemical analyses of groundwater for major ions and trace elements using trilinear diagrams for two or more analyses. It is the first of several documents intended to inform hydrology professionals about traditional graphical methods available to display groundwater chemistry. By utilizing two-dimensional trilinear graphs, this guide helps interpret the physical and chemical mechanisms controlling water composition.
This guide covers the category of water analysis diagrams that use two-dimensional trilinear graphs as a technique for displaying common chemical components from two or more complete analyses of natural groundwater on a single diagram. The category includes not only trilinear-shaped diagrams but also diamond-, parallelogram-, rectangular-, or square-shaped graphs that have trilinear subdivisions.
The standard references several key companion documents, including Guide D596 for reporting results of water analysis, Terminology D653 for soil, rock, and contained fluids, and Terminology D1129 relating to water, ensuring consistency across related ASTM standards.
Accurate plotting on these diagrams requires a complete analysis of the dissolved ions reported in consistent units. The standard defines the critical terminology needed for this graphical representation.
| 📏 Term | 📝 Definition (per D5754) | ⚡ Unit of Measure |
|---|---|---|
| Cation | An ion that moves or would move toward a cathode (positive ion). | epm (equiv/million) |
| Anion | An ion that moves or would move toward an anode (negative ion). | epm (equiv/million) |
| epm | Equivalent weight unit expressed as milligram-equivalent per kilogram. | mg-eq/kg |
Major cations typically plotted include calcium (Ca²⁺), magnesium (Mg²⁺), sodium (Na⁺), and potassium (K⁺). Major anions include bicarbonate (HCO₃⁻), sulfate (SO₄²⁻), and chloride (Cl⁻). All data must be converted to equivalent units (epm) before plotting to ensure accurate ionic balance and comparison.
Several established methodologies for constructing and interpreting trilinear diagrams are detailed in the standard. These are proven systems for interpreting the origin of ions in natural groundwater and facilitating the comparison of results from a large number of analyses.
| 🟦 Method | 🎯 Key Proponent(s) | 📐 Diagram Type |
|---|---|---|
| Hill | Hill (Refs 1-3) | Trilinear |
| Langelier-Ludwig | Langelier and Ludwig (Ref 4) | Square / Rectangular |
| Piper | Piper (Refs 5, 6) | Diamond / Trilinear |
| Durov | Durov (Refs 7-13) | Square / Trilinear |
By plotting analyses on these diagrams, professionals can visually assess hydrochemical facies, trace evolutionary paths, and compare datasets across different aquifers or sampling events. This standard serves as the foundational reference for these widely used interpretive techniques in groundwater chemistry.
🔍 What is the primary purpose of ASTM D5754-95?
It provides a standardized guide for displaying results of groundwater chemical analyses for major ions and trace elements using two-dimensional trilinear diagrams for two or more analyses to help interpret the physical and chemical mechanisms controlling water composition.
💡 What types of diagram shapes are covered by this standard?
The standard covers diagrams with trilinear subdivisions, including classic trilinear-shaped diagrams, as well as diamond-, parallelogram-, rectangular-, and square-shaped graphs.
⚡ Why must data be converted to epm (equivalent per million) units for plotting?
Equivalent units are essential because they account for the charge balance of ions. Expressing concentrations in milligram-equivalents per kilogram ensures that the sums of cations and anions are comparable and accurately represent the chemical equivalence of the dissolved species.
📌 Which trilinear methods are specifically identified as the most commonly used?
The standard specifically identifies the methods developed by Hill, Langelier and Ludwig, Piper, and Durov as proven techniques for interpreting the origin of ions in natural groundwater and facilitating the comparison of results from a large number of analyses.