方法对比
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| Munsell Soil Color× | Harris Matrix× | |
|---|---|---|
| 领域 | 考古学 | 考古学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 1905 | 1973 |
| 提出者≠ | Albert H. Munsell (color system); standardized for soils by the USDA and soil-science community | Edward C. Harris (with the Winchester excavation team) |
| 类型≠ | Standardized perceptual color description pipeline | Stratigraphic recording and sequence-diagramming pipeline |
| 开创性文献≠ | Goldberg, P., & Macphail, R. I. (2006). Practical and Theoretical Geoarchaeology. Blackwell Publishing. ISBN: 9780632060443 | Harris, E. C. (1989). Principles of Archaeological Stratigraphy (2nd ed.). Academic Press. ISBN: 9780123266514 |
| 别名 | Munsell Color Notation, Munsell Soil Color Charts, Soil Color Description, HVC Color Recording | Stratigraphic Sequence Diagram, Harris-Winchester Matrix, Single-Context Recording, Context Sequence Diagram |
| 相关 | 2 | 2 |
| 摘要≠ | Munsell soil color recording is the standard method for describing the color of soils, sediments, and artifacts in archaeology and geoarchaeology using Albert Munsell's perceptually ordered color system. Rather than relying on subjective names like 'brown' or 'tan,' the analyst matches a sample to printed color chips and records a three-part notation — hue, value, and chroma — that fixes the color as a point in a standardized three-dimensional space. This makes color a reproducible, communicable observation that different excavators, sites, and decades can compare directly. Color in turn carries information about organic content, oxidation and reduction, burning, and parent material, so disciplined Munsell recording is a routine first step in distinguishing deposits, defining horizons, and reading site formation. | The Harris matrix is a method for recording and diagramming the stratigraphic sequence of an archaeological site as a partial-order diagram of individually defined contexts. Devised by Edward C. Harris at the Winchester excavations in 1973 and codified in his Principles of Archaeological Stratigraphy, it treats every deposit, cut, and interface as a separate stratigraphic unit and reduces the tangle of physical relationships among them to a minimal directed acyclic graph that expresses only relative temporal order. By distinguishing physical superposition from temporal sequence and stripping away redundant relationships through transitive reduction, the matrix turns the three-dimensional complexity of a dig into a single, auditable diagram. It is the structural backbone of single-context recording and the standard interface between excavation and chronological modeling. |
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