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Size Frequency Distributions of Sediments
Abstract
Abstract Distinction is made between continuous and discontinuous variables in frequency distributions. Histograms, frequency curves, and cumulative curves are discussed in relation to each other. On the basis of these relations an attempt is made to explain why histograms vary with the grade scale used in mechanical analysis, while cumulative curves do not. The disadvantages of histograms may be avoided by a simple graphic method for obtaining a continuous frequency curve independent of the grade scale. This curve is obtained by graphic differentiation of the cumulative curve, and is expressed in terms of the Wentworth descriptive grade scale. The analytic scale for obtaining the data is, however, shown to he independent of the descriptive scale units. It is suggested that in analyzing sediments, as many points as necessary be determined along the cumulative curve, to reduce errors of smoothing to a minimum.
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Citations
Cited by
Blott, S. J., & Pye, K. (2001) · Earth Surface Processes and Landforms · doi:10.1002/esp.261 · Cited by 4,385
Comparison of soil infiltration rates in burned and unburned mountainous watersheds
Martin, D. A., & Moody, J. A. (2001) · Hydrological Processes · doi:10.1002/hyp.380 · Cited by 316
Metadata
- Authors
- Krumbein, W. C.
- Venue
- SEPM Journal of Sedimentary Research
- Publisher
- Society for Sedimentary Geology
- Published
- 1934
- Volume
- Vol. 4
- Issue
- 2
- Pages
- 65-77
- ISSN
- 0022-4472 (ISSN-L)
- 1527-1404
- OpenAlex
- W2143370091
- Cited by
- 741
- References
- 0
- FWCI
- 0.00
- Type
- journal article
- Language
- en
- Open access
- closed
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- Krumbein, W. C. (1934). Size Frequency Distributions of Sediments. SEPM Journal of Sedimentary Research. https://doi.org/10.1306/d4268eb9-2b26-11d7-8648000102c1865d
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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