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GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments

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TLDR
GRADISTAT as discussed by the authors is a computer program for the rapid analysis of grain size statistics from any of the standard measuring techniques, such as sieving and laser granulometry.
Abstract
Grain size analysis is an essential tool for classifying sedimentary environments. The calculation of statistics for many samples can, however, be a laborious process. A computer program called GRADISTAT has been written for the rapid analysis of grain size statistics from any of the standard measuring techniques, such as sieving and laser granulometry. Mean, mode, sorting, skewness and other statistics are calculated arithmetically and geometrically (in metric units) and logarithmically (in phi units) using moment and Folk and Ward graphical methods. Method comparison has allowed Folk and Ward descriptive terms to be assigned to moments statistics. Results indicate that Folk and Ward measures, expressed in metric units, appear to provide the most robust basis for routine comparisons of compositionally variable sediments. The program runs within the Microsoft Excel spreadsheet package and is extremely versatile, accepting standard and non-standard size data, and producing a range of graphical outputs including frequency and ternary plots. Copyright © 2001 John Wiley & Sons, Ltd.

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Use of indicators and pore volume-function characteristics to quantify soil physical quality

TL;DR: The Dexter "S -value" (S gi ) is a promising new indicator of soil physical quality (SPQ), but it is not well tested against established indicators, such as relative field capacity (RFC), plant-available water capacity (PAWC), air capacity (AC), macroporosity (P MAC), bulk density (BD), organic carbon content (OC), and structural stability index (SI) as discussed by the authors.
Journal ArticleDOI

Particle size scales and classification of sediment types based on particle size distributions: review and recommended procedures.

Simon J. Blott, +1 more
- 01 Dec 2012 - 
TL;DR: A review of different particle size scales, size class terminology and particle size distribution (textural) classification schemes is provided in this article, where a revised system of size class nomenclature, based on the Udden (1898) and Wentworth (1922) schemes, provides the most logical and consistent framework for use with sediments and other particulate materials.
Journal ArticleDOI

Late Pleistocene evolution of the Rhine-Meuse system in the southern North Sea basin: imprints of climate change, sea-level oscillation and glacio-isostacy

TL;DR: In this paper, high-resolution continuous core material, geophysical measurements and hundreds of archived core descriptions enabled to identify 13 Late Pleistocene Rhine-Meuse sedimentary units in the infill of the southern part of the North Sea basin (the Netherlands, northwestern Europe).
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Fine ash content of explosive eruptions

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References
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Journal ArticleDOI

Brazos River bar [Texas]; a study in the significance of grain size parameters

TL;DR: In this paper, a bar on the Brazos River near Calvert, Texas, has been analyzed in order to determine the geologic meaning of certain grain size parameters and to study the behavior of the size fractions with transport.
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A Scale of Grade and Class Terms for Clastic Sediments

TL;DR: In this paper, the problem of terminology in geology has been discussed and the need for greater uniformity of usage and hence much confusion has arisen due to the indiscriminate use of the terms both in the old and new senses.
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The Distinction between Grain Size and Mineral Composition in Sedimentary-Rock Nomenclature

TL;DR: In this paper, a system of grain-size nomenclature of terrigenous sediments and sedimentary rocks is introduced wherein fifteen major textural groups are defined on the ratios of gravel, sand, silt, and clay.
Journal ArticleDOI

Measures for describing the size distribution of sediments

TL;DR: In this article, the use of five parameters that serve as approximate graphic analogies to the moment measures commonly employed in statistics is recommended, which are computed from five percentile diameters obtained from the cumulative size-frequency curve of a sediment.
Journal ArticleDOI

Grain Size Distributions and Depositional Processes

TL;DR: In this article, a genetic interpretation of sand texture is provided based on recognizing sub-populations within individual log-normal grain size distributions, which may be related to a different mode of sediment transport and deposition, thus providing a measure of their importance in the genesis of a sand unit.
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