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電子書籍・電子雑誌Progress in earth and planetary science
Volume number5
Reconstruc...

Reconstruction of sediment-transport pathways on a modern microtidal coast by a new grain-size trend analysis method

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Reconstruction of sediment-transport pathways on a modern microtidal coast by a new grain-size trend analysis method

Call No. (NDL)
Z19-B878
Bibliographic ID of National Diet Library
11068296
Persistent ID (NDL)
info:ndljp/pid/11068296
Material type
記事
Author
Shota Yamashitaほか
Publisher
Springer Nature
Publication date
2018-02-01
Material Format
Paper・Digital
Journal name
Progress in earth and planetary science 5(7)
Publication Page
-
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Summary, etc.:

A new method for granulometric-parameter-based reconstruction of sediment-transport pathways is proposed and is termed P-GSTA (grain-size trend analys...

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Bibliographic Record

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Digital

Material Type
記事
Author/Editor
Shota Yamashita
Hajime Naruse
Takeshi Nakajo
Publication, Distribution, etc.
Publication Date
2018-02-01
Publication Date (W3CDTF)
2018-02-01
Periodical title
Progress in earth and planetary science
No. or year of volume/issue
5(7)
Volume
5(7)
ISSN (Periodical Title)
2197-4284
ISSN-L (Periodical Title)
2197-4284
Text Language Code
eng
Persistent ID (NDL)
info:ndljp/pid/11068296
Collection (Materials For Handicapped People:1)
Collection (particular)
国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
Acquisition Basis
オンライン資料収集制度
Date Accepted (W3CDTF)
2018-04-16T21:38:33+09:00
Date Captured (W3CDTF)
2018-04-16
Format (IMT)
application/pdf
Access Restrictions
国立国会図書館内限定公開
Service for the Digitized Contents Transmission Service
図書館・個人送信対象外
Availability of remote photoduplication service
Periodical Title (Persistent ID (NDL))
info:ndljp/pid/11018906
Data Provider (Database)
国立国会図書館 : 国立国会図書館デジタルコレクション

Digital

Summary, etc.
A new method for granulometric-parameter-based reconstruction of sediment-transport pathways is proposed and is termed P-GSTA (grain-size trend analysis using principal component analysis) herein. The main advantage of this method is its applicability to depositional environments involving mixed transport processes, for instance, fluvial, tidal, and wave-influenced environments. In the P-GSTA method, a linear function with all significant granulometric parameters that are summed with different weighting factors was used to infer sediment-transport direction (sediment flux pattern); the previous grain-size trend analysis (GSTA) methods considered only three parameters (mean grain size, sorting, and skewness) with equal weighting. This study chose six parameters (namely, median grain size, coefficient of variation, skewness, kurtosis, and mud and gravel log-ratios) for calculation. First, the zero values of mud and gravel fractions are replaced, and their log-ratios are defined. Then, all values are standardized. Thereafter, principal component analysis (PCA) is conducted to determine the weighting factor of each granulometric parameter. Each principal component is then interpreted, and the function best representing a sediment flux pattern is chosen from these components. Trend vectors are calculated, solely on the basis of a map interpolated from the scores of the chosen principal component, as the two-dimensional gradient of this value. The P-GSTA method proposed in this study was applied to a modern microtidal coast (tidal sand flat along the Kushida River Delta, central Japan). Sediment-transport pathways reconstructed by this method were consistent with observed sediment-transport patterns determined by field experiments using tracer sediments and geomorphologic observation; the results of the previous GSTA method were inconsistent with the observations. The proposed method also revealed additional minor depositional processes on the sand flat, namely, the deposition of fluvial-channel lags and muddy particles. Thus, this study demonstrates that the proposed P-GSTA method is a potentially powerful tool to reconstruct sediment-transport patterns even under mixed transport processes, where the estimation of the sediment-transport function is difficult.
Access Restrictions
インターネット公開
Rights (production)
© The Author(s). 2018
This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
Is Referenced By
Logratio analysis of components separated from grain‐size distributions and implications for sedimentary processes: An example of bottom surface sediments in a shallow lake
Validation of appropriate estimation criteria for the number of components for separating a polymodal grain-size distribution into lognormal distributions
References
Dealing with Zeros and Missing Values in Compositional Data Sets Using Nonparametric Imputation
Non-uniform sediment transport: dynamics of the active layer
Sediment trend models fail to reproduce small‐scale sediment transport patterns on an intertidal beach
Sediment transport patterns determined from grain size parameters: Overview and state of the art
Grain-size trends used to assess the effective discharge for floodplain sedimentation, River Waal, the Netherlands
The three-dimensional distribution of sedimentary facies and characteristics of sediment grain-size distribution in a sandy tidal flat along the Kushida River estuary, Ise Bay, central Japan
Net sediment transport patterns over the Bohai Strait based on grain size trend analysis
The coastal depositional system of a small mountainous river: a perspective from grain-size distributions
Probabilistic Exner Sediment Continuity Equation for Mixtures with No Active Layer
A settling tube system for sand-size analysis
Between beds and sequences: stratigraphic organization at intermediate scales in the Quaternary of the Virginia coast, USA
OPTIMAL INTERPOLATION AND ISARITHMIC MAPPING OF SOIL PROPERTIES
Compositional Data Analysis: Where Are We and Where Should We Be Heading?
A Simple Universal Equation for Grain Settling Velocity
Application of grain size trend analysis for the determination of sediment transport pathways in intertidal areas
Net sediment transport patterns inferred from grain-size trends, based upon definition of “transport vectors”
The Statistical Analysis of Compositional Data
Downdrift coarsening of beach foreshore sediments at tidal inlets: An example from the coast of New Jersey
OPTIMAL INTERPOLATION AND ISARITHMIC MAPPING OF SOIL PROPERTIES III CHANGING DRIFT AND UNIVERSAL KRIGING
Grain-size trends and transport along beaches: Example from eastern England
A REVIEW OF GRAIN‐SIZE PARAMETERS
Armoring をともなう河床低下について
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Crossref
Bibliographic ID (NDL)
11068296
NAID
120006410710