Matches in SemOpenAlex for { <https://semopenalex.org/work/W4205364757> ?p ?o ?g. }
- W4205364757 endingPage "1648" @default.
- W4205364757 startingPage "1626" @default.
- W4205364757 abstract "Abstract Sediments in deltaic tidal flats regulate physical and chemical processes. Grain‐size distribution plays an important role in determining sediment dynamics and substrate properties. However, it is challenging to quantify large‐scale depositional environments in intertidal flats, due to time‐consuming grain‐size analyses and sparse sedimentary information extracted from scattered sediment samples. In this study, a novel terrestrial laser scanner (TLS) based method was developed to characterize the substrate of an intertidal flat. Surface sediment samples in the Nanhui flats in the Yangtze Delta, China, and the corresponding waveform amplitudes of TLS echoes at fixed sampling sites were collected for a total of 22 months. A negative logarithmic relationship was found between the sediment sand fraction, average grain size, D 50 , and corrected waveform amplitude of TLS echo in different hydro‐meteorological conditions. The mean of average grain size of five sediment sampling sites along a transect was 58.78 μm when measured by traditional grain‐size analysis, and 49.48 μm when calculated with the proposed logarithmic equation. The mean error at each site was up to 21.77%. The mean error for the sand and silt fraction at each location was as high as 27.28% and 21.75%, respectively. The spatial distribution pattern of TLS‐based average grain size in the entire study area was consistent with the measured pattern with a Root Mean Square Error of 13.83 μm. These errors could be caused by the accuracy of the TLS waveform amplitude correction and by limits of the method in recognizing different substrates. The effects produced by the presence of microphytobenthos (for example, cyanobacterial mats or diatom biofilms) or bedforms have not been investigated and may have affected the results. The TLS‐based grain‐size measurements can rapidly and effectively discriminate sediment characteristics, thus avoiding traditional time‐consuming measurements. It is expected that the TLS‐based method proposed here will have wide applications in shoreline studies, especially in inaccessible tidal flats." @default.
- W4205364757 created "2022-01-26" @default.
- W4205364757 creator A5066134990 @default.
- W4205364757 creator A5072894779 @default.
- W4205364757 creator A5072999536 @default.
- W4205364757 creator A5075173202 @default.
- W4205364757 date "2022-02-10" @default.
- W4205364757 modified "2023-09-27" @default.
- W4205364757 title "A novel approach to discriminate sedimentary characteristics of deltaic tidal flats with terrestrial laser scanner: Results from a case study" @default.
- W4205364757 cites W1580205926 @default.
- W4205364757 cites W1601607554 @default.
- W4205364757 cites W1966034864 @default.
- W4205364757 cites W1967315984 @default.
- W4205364757 cites W1969437907 @default.
- W4205364757 cites W1970431923 @default.
- W4205364757 cites W1970647949 @default.
- W4205364757 cites W1974331217 @default.
- W4205364757 cites W1977308279 @default.
- W4205364757 cites W1979198083 @default.
- W4205364757 cites W1991072018 @default.
- W4205364757 cites W1993754118 @default.
- W4205364757 cites W1995798243 @default.
- W4205364757 cites W1996080638 @default.
- W4205364757 cites W1997384433 @default.
- W4205364757 cites W1997887142 @default.
- W4205364757 cites W1998350284 @default.
- W4205364757 cites W1998492031 @default.
- W4205364757 cites W1998809317 @default.
- W4205364757 cites W2003987953 @default.
- W4205364757 cites W2006848431 @default.
- W4205364757 cites W2011131989 @default.
- W4205364757 cites W2013383027 @default.
- W4205364757 cites W2014197200 @default.
- W4205364757 cites W2017454686 @default.
- W4205364757 cites W2021077202 @default.
- W4205364757 cites W2030080266 @default.
- W4205364757 cites W2033269027 @default.
- W4205364757 cites W2034385314 @default.
- W4205364757 cites W2035141327 @default.
- W4205364757 cites W2037326007 @default.
- W4205364757 cites W2037504032 @default.
- W4205364757 cites W2039834035 @default.
- W4205364757 cites W2043867631 @default.
- W4205364757 cites W2045743675 @default.
- W4205364757 cites W2053384936 @default.
- W4205364757 cites W2055033732 @default.
- W4205364757 cites W2057137459 @default.
- W4205364757 cites W2068084825 @default.
- W4205364757 cites W2074408352 @default.
- W4205364757 cites W2076606872 @default.
- W4205364757 cites W2079543476 @default.
- W4205364757 cites W2081077635 @default.
- W4205364757 cites W2083336665 @default.
- W4205364757 cites W2084407493 @default.
- W4205364757 cites W2085418190 @default.
- W4205364757 cites W2086461898 @default.
- W4205364757 cites W2086557208 @default.
- W4205364757 cites W2091525788 @default.
- W4205364757 cites W2100633852 @default.
- W4205364757 cites W2108338372 @default.
- W4205364757 cites W2113551198 @default.
- W4205364757 cites W2114191733 @default.
- W4205364757 cites W2115233283 @default.
- W4205364757 cites W2119616250 @default.
- W4205364757 cites W2126927175 @default.
- W4205364757 cites W2130023530 @default.
- W4205364757 cites W2133732249 @default.
- W4205364757 cites W2134207582 @default.
- W4205364757 cites W2139032490 @default.
- W4205364757 cites W2140161421 @default.
- W4205364757 cites W2142069533 @default.
- W4205364757 cites W2153927283 @default.
- W4205364757 cites W2159525271 @default.
- W4205364757 cites W2160291979 @default.
- W4205364757 cites W2161930174 @default.
- W4205364757 cites W2325095476 @default.
- W4205364757 cites W23313910 @default.
- W4205364757 cites W2581089300 @default.
- W4205364757 cites W2742572994 @default.
- W4205364757 cites W2742739534 @default.
- W4205364757 cites W2749416095 @default.
- W4205364757 cites W2762961276 @default.
- W4205364757 cites W2777478767 @default.
- W4205364757 cites W2784764570 @default.
- W4205364757 cites W2793446724 @default.
- W4205364757 cites W2808324030 @default.
- W4205364757 cites W2808422467 @default.
- W4205364757 cites W2896258468 @default.
- W4205364757 cites W2901397829 @default.
- W4205364757 cites W2902394412 @default.
- W4205364757 cites W2910900897 @default.
- W4205364757 cites W2914897861 @default.
- W4205364757 cites W291897460 @default.
- W4205364757 cites W2943177046 @default.
- W4205364757 cites W2948559686 @default.
- W4205364757 cites W2963809831 @default.
- W4205364757 cites W2971380590 @default.
- W4205364757 cites W3020629826 @default.