Wyniki wyszukiwania

1

Decomposition study of in vivo phytoplankton absorption spectra aimed at identifying the pigments and the phytoplankton group in complex case 2 coastal waters of the Arabian Sea

100%

Shaju S. S., Minu P., Srikanth A. S., Ashraf P. M., Vijayan A. K., Meenakumari B.

Oceanological and Hydrobiological Studies

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2015

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tom 44

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nr 3

2

Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik

Optical properties of maize seeds

100%

Hernandez A., Cruz O., Ivanov R., Dominguez P., Carballo C., Moreno I.

International Agrophysics

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2011

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tom 25

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nr 3

3

Theoretical aspects of formation and development of cavitation processes in technological environment

100%

Bernyk I.

Motrol. Motoryzacja i Energetyka Rolnictwa

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2017

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tom 19

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nr 3

4

Modelling the light absorption properties of particulate matter forming organic particles suspended in sea water. Part 3. Practical applications

100%

Wozniak B., Wozniak S. B., Tyszka K., Ostrowska M., Ficek D., Majchrowski R., Dera J.

Oceanologia

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2006

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tom 48

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nr 4

5

Performance evaluation of non-water absorption coefficient partitioning algorithms in optically complex coastal waters of Kochi and Goa, India

84%

Kolluru S., Gedam S. S., Inamdar A. B.

Oceanologia

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2021

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tom 63

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nr 4

6

Chromophoric dissolved organic matter (CDOM) variability over the continental shelf of the Northern Bay of Bengal

84%

Das S., Das I., Giri S., Chanda A., Maity S., Lotliker A. A., Kumar T. S., Akhand A., Hazra S.

Oceanologia

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2017

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tom 59

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nr 3

The present paper dealt with the annual dynamics of the absorption coefficient of chromophoric dissolved organic matter at 440 nm {aCDOM(440)} during February 2015 to January 2016 in the continental shelf of northern Bay of Bengal (nBoB) for the first time. Sea surface salinity (SSS), chlorophyll-a (Chl-a), total suspended matter (TSM) were also analyzed. It was hypothesized that CDOM should exhibit significant spatial and temporal variability in this region. aCDOM(440) and spectral slope ranged between 0.1002 m1—0.6631 m1 and 0.0071 nm1— 0.0229 nm1 respectively during the entire study period. Higher values of aCDOM(440) were observed in the near shore stations and gradually decreased towards the offshore. Significant seasonal variability of aCDOM(440) was observed between the monsoon and non-monsoon seasons ( p < 0.05). Thus the framed hypothesis was successfully accepted by means of the present study. The CDOM was mainly found to be of allochthonous character in this region. aCDOM(440) portrayed a significant negative linear relationship with SSS (R2 = 0.80; p < 0.05) implying conservative mixing of marine and terrestrial end members. However, examining the spatial variability of the relationship, it was observed that this relationship was significant only in the nearshore stations. While examining the seasonal variability of this relationship, it was found to be most significant during the monsoon (R2 = 0.81; p < 0.05). Thus it was inferred that whenever the SSS gradient was higher, the relationship between aCDOM(440) and SSS was found to be most significant.

7

Experimental study of the composite parts of the light-beam attenuation process in the waters of the Gulf of Gdansk

84%

Dera J., Gohs L., Wozniak B.

Oceanologia

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1978

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tom 10

8

Influence of chosen parameters on seasonal changes of spectrum of light absorption coefficient in waters of the Pomeranian Bay [Southern Baltic]

84%

Mrozek-Lejman J., Miklaszewicz B.

Polish Journal of Ecology

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2001

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tom 49

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nr 2

9

Relationship between texture sensory profiles and optical properties measured by time-resolved reflectance spectroscopy during post-storage shelf life of ‘Braeburn’ apples

67%

Rizzolo A., Vanoli M., Bianchi G., Zanella A., Grassi M., Torricelli A., Spinelli L.

Journal of Horticultural Research

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2014

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tom 22

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nr 1

10

Spectral light absorption by yellow substance in the Kattegat-Skagerrak area

67%

Hojerslev N. K., Aas E.

Oceanologia

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2001

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tom 43

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nr 1

More than 1500 water samples were taken from the Kattegat, the Skagerrak and adjacent waters. The value of the absorption coefficient of yellow substance at 310 nm was found to varyf rom 0.06 to 7.4 m−1 in the open coastal waters, with a mean value of 1.3 m−1. The corresponding wavelength-averaged value (250–450 nm) of the semilogarithmic spectral slope of the coefficient ranges from 0.008 to 0.042 nm−1, and the mean value is 0.023 nm−1. Closer to river discharges, as in the fjords, the values of the slope seem to be more constant at around 0.0175±0.0015 nm−1. In this area the slope must then be known in order to compare absorption at different wavelengths or to model the yellow substance absorption.

Ograniczanie wyników

Decomposition study of in vivo phytoplankton absorption spectra aimed at identifying the pigments and the phytoplankton group in complex case 2 coastal waters of the Arabian Sea

Optical properties of maize seeds

Theoretical aspects of formation and development of cavitation processes in technological environment

Modelling the light absorption properties of particulate matter forming organic particles suspended in sea water. Part 3. Practical applications

Performance evaluation of non-water absorption coefficient partitioning algorithms in optically complex coastal waters of Kochi and Goa, India

Chromophoric dissolved organic matter (CDOM) variability over the continental shelf of the Northern Bay of Bengal

Experimental study of the composite parts of the light-beam attenuation process in the waters of the Gulf of Gdansk

Influence of chosen parameters on seasonal changes of spectrum of light absorption coefficient in waters of the Pomeranian Bay [Southern Baltic]

Relationship between texture sensory profiles and optical properties measured by time-resolved reflectance spectroscopy during post-storage shelf life of ‘Braeburn’ apples

Spectral light absorption by yellow substance in the Kattegat-Skagerrak area