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specific ultraviolet absorbance

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General representation of dissolved organic C (DOC), specific ultraviolet absorbance (SUVA), discharge (Q), precipitation (P), and solute concentrations measured in the stream outlet of the Meerdaal catchment during a rainfall event (29 June 2011).
Published: 01 July 2014
Fig. 5. General representation of dissolved organic C (DOC), specific ultraviolet absorbance (SUVA), discharge ( Q ), precipitation ( P ), and solute concentrations measured in the stream outlet of the Meerdaal catchment during a rainfall event (29 June 2011).
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General representation of dissolved organic C (DOC), specific ultraviolet absorbance (SUVA), discharge (Q), precipitation (P), and solute concentrations measured in the stream outlet of the Blégny catchment during the spring to summer period (20 May 2012, left) and the fall-winter period (5 Dec. 2011, right).
Published: 01 July 2014
Fig. 7. General representation of dissolved organic C (DOC), specific ultraviolet absorbance (SUVA), discharge ( Q ), precipitation ( P ), and solute concentrations measured in the stream outlet of the Blégny catchment during the spring to summer period (20 May 2012, left) and the fall-winter
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Schematic depiction of the temporal development of specific ultraviolet absorbance (SUVA), dissolved organic C (DOC), total Fe content, and pH values during the period of observation for the Wu01, Wu03, Wu08, Wu09, Wu12, and Wu15 sampling locations and the Wüstebach main gauging point (Wu14). The letter W is used for Wu here.
Published: 01 April 2015
Fig. 4. Schematic depiction of the temporal development of specific ultraviolet absorbance (SUVA), dissolved organic C (DOC), total Fe content, and pH values during the period of observation for the Wu01, Wu03, Wu08, Wu09, Wu12, and Wu15 sampling locations and the Wüstebach main gauging point
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Correlation between bulk and molecular measurements: (A) comparison between the percentage of lignin and tannin markers (LIG-TAN) and specific ultraviolet absorbance (SUVA) values determined at 254 nm; (B) comparison between the percentage of LIG-TAN and δ13C values; and (C) comparison between the percentage of microbial markers (MICMAK) and δ13C values. White, gray, and black symbols demarcate samples from the organo-mineral, transition, and mineral layers, respectively. For the mineral layer, the triangle, circles, and square indicate samples from Periods A, B, and C, respectively.
Published: 01 July 2014
Fig. 4. Correlation between bulk and molecular measurements: (A) comparison between the percentage of lignin and tannin markers (LIG-TAN) and specific ultraviolet absorbance (SUVA) values determined at 254 nm; (B) comparison between the percentage of LIG-TAN and δ 13 C values; and (C) comparison
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Statistical boxplots for (a) dissolved organic C (DOC), (b) specific ultraviolet absorbance (SUVA254), (c) pH, and (d) Fe3+for the complete observation period. The Wüstebach main gauging point (Wu14) is compared with surface water sampling locations potentially representing surface water (Wu01, Wu08, and Wu09) in blue and groundwater (Wu03, Wu12, and Wu15) inflows in green into the Wüstebach. The respective number of results used for each boxplot is given in brackets below the point indications. The black line in the box denotes the mean; horizontal lines of the box denote the 25th, 50th, and 75th percentile values. The cross and the line symbol above and below the box denote the 99th and 100th percentiles. Different letters above the boxplots indicate significant differences between sampling points.
Published: 01 April 2015
Fig. 3. Statistical boxplots for (a) dissolved organic C (DOC), (b) specific ultraviolet absorbance (SUVA 254 ), (c) pH, and (d) Fe 3+ for the complete observation period. The Wüstebach main gauging point (Wu14) is compared with surface water sampling locations potentially representing surface
Journal Article
Published: 01 July 2014
Vadose Zone Journal (2014) 13 (7): vzj2013.08.0155.
... into four different molecular-weight fractions with ultrafiltration, and the fractions were measured for the concentrations of dissolved organic C (DOC), N, and carbohydrates, aromaticity (specific ultraviolet [UV] absorbance at 254 nm), pH, and bioavailability to bacteria. The percentage of DOC in the low...
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Response of dissolved organic C (DOC) concentrations, specific ultraviolet (UV) absorbance at 280 nm, and the humification index (HIX) of dissolved organic matter to throughfall addition during the snow-free period in 2002 to 2007.
Published: 01 July 2014
Fig. 1. Response of dissolved organic C (DOC) concentrations, specific ultraviolet (UV) absorbance at 280 nm, and the humification index (HIX) of dissolved organic matter to throughfall addition during the snow-free period in 2002 to 2007.
Journal Article
Published: 01 July 2014
Vadose Zone Journal (2014) 13 (7): vzj2013.11.0199.
...Fig. 5. General representation of dissolved organic C (DOC), specific ultraviolet absorbance (SUVA), discharge ( Q ), precipitation ( P ), and solute concentrations measured in the stream outlet of the Meerdaal catchment during a rainfall event (29 June 2011). ...
FIGURES | View All (11)
Journal Article
Published: 01 April 2015
Vadose Zone Journal (2015) 14 (4): vzj2015.01.0005.
...Fig. 4. Schematic depiction of the temporal development of specific ultraviolet absorbance (SUVA), dissolved organic C (DOC), total Fe content, and pH values during the period of observation for the Wu01, Wu03, Wu08, Wu09, Wu12, and Wu15 sampling locations and the Wüstebach main gauging point...
FIGURES | View All (4)
Journal Article
Published: 01 July 2014
Vadose Zone Journal (2014) 13 (7): vzj2014.02.0015.
...Fig. 4. Correlation between bulk and molecular measurements: (A) comparison between the percentage of lignin and tannin markers (LIG-TAN) and specific ultraviolet absorbance (SUVA) values determined at 254 nm; (B) comparison between the percentage of LIG-TAN and δ 13 C values; and (C) comparison...
FIGURES | View All (4)
Journal Article
Published: 01 December 2014
Vadose Zone Journal (2014) 13 (12): vzj2014.06.0071.
... interference, Fe 2+ ions and DOC absorbed ultraviolet light strongly in regions of the spectrum where NO 3 − also exhibited significant absorption. Natural water samples showed very low concentrations of Fe 2+ , which do not cause interference with nitrate measurements. A two-wavelength measurement scheme...
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Journal Article
Journal: Geosphere
Published: 10 April 2024
Geosphere (2024) 20 (3): 880–894.
.... , Fugii , R. , and Mopper , R. , 2003 , Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon : Environmental Science & Technology , v. 37 , p. 4702 – 4708 , https://doi.org/10.1021/es030360x...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1961
AAPG Bulletin (1961) 45 (10): 1713–1720.
...-260 m µ is fairly persistent and one of the samples had a strong peak at 260 m µ . Benzenoid compounds as well as pyridines absorb in this region, as do humic acid extracts ( Gex and Firtion, 1944 ) and the present substance or substances may be of this nature. Fig. 3. Ultraviolet absorption...
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Journal Article
Journal: Clay Minerals
Published: 16 March 2022
Clay Minerals (2021) 56 (4): 292–298.
... of solar radiation. The wavelength of incoming solar radiation varies between ~300 and 2500 nm. Ultraviolet (UV) radiation consists of radiation with wavelengths <400 nm, while infrared (IR) radiation consists of radiation with wavelengths >800 nm. UV-C (200–280 nm) radiation is absorbed...
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Journal Article
Journal: Elements
Published: 01 April 2010
Elements (2010) 6 (2): 87–92.
... in the plume. The first volcanological DOAS observations were made in 1992 from a scientific vessel cruising the Mediterranean – more specifically, downwind of the steaming craters of Etna, Stromboli and Vulcano ( Edner et al. 1994 ). A rather bulky ultraviolet spectrometer was employed...
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Journal Article
Journal: Clay Minerals
Published: 01 December 2001
Clay Minerals (2001) 36 (4): 541–546.
... between ~250 and 800°C. Removal of these strongly held molecules probably occurs at the same time as the decomposition of the drug molecule, accounting for the DTA steps recorded in this temperature range. The ability of the systems prepared to absorb visible-ultraviolet (V-UV) radiation was checked...
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Journal Article
Published: 01 May 2015
Journal of Micropalaeontology (2015) 34 (2): 139–149.
... on the absorbance spectra. oxidation palynology ultraviolet-B FTIR sporopollenin Sporomorphs (pollen and spores) are the reproductive vectors of land plants. The outer sporomorph wall, or exine, is formed of a highly durable biopolymer called sporopollenin ( Brooks & Shaw, 1968 , 1978...
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Journal Article
Journal: Geology
Published: 01 December 2015
Geology (2015) 43 (12): 1067–1070.
... of an ozone (O 3 ) layer, plankton would have been subject to higher levels of ultraviolet radiation (UVR), in particular UV-C (100–280 nm) ( Cockell, 2000 ). Because DNA strongly absorbs at 254 nm, UV-C causes DNA strand breakage ( Sinha and Häder, 2002 ) and the formation of photoproducts...
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Journal Article
Published: 01 August 2022
Clays and Clay Minerals (2022) 70 (4): 555–565.
... its practical applications. The objective of the present study was to mitigate these problems by synthesizing the g-C 3 N 4 in the presence of exfoliated montmorillonite (Mnt). Compared with bulk montmorillonite, the specific surface area of exfoliated two-dimensional Mnt layers was significantly...
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Journal Article
Published: 01 January 2009
European Journal of Mineralogy (2009) 21 (1): 85–97.
... by Raman spectroscopy can be related to a specific absorption with apparent maximum in the range 405–568 nm, thus absorbing from violet to yellow–green. This is the first study of the precise relation between Raman and diffuse reflectance spectra of cultured freshwater pearls. * Corresponding author, e...
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