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Journal articles on the topic 'Suwannee'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Holcomb, Jordan M., Colin P. Shea, and Nathan A. Johnson. "Cumulative Spring Discharge and Survey Effort Influence Occupancy and Detection of a Threatened Freshwater Mussel, the Suwannee Moccasinshell." Journal of Fish and Wildlife Management 9, no. 1 (February 2, 2018): 95–105. http://dx.doi.org/10.3996/052017-jfwm-042.

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AbstractFreshwater mussels (Unionidae) are among the most imperiled groups of organisms in the world, and the lack of information regarding species distributions, life-history characteristics, and ecological and biological requirements may limit the protection of remaining mussel populations. We examined the influence of hydrologic factors on the occurrence of the Suwannee Moccasinshell Medionidus walkeri, a federally threatened freshwater mussel species, endemic to the Suwannee River Basin in Georgia and Florida. We also evaluated the influence of survey effort on detection of Suwannee Moccasinshell during field surveys. We compiled all recent (2013–2016) mussel survey records in the Suwannee River Basin. We calculated cumulative discharge contributed by upstream springs for each of 220 survey locations. We combined the spring discharge predictor variable with Suwannee Moccasinshell detection and nondetection data from each survey location to develop a suite of occupancy models. Modeling results indicated that detection of Suwannee Moccasinshell during surveys was strongly and positively related to survey effort. Modeling results also indicated that sites with cumulative spring discharge inputs exceeding ∼28 cubic meters per second were most likely (i.e., predicted occupancy probabilities >0.5) to support Suwannee Moccasinshell populations. However, occupancy declined in the lowermost reaches of the Suwannee mainstem despite high spring discharge inputs, presumably due to greater tidal influences and differences in physicochemical habitat conditions. Historical localities where Suwannee Moccasinshell has presumably been extirpated are all devoid of springs in their upstream watersheds. We hypothesize that springs may buffer extremely tannic, and at times polluted, surface waters, in addition to maintaining adequate flows during periods of drought, thereby promoting the persistence of Suwannee Moccasinshell populations. Our study suggests that springs are a critical resource for Suwannee Moccasinshell and may be more important for conservation planning than was previously recognized.

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2

Rajabi, Masoumeh, Melissa Jones, Michael Hubbard, Gary Rodrick, and Anita C. Wright. "Distribution and Genetic Diversity ofSalmonella entericain the Upper Suwannee River." International Journal of Microbiology 2011 (2011): 1–9. http://dx.doi.org/10.1155/2011/461321.

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The Suwannee River spans the Florida/Georgia border to the Gulf of Mexico, and contributes to regional irrigation and recreational activities. Association ofSalmonella entericawith these resources may result in the contamination of produce and disease outbreaks. Therefore, surface water was examined for the distribution ofS. entericaat multiple time points from 4 sites on the upper Suwannee River. Isolates were confirmed by detection of theinvAgene, and 96% of all samples were positive for the bacterium. Most probable number enumeration ranged from <18 to 5400 MPN/100 mL. Genetic diversity of these isolates (n=110) was compared to other environmental (n=47) or clinical (n=28) strains and to an online library (n=314) using DiversiLab rep-PCR. All strains showed >60% similarity and distributed into 16 rep-PCR genogroups. Most (74%) of the Suwannee River isolates were clustered into two genogroups that were comprised almost exclusively (97%) of just these isolates. Conversely, 85% of the clinical reference strains clustered into other genogroups. However, some Suwannee River isolates (12%) were clustered with these primarily clinically-associated genogroups, supporting the hypothesis that river water can serve as a disease reservoir and that pathogenic strains may persist or possibly originate from environmental sources.

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3

Thorn, Coben D., and Michael L. Falgiani. "Jumping Sturgeon in the Suwannee River." Wilderness & Environmental Medicine 24, no. 3 (September 2013): 298–99. http://dx.doi.org/10.1016/j.wem.2013.01.006.

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4

Ong, Kimberly J., Lindsey C. Felix, David Boyle, James D. Ede, Guibin Ma, Jonathan G. C. Veinot, and Greg G. Goss. "Humic acid ameliorates nanoparticle-induced developmental toxicity in zebrafish." Environmental Science: Nano 4, no. 1 (2017): 127–37. http://dx.doi.org/10.1039/c6en00408c.

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5

Loosli, Frédéric, Letícia Vitorazi, Jean-François Berret, and Serge Stoll. "Isothermal titration calorimetry as a powerful tool to quantify and better understand agglomeration mechanisms during interaction processes between TiO2 nanoparticles and humic acids." Environmental Science: Nano 2, no. 5 (2015): 541–50. http://dx.doi.org/10.1039/c5en00139k.

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6

Burnett, William C., James B. Cowart, and Suchint Deetae. "Radium in the Suwannee River and estuary." Biogeochemistry 10, no. 3 (July 1990): 237–55. http://dx.doi.org/10.1007/bf00003146.

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7

Carter, Burchard D., and Michael L. McKinney. "Eocene echinoids, the Suwannee Strait, and biogeographic taphonomy." Paleobiology 18, no. 3 (1992): 299–325. http://dx.doi.org/10.1017/s0094837300010861.

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Faunal similarity among regions is often used as a means of identifying regions of endemism in fossil faunas. At least two large-scale taphonomic effects can affect apparent faunal similarity: stratigraphic and facies mismatching. In stratigraphic mismatching, an unconformity represents removal of most or all of a complete assemblage zone in one region, and the constituent taxa are mistakenly interpreted as having never inhabited that region. In facies mismatching, environmental differences between two regions (possibly unrecognized) cause the inference of a barrier that never existed. The two types of mismatching can work in concert if a facies was originally represented in a single stratigraphic interval that has been completely removed from one region. Analysis of faunal similarity via multivariate analysis of individual localities, coupled with comparison of the regions as single samples, may indicate mismatching if the results differ significantly.We view these two problems as part of a suite of taphonomic effects that are not evident in paleobiological analyses of smaller geographic scope. First, there is ambiguity in the notion of “barrier,” even when a candidate is obvious. Second, barriers in paleobiogeography are often hidden and must be inferred from their effects rather than observed. Third, stratigraphic and facies mismatching produce effects on regional faunas similar to those produced by barriers. Anyone using barriers to explain faunal disruptions should address these three points.Upper Eocene faunas of central Florida seem taxonomically distinct from those of the remainder of the Gulf Coastal Plain. This has historically been attributed to a known paleogeographic feature, the Suwannee Strait, which acts as a barrier. The amount of dissimilarity of the echinoid faunas is greater than the amount predicted as a result of sampling problems. Comparison of the results of multivariate and whole-region analyses suggests that mismatching of the two faunas, rather than a true barrier, causes the distinction. Principally facies, but also strata are mismatched. Early Late Eocene faunas inhabited terrigenous sands to the north of the strait and carbonate sands to the south and show the highest distinctiveness. Middle Late Eocene faunas inhabited primarily carbonate sands to the south and both carbonate sands and muds to the north. Overall similarity is higher for both local and regional analyses, and the faunas of northern sands are more similar to those of the southern region than to the northern mud faunas. Overall similarity across the strait is highest in the late Late Eocene strata when both regions had carbonate mud and sand facies. The faunas exhibit greater similarity within facies than they do within regions. Upper Late Eocene strata are poorly preserved north of the strait because of post-Eocene erosion.

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8

Camp, Janey V., Dennis B. George, Martha J. M. Wells, and Pedro E. Arce. "Monitoring advanced oxidation of Suwannee River fulvic acid." Environmental Chemistry 7, no. 3 (2010): 225. http://dx.doi.org/10.1071/en09146.

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Environmental context.Potentially toxic disinfection by-products form when water containing humic and fulvic acids is chlorinated to destroy pathogenic microorganisms. A pulsed electrical discharge was examined for its ability to destroy an aquatic fulvic acid by oxidation. Spectroscopically, changes in the organic structures were observed, but carbon content and disinfection by-products were not reduced. Abstract.A pilot-scale pulsed electrical discharge (PED) system was used to treat Suwannee River fulvic acid (SRFA) as a representative precursor material for the formation of disinfection by-products (DBPs), specifically trihalomethane compounds. Ultraviolet-visible and fluorescence spectroscopy, dissolved organic carbon (DOC), and the trihalomethane formation potential (THMFP) were used as analytical parameters to monitor the effects of treatment on the substrate. The potential for SRFA degradation (5 mg L–1 DOC) was examined over 60 min at each of four operational configurations, varying pulse energy and frequency (0.15 J and 60 Hz, 0.15 J and 120 Hz, 0.4 J and 60 Hz, and 0.4 J and 120 Hz) in a factorial design. Statistically significant changes occurred for UV254, EX254EM460, and EX328EM460 under selected conditions; however, concomitant changes in DOC and THMFP were not observed. The composition of SRFA changed, but organic carbon was not mineralised to carbon dioxide. In addition to showing degradation by PED, the significance of the preliminary findings of this research was to demonstrate that spectroscopic monitoring of precursor degradation alone can be misleading, and that whereas ultraviolet-visible and fluorescence spectroscopy indicated degradation of precursor compounds, DOC and THMFP measurements were unchanged and did not support the occurrence of mineralisation in this system.

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9

Pollock, Jeffrey C., James P. Hibbard, and Cees R. van Staal. "A paleogeographical review of the peri-Gondwanan realm of the Appalachian orogen1This article is one of a series of papers published in this CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology." Canadian Journal of Earth Sciences 49, no. 1 (January 2012): 259–88. http://dx.doi.org/10.1139/e11-049.

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The eastern edge of the Appalachian orogen is composed of a collection of Neoproterozoic – early Paleozoic domains, Avalonia, Carolinia, Ganderia, Meguma, and Suwannee, which are exotic to North America. Differences in the geological histories of these peri-Gondwanan domains indicate that each separated independently from Gondwana, opening the Rheic Ocean in their wake. Cambrian departure of Ganderia and Carolina was followed by the Ordovician separation of Avalonia and Silurian separation of Meguma. After separation in the early Paleozoic, these domains constituted the borderline between the expanding Rheic Ocean and contracting Iapetus Ocean. They were transferred to Laurentia by early Silurian closure of Iapetus and Devonian–Carboniferous closure of the Rheic Ocean during the assembly of Gondwana and Laurentia into Pangaea. The first domain to arrive at Laurentia was Carolinia, which accreted in the Middle Ordovician during the Cherokee orogeny. Salinic accretion of Ganderia occurred shortly thereafter and was followed by the Acadian accretion of Avalonia. The Acadian orogeny was immediately followed by Middle Devonian – Early Carboniferous accretion of Meguma and possibly Suwannee which led to the Fammenian orogeny. The episodicity of orogeny suggests that the present location of these domains parallels their order of accretion. However, each of these crustal blocks was translated along strike by large-scale Late Devonian – Carboniferous dextral strike–slip motion. The breakup of Pangaea occurred outboard of the Paleozoic collision zones that accreted Carolinia, Ganderia, Avalonia, Meguma, and Suwannee to Laurentia, leaving these terranes appended to North America during the Mesozoic opening of the Atlantic.

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10

Leadon, Christopher J., and Orjan F. Wetterqvist. "Land acquisition criteria for the Suwannee river estuary, Florida." Coastal Zone Management Journal 14, no. 3 (January 1986): 217–39. http://dx.doi.org/10.1080/08920758609362003.

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11

Mason, William T., and James P. Clugston. "Foods of the Gulf Sturgeon in the Suwannee River, Florida." Transactions of the American Fisheries Society 122, no. 3 (May 1993): 378–85. http://dx.doi.org/10.1577/1548-8659(1993)122<0378:fotgsi>2.3.co;2.

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12

Foster, Ann M., and James P. Clugston. "Seasonal Migration of Gulf Sturgeon in the Suwannee River, Florida." Transactions of the American Fisheries Society 126, no. 2 (March 1997): 302–8. http://dx.doi.org/10.1577/1548-8659(1997)126<0302:smogsi>2.3.co;2.

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13

Yan, Mingquan, Mingyang Li, Dongsheng Wang, and Feng Xiao. "Optical property of iron binding to Suwannee River fulvic acid." Chemosphere 91, no. 7 (May 2013): 1042–48. http://dx.doi.org/10.1016/j.chemosphere.2013.01.069.

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14

Mason, William T. "A survey of benthic invertebrates in the Suwannee River, Florida." Environmental Monitoring and Assessment 16, no. 2 (February 1991): 163–87. http://dx.doi.org/10.1007/bf00418103.

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15

Yamamoto, H., and H. M. Liljestrand. "The fate of estrogenic compounds in the aquatic environment: sorption onto organic colloids." Water Science and Technology 47, no. 9 (May 1, 2003): 77–84. http://dx.doi.org/10.2166/wst.2003.0497.

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In this study, sorption of some estrogens and estrogenic compounds onto several organic colloids was examined using fluorescence quenching techniques. Selected organic colloids included humic substances of several sources, Aldrich humic acid (AHA), Suwannee River humic acid (SRHA), Suwannee River fulvic acid (SRFA), and Nordic fulvic acid (NFA). Polysaccharides, alginic acid (AA) and dextran (Dex), and tannic acid (TA) were also selected. 17β-estradiol (E2), 17α-ethynylestradiol (EES), and estriol (E3) were selected as estrogens. Nonylphenol (NP), octylphenol (OP), and dibutylphthalate (DBP) were selected as estrogenic compounds. For most of the selected compounds, the sorption coefficients were in the order of TA > humic acids (SRHA or AHA) > fulvic acids (NFA or SRFA) > AA. The smallest or no significant sorption onto dextran was found for selected estrogens and estrogenic compounds. Comparing those compounds, neither a significant trend nor linear correlation with Log Kow was found. The resulting sorption coefficients for humic substances and TA suggested approximately 15 to 50% of the estrogens and estrogenic compounds were bound in typical natural water of 5 mgTOC/L and significant effects on the removal of them by water treatment processes, toxicity, or bioavailability were suggested.

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16

Andersen, Peter C., and Charles A. Sims. "Yield and Quality of Vitis Hybrid `Suwannee' as Affected by Training System and Pruning Severity." HortScience 26, no. 4 (April 1991): 366–68. http://dx.doi.org/10.21273/hortsci.26.4.366.

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The influence of bilateral cordon (BC) and cane training systems and level of pruning severity on vegetative and reproductive characteristics of Vitis hybrid `Suwannee' were determined from 1987 to 1989. In 1987, yield and quality were similar on BC- and cane-trained vines. In 1988, shoot count, yield, and quality were similar regardless of training system and pruning severity (50, 70, or 90 nodes per vine). When data from both training systems were combined, yield was related to the number of shoots. Vines pruned more severely compensated by producing more shoots from non-count (non-node) positions on the canes, cordon, or spurs. Similarly, in 1989 yield and berry quality were not affected by training system or levels of pruning severity (50, 70, 90, or 110 nodes), although berry weight was affected by training system, and shoot count and shoot length were affected by level of pruning severity. Interactive effects of training system and pruning level were not significant in either year. An analysis of combined data for 1989 indicated that yield was affected by the number of nodes and shoots. Thus, `Suwannee' may be trained to the BC system, which is more readily adapted to mechanization. Pruning to a specific number of nodes per vine was not critical.

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17

Umbarger, Keelan F., and John W. Snedden. "Delineation of post-KPg carbonate slope deposits as a sedimentary record of the Paleogene linkage of De Soto Canyon and Suwannee Strait, northern Gulf of Mexico." Interpretation 4, no. 1 (February 1, 2016): SC51—SC61. http://dx.doi.org/10.1190/int-2015-0086.1.

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Seismicity generated from the Chicxulub impact has been postulated as the cause for the dramatic alteration of basin margin morphology and catastrophic movement of sediments in the Gulf of Mexico (GOM). Immediately following the impact, the formation of the Cretaceous-Paleogene boundary deposit (KPBD) was widespread and caused considerable erosion as portions of the Florida Escarpment collapsed, inducing sediment failure on the northern Florida Platform and formation of the ancestral De Soto Canyon. Overlying the more prominent KPBD existed a distinct, younger, post-Cretaceous/Paleogene carbonate slope deposit (CSD) confined within the De Soto Canyon bathymetric feature. Presence of this discrete unit provided insight into the post-impact history of De Soto Canyon and its long-duration connection to the Suwannee Strait, which linked the GOM with the Atlantic Ocean for almost 40 ma. We have postulated that the bathymetric low of the De Soto Canyon acted as a conduit for west to east sediment movement from nearby carbonate-dominated shorelines into the canyon in episodic sediment transport events from the Danian to the earliest Miocene. Closure of the Suwannee Strait, due to sediment infilling, terminated deposition of the De Soto Canyon CSD. This was followed by major siliciclastic influx as the paleo-Tennessee drainage system began to enter the Mississippi Canyon area.

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18

Arakawa, Neal, and Lihini Aluwihare. "Direct Identification of Diverse Alicyclic Terpenoids in Suwannee River Fulvic Acid." Environmental Science & Technology 49, no. 7 (March 27, 2015): 4097–105. http://dx.doi.org/10.1021/es5055176.

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19

Saleh, Farada Y., and David Y. Chang. "Retention behavior of suwannee river fulvic acid components in RP-HPLC." Science of The Total Environment 62 (January 1987): 67–74. http://dx.doi.org/10.1016/0048-9697(87)90483-9.

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20

Trout, Chad C., and James D. Kubicki. "Molecular modeling of Al3+ and benzene interactions with Suwannee fulvic acid." Geochimica et Cosmochimica Acta 71, no. 15 (August 2007): 3859–71. http://dx.doi.org/10.1016/j.gca.2007.05.017.

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21

Tootle, Glenn A., and Thomas C. Piechota. "SUWANNEE RIVER LONG RANGE STREAMFLOW FORECASTS BASED ON SEASONAL CLIMATE PREDICTORS." Journal of the American Water Resources Association 40, no. 2 (April 2004): 523–32. http://dx.doi.org/10.1111/j.1752-1688.2004.tb01047.x.

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22

Wang, Xuejun, Tao Lou, and Huixiang Xie. "Photochemical production of dissolved inorganic carbon from suwannee river humic acid." Chinese Journal of Oceanology and Limnology 27, no. 3 (September 2009): 570–73. http://dx.doi.org/10.1007/s00343-009-9156-5.

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23

Dryer, D. J., G. V. Korshin, A. Heitz, and C. Joll. "Characterization of proton and copper binding properties of natural organic matter from an Australian drinking water source by differential absorbance spectroscopy." Water Supply 8, no. 6 (December 1, 2008): 611–14. http://dx.doi.org/10.2166/ws.2008.140.

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This study examined the effects of changes in pH and copper concentration on the absorbance spectra of natural organic matter (NOM) from a reservoir in Western Australia. Differential absorbance spectra generated for this NOM under changing pH and copper concentration conditions revealed features that could be correlated to the activity of distinct types of chromophores. A comparison of results with those generated for experiments with standard Suwannee River fulvic acid highlighted important differences in chemistry between the two samples.

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24

Trubetskoy, O. A., and O. E. Trubetskaya. "Analysis of fluorophores of organic substances dissolved in Suvani river water using reversed-phase liquid chromatography." Водные ресурсы 46, no. 4 (August 21, 2019): 428–37. http://dx.doi.org/10.31857/s0321-0596464428-437.

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Reversed-phase high-efficiency liquid chromatography was used in combination with detection by multiwave fluorescence for analysis of organic substances dissolved in natural water of the Suwannee River. Also analyzed were the stable electrophoretic fractions А, В, and C+D, obtained by a combination of preparative size-exclusion chromatography and analytical electrophoresis in a polyacrylamide gel. Fraction А has the largest molecular size, and fraction C+D, the smallest. Using 3D fluorescent analysis, humic-like fluorescence was detected both in the original sample and in all fractions; protein-like fluorescence is almost fully localized in fractions А and В of the largest and middle molecular sizes. The wide peak of humic-like fluorescence is split into several groups of fluorophores with different emissions maxima (435, 455, 460, and 465 nm) and degrees of hydrophobicity. The obtained results were analyzed in relation to contemporary theories of formation of humic-like fluorescence of dissolved organic substances. The low-molecular free aromatic amino acids tyrosine and tryptophan were identified in fractions А and В of the highest molecular size and constitute >50% of the protein-like fluorescence of the organic substances dissolved in the Suwannee River water. The data obtained ensure better understanding of the molecular nature of protein-like and humic-like fluorescence of organic substance dissolved in natural water.

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25

Sulak, Kenneth J., and James P. Clugston. "Early Life History Stages of Gulf Sturgeon in the Suwannee River, Florida." Transactions of the American Fisheries Society 127, no. 5 (September 1998): 758–71. http://dx.doi.org/10.1577/1548-8659(1998)127<0758:elhsog>2.0.co;2.

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26

Bonvechio, Timothy F., Kimberly I. Bonvechio, and Richard L. Cailteux. "Proposed Standard Weight (Ws) Equation and Standard Length Categories for Suwannee Bass." North American Journal of Fisheries Management 30, no. 4 (August 2010): 983–88. http://dx.doi.org/10.1577/m10-034.1.

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27

Cabaniss, S. E., and M. S. Shuman. "Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria." Geochimica et Cosmochimica Acta 52, no. 1 (January 1988): 185–93. http://dx.doi.org/10.1016/0016-7037(88)90066-x.

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28

Levy, Jacqueline L., Hao Zhang, William Davison, Josep Galceran, and Jaume Puy. "Kinetic Signatures of Metals in the Presence of Suwannee River Fulvic Acid." Environmental Science & Technology 46, no. 6 (March 7, 2012): 3335–42. http://dx.doi.org/10.1021/es2043068.

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29

Li, Yan, Mourad Harir, Marianna Lucio, Basem Kanawati, Kirill Smirnov, Ruth Flerus, Boris P. Koch, Philippe Schmitt-Kopplin, and Norbert Hertkorn. "Proposed Guidelines for Solid Phase Extraction of Suwannee River Dissolved Organic Matter." Analytical Chemistry 88, no. 13 (June 23, 2016): 6680–88. http://dx.doi.org/10.1021/acs.analchem.5b04501.

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30

Bonvechio, Timothy F., Micheal S. Allen, and Richard L. Cailteux. "Relative Abundance, Growth, and Mortality of Suwannee Bass in Four Florida Rivers." North American Journal of Fisheries Management 25, no. 1 (February 2005): 275–83. http://dx.doi.org/10.1577/m03-161.1.

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31

Maurice, Patricia A. "Special Issue Introduction: Dissolved Organic Matter from the Suwannee River (GA, USA)." Environmental Engineering Science 32, no. 1 (January 2015): 1–3. http://dx.doi.org/10.1089/ees.2014.1502.

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32

Yates III, Leland M., and R. von Wandruszka. "Functional group analysis of Suwannee River fulvic acid with reactive fluorescent probes." Fresenius' Journal of Analytical Chemistry 364, no. 8 (August 18, 1999): 746–48. http://dx.doi.org/10.1007/s002160051425.

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33

Serkiz, Steven M., and E. Michael Perdue. "Isolation of dissolved organic matter from the suwannee river using reverse osmosis." Water Research 24, no. 7 (July 1990): 911–16. http://dx.doi.org/10.1016/0043-1354(90)90142-s.

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34

Wilson, Sandra B., Gary W. Knox, Keona L. Nolan, and James Aldrich. "Landscape Performance and Fruiting of 12 Privet Selections Grown in Northern and Southern Florida." HortTechnology 24, no. 1 (February 2014): 148–55. http://dx.doi.org/10.21273/horttech.24.1.148.

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Chinese privet (Ligustrum sinense) and glossy privet (L. lucidum) have been classified as Category I invasives in Florida. The closely related japanese privet (L. japonicum) has escaped cultivation but is not considered a problem species in Florida. Plant growth, visual quality, flowering, and fruiting were assessed for the resident species (wild-type form) and selected cultivars of chinese privet, glossy privet, and japanese privet planted in northern and southern Florida for 132 weeks. Visual quality varied by site, month, and cultivar. With the exception of ‘Swift Creek’ chinese privet (which did not survive in southern Florida), all cultivars survived the study. All plants fruited in northern Florida. In southern Florida, fruiting was less abundant and not observed for ‘Jack Frost’ japanese privet, ‘Rotundifolium’ japanese privet, ‘Swift Creek’ chinese privet, ‘Suwannee River’ hybrid privet, and glossy privet within 132 weeks. In northern and southern Florida, the growth index rate was lower for ‘Lake Tresca’ japanese privet, ‘Rotundifolium’ japanese privet, and ‘Suwannee River’ hybrid privet than other cultivars. There was a significant interaction between temperature and species for seed germination. Germination in incubators set with a 12-hour photoperiod ranged from 51% to 78.5% for chinese privet, japanese privet, and glossy privet among temperatures, with the exception of glossy privet at 35/25 °C, where only 2.0% of seeds germinated. Germination in complete darkness ranged from 39.5% to 80.5% for chinese privet and glossy privet among temperatures, with the exception of glossy privet at 35/25 °C, where only 0.5% of seeds germinated.

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35

Washenfelder, R. A., J. M. Flores, C. A. Brock, S. S. Brown, and Y. Rudich. "Broadband measurements of aerosol extinction in the ultraviolet spectral region." Atmospheric Measurement Techniques Discussions 6, no. 1 (January 3, 2013): 113–57. http://dx.doi.org/10.5194/amtd-6-113-2013.

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Abstract. Aerosols influence the Earth's radiative budget by scattering and absorbing incoming solar radiation. The optical properties of aerosols vary as a function of wavelength, but few measurements have reported the wavelength dependence of aerosol extinction cross-sections and complex refractive indices. We describe a new laboratory instrument to measure aerosol optical extinction as a function of wavelength, using cavity enhanced spectroscopy with a broadband light source. The instrument consists of two broadband channels which span the 360–390 and 385–420 nm spectral regions using two light emitting diodes (LED) and a grating spectrometer with charge-coupled device (CCD) detector. We determined aerosol extinction cross-sections and directly observed Mie scattering resonances for aerosols that are purely scattering (polystyrene latex spheres and ammonium sulfate), slightly absorbing (Suwannee River fulvic acid), and strongly absorbing (nigrosin dye). We describe an approach for retrieving refractive indices as a function of wavelength from the measured extinction cross-sections over the 360–420 nm wavelength region. The retrieved refractive indices for PSL and ammonium sulfate agree within uncertainty with literature values for this spectral region. The refractive index determined for nigrosin is 1.78 (±0.03) + 0.19 (±0.08) i at 360 nm and 1.53 (±0.03) + 0.21 (±0.05) i at 420 nm. The refractive index determined for Suwannee River fulvic acid is 1.71 (±0.02) + 0.07 (±0.06) i at 360 nm and 1.66 (±0.02) + 0.06 (±0.04) i at 420 nm. These laboratory results support the potential for a field instrument capable of determining ambient aerosol optical extinction, average aerosol extinction cross-section, and complex refractive index as a function of wavelength.

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36

Nnaji, Gideon A., Wenrui Huang, Margaret W. Gitau, and Clayton Clark. "Frequency Analysis of Minimum Ecological Flow and Gage Height in Suwannee River, Florida." Journal of Coastal Research 68 (November 2014): 152–59. http://dx.doi.org/10.2112/si68-020.1.

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37

Leenheer, J. A., G. K. Brown, P. MacCarthy, and S. E. Cabaniss. "Models of Metal Binding Structures in Fulvic Acid from the Suwannee River, Georgia." Environmental Science & Technology 32, no. 16 (August 1998): 2410–16. http://dx.doi.org/10.1021/es9708979.

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38

Heatherington, A. L., and P. A. Mueller. "Mesozoic Igneous Activity in the Suwannee Terrane, Southeastern USA: Petrogenesis and Gondwanan Affinities." Gondwana Research 6, no. 2 (April 2003): 296–311. http://dx.doi.org/10.1016/s1342-937x(05)70979-5.

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39

Mossa, J., and J. Konwinski. "Thalweg variability at bridges along a large karst river: the Suwannee River, Florida." Engineering Geology 49, no. 1 (February 1998): 15–30. http://dx.doi.org/10.1016/s0013-7952(97)00034-3.

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40

Ginwalla, Arwa S., and Michael A. Mikita. "Reaction of Suwannee River Fulvic Acid with Chloramine: Characterization of Products via15N NMR." Environmental Science & Technology 26, no. 6 (June 1992): 1148–50. http://dx.doi.org/10.1021/es50002a601.

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41

Katz, Brian G., Rodney S. DeHan, Joshua J. Hirten, and John S. Catches. "INTERACTIONS BETWEEN GROUND WATER AND SURFACE WATER IN THE SUWANNEE RIVER BASIN, FLORIDA." Journal of the American Water Resources Association 33, no. 6 (December 1997): 1237–54. http://dx.doi.org/10.1111/j.1752-1688.1997.tb03549.x.

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42

Mueller, Paul A., Ann L. Heatherington, David A. Foster, William A. Thomas, and Joseph L. Wooden. "The Suwannee suture: Significance for Gondwana-Laurentia terrane transfer and formation of Pangaea." Gondwana Research 26, no. 1 (July 2014): 365–73. http://dx.doi.org/10.1016/j.gr.2013.06.018.

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43

Washenfelder, R. A., J. M. Flores, C. A. Brock, S. S. Brown, and Y. Rudich. "Broadband measurements of aerosol extinction in the ultraviolet spectral region." Atmospheric Measurement Techniques 6, no. 4 (April 3, 2013): 861–77. http://dx.doi.org/10.5194/amt-6-861-2013.

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Abstract. Aerosols influence the Earth's radiative budget by scattering and absorbing incoming solar radiation. The optical properties of aerosols vary as a function of wavelength, but few measurements have reported the wavelength dependence of aerosol extinction cross sections and complex refractive indices. We describe a new laboratory instrument to measure aerosol optical extinction as a function of wavelength, using cavity enhanced spectroscopy with a broadband light source. The instrument consists of two broadband channels which span the 360–390 and 385–420 nm spectral regions using two light emitting diodes (LED) and a grating spectrometer with charge-coupled device (CCD) detector. We determined aerosol extinction cross sections and directly observed Mie scattering resonances for aerosols that are purely scattering (polystyrene latex spheres and ammonium sulfate), slightly absorbing (Suwannee River fulvic acid), and strongly absorbing (nigrosin dye). We describe an approach for retrieving refractive indices as a function of wavelength from the measured extinction cross sections over the 360–420 nm wavelength region. The retrieved refractive indices for PSL and ammonium sulfate agree within uncertainty with the literature values for this spectral region. The refractive index determined for nigrosin is 1.78 (± 0.03) + 0.19 (± 0.08)i at 360 nm and 1.63 (± 0.03) + 0.21 (± 0.05)i at 420 nm. The refractive index determined for Suwannee River fulvic acid is 1.71 (± 0.02) + 0.07 (± 0.06)i at 360 nm and 1.66 (± 0.02) + 0.06 (± 0.04)i at 420 nm. These laboratory results support the potential for a field instrument capable of determining ambient aerosol optical extinction, average aerosol extinction cross section, and complex refractive index as a function of wavelength.

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Yang, Xin Yao, Shi Huai Deng, Fang Min Chen, Raymond Flynn, Frank von der Kammer, and Thilo Hofmann. "Comparing the Influence of Two Different Natural Organic Matter Types on Colloid Deposition in Saturated Porous Medium." Advanced Materials Research 455-456 (January 2012): 1324–29. http://dx.doi.org/10.4028/www.scientific.net/amr.455-456.1324.

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Humic acid and protein are two major organic matter types encountered in natural and polluted environment, respectively. This study employed Triple Pulse Experiments (TPEs) to investigate and compare the influence of Suwannee River Humic Acid (SRHA) (model humic acid) and Bovine Serum Albumin (BSA) (model protein) on colloid deposition in a column packed with saturated iron oxide-coated quartz sand. Study results suggest that adsorbed SRHA may inhibit colloid deposition by occupying colloid sites on the porous medium. Conversely, BSA may promote colloid deposition by a ‘filter ripening’ mechanism. This study provides insight to understand the complex behavior of colloids in organic matter-presented aquifers and sand filters.

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Amirtharajah, A., K. E. Dennett, and Anne Studstill. "Ferric Chloride Coagulation for Removal of Dissolved Organic Matter and Trihalomethane Precursors." Water Science and Technology 27, no. 11 (June 1, 1993): 113–21. http://dx.doi.org/10.2166/wst.1993.0270.

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Ferric chloride coagulation of two types of natural dissolved organic matter was studied. The molecular weight distribution of Suwannee River humic substances currently used as an international standard was characterized using fast atom bombardment mass spectrometry (FABMS). The molecular weight distributions were characterized before and after coagulation. Ferric chloride dosage and pH domains on the iron coaglation diagrams were developed for removal of these humic substances and for determination of the resulting trihalomethane formation potentials (THMFP) of the treated water. The results indicate that it is possible to maximize the removal of dissolved organic matter and minimize trihalomethanes by coagulation only under very specific conditions of pH and ferric chloride dosage.

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Fattahi, Alireza, and Touradj Solouki. "Using solution equilibria to determine average molecular weight of the Suwannee River fulvic acids." Analytica Chimica Acta 496, no. 1-2 (October 2003): 325–37. http://dx.doi.org/10.1016/s0003-2670(03)01010-9.

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Niu, Xi-Zhi, Mourad Harir, Philippe Schmitt-Kopplin, and Jean-Philippe Croué. "Sunlight-induced phototransformation of transphilic and hydrophobic fractions of Suwannee River dissolved organic matter." Science of The Total Environment 694 (December 2019): 133737. http://dx.doi.org/10.1016/j.scitotenv.2019.133737.

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Haiber, S., H. Herzog, P. Burba, B. Gosciniak, and J. Lambert. "Two-Dimensional NMR Studies of Size Fractionated Suwannee River Fulvic and Humic Acid Reference." Environmental Science & Technology 35, no. 21 (November 2001): 4289–94. http://dx.doi.org/10.1021/es010033u.

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Randall, M. T., and K. J. Sulak. "Evidence of autumn spawning in Suwannee River Gulf sturgeon, Acipenser oxyrinchus desotoi (Vladykov, 1955)." Journal of Applied Ichthyology 28, no. 4 (March 3, 2012): 489–95. http://dx.doi.org/10.1111/j.1439-0426.2012.01960.x.

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50

Gutierrez, Leonardo, and Thanh H. Nguyen. "Interactions between Rotavirus and Suwannee River Organic Matter: Aggregation, Deposition, and Adhesion Force Measurement." Environmental Science & Technology 46, no. 16 (August 10, 2012): 8705–13. http://dx.doi.org/10.1021/es301336u.

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