ESTABLISHING THE NATURAL RANGE OF DISSOLVED OXYGEN LEVELS IN STREAMS OF THE SOUTHERN COASTAL PLAIN OF GEORGIA

2013 ◽  
Author(s):  
G. Vellidis ◽  
R. Lowrance ◽  
M.C. Smith ◽  
A.W. Milton
1987 ◽  
Vol 19 (5-6) ◽  
pp. 823-832 ◽  
Author(s):  
J. M. Salomão

Following surveys recently carried out in Maputo estuary, a survey with the purpose of acquiring data required to characterize the estuary was carried out in December 1983. After reviewing the hydrology of the tributaries to the estuary, the parameters to be monitored - salinity, conductivity, temperature, and dissolved oxygen, are referred. Finally, taking also into account previous information available, an evaluation of the results, and an assessment of the estuary are done. The estuary can be classified as well mixed, since the vertical salinity gradients found are small. The Umbeluzi estuary, however, is partially mixed. Temperature decreases with the depth, and when moving downstream. Some pollution was found along the lower part of the estuary, probably due to the discharge of domestic and industrial wastewater, which brings the dissolved oxygen figures below the saturation level. As for the upper part of the estuary, the dissolved oxygen levels are not only dependent on the pollutant load, but also on the growing of algae, which by photosynthesis under daylight produce oxygen that dissolves into the water. Quite often, the dissolved oxygen figures are above the saturation level. The growth of algae could be due to the input of phosphorus and nitrogen brought in by the tributary streams. A pollutant load discharged upstream could be the reason for some pollution seen in the Umbeluzi estuary.


1989 ◽  
Vol 16 (3) ◽  
pp. 308-316 ◽  
Author(s):  
C. A. Town ◽  
D. S. Mavinic ◽  
B. Moore

Urban encroachment and intensive agricultural activity within the Serpentine–Nicomekl watershed (near Vancouver, B.C.) have caused a series of fish (salmon) kills on the Serpentine River since 1980. Low dissolved oxygen was responsible for these kills. This field project investigated some of the dynamic chemical and biological relationships within the river, as well as the use of an instream aerator as a temporary, in situ, water quality improvement measure. Weekly sampling for a 6-month period during the latter half of 1985 established a solid data base for deriving and interpreting meaningful interrelationships. A strong correlation between chlorophyll a and dissolved oxygen levels before the algae die-off supported the hypothesis that algae blooms dying in the fall could create a serious oxygen demand. Because of these environmental conditions, the river is unable to sustain healthy dissolved oxygen levels during this period. As such, a prototype, 460 m artificial aeration line was designed, installed, and monitored to evaluate its potential for alleviating low dissolved oxygen conditions and improving overall water quality during the critical fall period.The instream aerator ran continuously for over 2 months, starting in September 1985. Despite better-than-expected weather conditions (i.e., cool, wet weather) and relatively high dissolved oxygen levels during the fall of 1985, the data base appeared to support the use of this prototype aeration unit as a means of "upgrading" a stretch of an urban river subject to periodic, low dissolved oxygen levels. As a result, a 2-year follow-up study and river monitoring was initiated. In both 1986 and 1987, late summer and early fall river conditions resulted in the potential for serious salmon kills, due to higher-than-normal river temperatures and very low dissolved oxygen. In both instances, the instream aerator prevented such fish kills in a key stretch of the river. Expansion of the system to include other critical stretches of the Serpentine and other urban river systems, near Vancouver, is being considered. Key words: algae, aerator, chlorophyll a, eutrophic, fish kills, instream aeration, river improvement, urban river.


2019 ◽  
pp. 180-199
Author(s):  
Renata Cardia Rebouças ◽  
Felipe Castro

RESUMO:A classificação de ambientes costeiros pode ser uma tarefa complexa. O estudo da geomorfologia na identificação de ambientes sedimentares necessita de uma validação. Não raro, feições como cordões litorâneos são confundidas com dunas. O depósito sedimentar em forma de dunas fica melhor caracterizado quando realizados estudos sedimentológicos, nos quais são observados os parâmetros granulométricos e a morfoscopia dos grãos. Neste trabalho estes métodos clássicos de sedimentologia foram aplicados aos sedimentos de testemunhos coletados na planície costeira da localidade de Mosqueiro (SE). A análise granulométrica e morfoscópica mostrou que, apesar de os sedimentos possuírem algumas características peculiares às areias de dunas, como uma granulometria fina, assimetria positiva tendendo para os finos e distribuição leptocúrtica da curva gaussiana, os sedimentos apresentam outras características como a seleção moderada e a superfície predominantemente polida que indicam que estes depósitos não foram formados exclusivamente pelo transporte eólico. O transporte misto, ora pela água, ora pelo vento, aponta para um ambiente de cordões litorâneos. Embora estes depósitos não tenham sido considerados dunas, é importante não construir na faixa de variação natural da praia para se evitar problemas com erosão costeira, bem como garantir a conservação ambiental e a segurança das pessoas e do patrimônio.Palavras-chave: Granulometria; Morfoscopia; Dunas; Cordões Litorâneos. ABSTRACT:The classification of coastal environments could be a complex task. The study of geomorphology in the identification of sedimentary environments requires validation. Often, features like beach ridges are confused with dunes. The sedimentary deposit in the form of dunes is better characterized when sedimentological studies are carried out, in which granulometric parameters and grain morphoscopy are observed. In this work, these classical methods of sedimentology were applied to the sediments of the samples collected in the coastal plain of Mosqueiro (SE). The granulometric and morphoscopic analysis showed that, although the sediments have some characteristics peculiar to the sand dunes, such as fine granulometry, positive asymmetry tending to the fines and leptokurtic distribution of the Gaussian curve, the sediments present other characteristics such as moderate selection and surface that indicate that these deposits were not formed exclusively by the wind transport. The mixed transport, sometimes by the water, or by the wind, points to an environment of coastal strings. Although these deposits have not been considered as dunes, it is important not to build on the natural range of the beach to avoid problems with coastal erosion, as well as to guarantee environmental conservation and the safety of people and property.Keywords: Granulometry; Morphoscopy; Dune; Beach Ridges.


1970 ◽  
Vol 19 (5) ◽  
pp. 800-804 ◽  
Author(s):  
Bernard Heinemann ◽  
Alma J. Howard ◽  
Henry J. Palocz

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