990 resultados para WELLS-DAWSON


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The purpose of the investigation is to make a detailed study of the geology and ground water in the Ruskin area, especially as related to the problem of salt-water encroachment. The major objectives of the program includes: (1) An inventory of wells to determine their number and distribution, their depths and diameters, and other pertinent information. (2) A study of artesian pressures. (3) Analyses of water from selected wells to determine the location and extent of any areas in which the artesian water is salty. (4) A study of the surface and subsurface geology as related to the occurrence and movement of ground water. (5) An estimate of the quantity of ground water withdrawn. (PDF contains 24 pages.)

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Salt-water encroachment is undoubtedly the problem of most concern to users of ground water in Florida. This is a problem in many coastal areas where water levels are lowered excessively by heavy pumping. It is a problem also in some inland areas where the water-bearing formations contain salty water at relatively shallow depths. Among the coastal areas where wells have become contaminated with salt water are Pinellas County and the Miami area of Dade County. Inland areas where wells are likely to become contaminated with salt water include Seminole County and the southwestern part of Volusia County. The purpose of the investigation is to make a detailed study of the geology and ground-water resources of the county with special emphasis on the problems associated with declining water levels and salt-water contamination. This report reviews briefly the progress of the investigation through February 1954. (PDF contains 43 pages.)

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Recently there has been much activity in reclaiming the low-lying coastal areas of Dade County for residential use, by the addition of fill. The fill is obtained by digging canals both normal to and parallel to Biscayne Bay. The canals serve the additional purpose of providing an access to the Bay for boats. A problem needing to be considered is the effect that these canals will have on the ground-water resources. It is expected that the canals will have little effect on ground water in parts of the county distant from the coast, but their effect in coastal areas is a matter of concern. In order to predict what, may happen in the vicinity of these new canals if they are not equipped with adequate control structures, it is instructive to review what has happened in the vicinity of similar canals in the past. The U. S. Geological Survey, in cooperation with Dade County, the cities of Miami and Miami Beach, the Central and Southern Florida Flood Control District, and the Florida Geological Survey has collected water-level and salinity data on wells and canals in Dade County since 1939. Some of the agencies named, and others, collected similar data before 1939. Analysis of all the data shows that sea water in the Atlantic Ocean and Biscayne Bayis the sole source of salt-water contamination in the Biscayne aquifer of the Dade County area. (PDF has 19 pages.)

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In December 1956 the U. S. Geological Survey, in cooperation with the Florida Geological Survey and the Board of County Commissioners of Pinellas County, collected waterlevel and chloride content of water in 94 wells in Pinellas County. First sampled in 1947, resampling and reanalyzing the water from these wells was used to determine the change in the chloride content of the ground water from 1947 to 1956. The chloride content of ground water is generally a reliable indication of the contamination of ground water by sea water, as 90 percent of the dissolved solids of sea water are chloride salts. (PDF contains 15 pages.)

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In the area of this investigation a partial inventory was made of the estimated 2,000 existing wells to obtain information on location, depth, and yield of representative wells. Also, data were obtained on the quality of water from the various aquifers, and on the fluctuation of water levels in certain wells in the Floridan aquifer. The hydraulic characteristics of the Floridan aquifer at several sites were determined by means of pumping tests. (PDF has 80 pages.)

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Practically all water for municipal and industrial use in the Fernandina area is supplied by artesian wells. In recent years, the use of artesian water in the area has increased to meet the needs of expanding industry and increasing population. The total industrial and municipal pumpage has increased from approximately 35 million gallons per day in 1941 to approximately 50 million gallons per day in 1959. Correlated with the increase in water use is the constant decline in the artesian pressure in the area. In many other areas in Florida, such a decline in artesian pressure has resulted in salt-water intrusion into the fresh-water supply.An intrusion of salt water in the Fernandina area would contaminate the existing fresh-water supply and would result in a hardship for the population and seriously injure the economy. Recognizing the threat to the fresh-water supplies of this area, the U. S. Geological Survey in cooperation with the Florida Geological Surveymade a reconnaissance to determineif there has been any intrusion of salt water into the fresh-water supply or if there is any danger of future intrusion. (PDF contains 28 pages.)

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Variable watermilfoil (Myriophyllum heterophyllum Michx.) has recently become a problem in Bashan Lake, East Haddam, CT, USA. By 1998, approximately 4 ha of the 110 ha lake was covered with variable watermilfoil. In 1999, the milfoil was spot treated with Aquacide®, an 18% active ingredient of the sodium salt of 2,4-D [(2,4-dichlorophenoxy) acetic acid], applied at a rate of 114 kg/ha. Aquacide® was used because labeling regarding domestic water intakes and irrigation limitations prevented the use of Navigate® or AquaKleen®, a 19% active ingredient of the butoxyethyl ester of 2,4-D. Variable watermilfoil was partially controlled in shallow protected coves but little control occurred in deeper more exposed locations. 2,4-D levels in the treatment sites were lower than desired and offsite dilution was rapid. In 2000, the United States Environmental Protection Agency (USEPA) issued a special local need (SLN) registration to allow the use of Navigate ® or AquaKleen® in lakes with potable and irrigation water intakes. Navigate® was applied at a rate of 227 kg/ha to the same areas as treated in 1999. An additional 2 ha of variable watermilfoil was treated with Navigate® in 2001, and 0.4 ha was treated in mid-September. Dilution of the 2,4-D ester formulation to untreated areas was slower than with the salt formulation. Concentrations of 2,4-D exceeded 1000 μg/ L in several lake water samples in 2000 but not 2001. Nearly all of the treated variable watermilfoil was controlled in both years. The mid-September treatment appeared as effective as the spring and early summer treatments. Testing of homeowner wells in all 3 years found no detectable levels of 2,4-D.(PDF contains 8 pages.)

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El 29 de abril del año próximo pasado se cumplieron veinte años del fallecimiento de Raúl Adolfo Ringuelet, quién fuera uno de los científicos más destacados que han dado las ciencias naturales de la Argentina. Salvo contadas excepciones, no hubo recordatorios sobre este acontecimiento, pero el Dr. Ringuelet es uno de los casos que no necesita de la magnanimidad y el tiempo de los mortales para tenerlo presente, ya que la vigencia y el peso de su obra, hacen cumplir con aquello de que “mientras el recuerdo permanece, la muerte no existe”. El Programa para el Estudio y Uso Sustentable de la Biota Austral (ProBiota) quiere recordarlo reproduciendo la publicación de una serie de conferencias dictadas en su juventud, durante 1943 y 1944, en LS 11 Radio Provincia de Buenos Aires y que fueron publicadas en 1946 bajo el título de “Temas de Ciencias Naturales”. En ese año, Raúl A. Ringuelet contaba con treinta dos años y el mundo se encontraba en su mayor parte lacerado y bajo ruinas por la conducta recurrente de la “especie hipócrita” que, en nombre de las ideologías y la paz universal, había concretado la matanza de varios millones de personas. En nuestro país se asistía al nacimiento de un nuevo movimiento histórico y el comienzo de profundos desencuentros en nuestra sociedad, los cuales, lamentablemente, aún no han terminado. En esta década la ciencia argentina sería destacada con el Premio Nóbel a través del Dr. Bernardo Houssay y en las ciencias naturales se habían publicado, entre otras obras, los rasgos principales de la Fitogeografía argentina de J. Frenguelli, la Zoogeografía de Cabrera y Yepes, la última entrega del catalógo sistemático de las aves de Argentina de Steullet y Deautier, y el estudio de la Selva Marginal de Punta Lara de A. L. Cabrera (hijo) y G. Dawson. La lectura de estas conferencias, un total de diez, nos muestra, ya entonces, el espíritu rico, inquieto y polifacético de Raúl A. Ringuelet, el cuál lo distinguiría pocos años después. En algunas de ellas realiza la reseña de la vida y obra de diferentes científicos y naturalistas de nuestro país; en las restantes, expresa ingeniosamente conceptos precursores sobre biodiversidad, conservación y manejo de los recursos naturales y su transferencia a los diferentes niveles de la sociedad. Finalmente, desde ProBiota consideramos que la trascripción de este tipo de documentos constituye un aporte para aquellos interesados en la historia de las ciencias naturales y, asimismo, una contribución para que nuestras jóvenes generaciones de biólogos y naturalistas posean una noción más clara de quienes marcaron rumbos e hicieron escuela en nuestra disciplina con un genuino sentido nacional.

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During the late 1980s to early 1990s a range of aquatic habitats in the central North Island of New Zealand were invaded by the filamentous green alga, water net Hydrodictyon reticulatum (Linn. Lagerheim). The alga caused significant economic and recreational impacts at major sites of infestation, but it was also associated with enhanced invertebrate numbers and was the likely cause of an improvement in the trout fishery. The causes of prolific growth of water net and the range of control options pursued are reviewed. The possible causes of its sudden decline in 1995 are considered, including physical factors, increase in grazer pressure, disease, and loss of genetic vigour.

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文章建立并求解了不同线性组合边界条件下的煤层气井不定常渗流模型,得到了井底压力和压力导数的理论曲线,以及压力场分布图。在不稳定流动的早期,压力和压力导数曲线都是斜率为1的直线段。当流体流动进入稳定流动状态时,在压力导数曲线上出现一个值为0.5的水平直线段。在理论曲线的晚期,理论曲线与边界性质存在密切关系。对于全封闭煤层气藏,所有压力和压力导数曲线是斜率为1的直线段。对于存在定压边界煤层气藏,压力双对数曲线的晚期是水平直线段,压力导数双对数曲线的晚期都是急剧下掉的曲线。但是混合边界的压力导数存在上翘现象,上翘程度和早晚与封闭边界的数目多少以及距离大小有关。压力场中,在靠近封闭边界的等压线垂直于边界,在靠近定压边界的等压线平行于边界。在邻近定压和封闭边界交合处,定压边界起主导作用。所得到的理论曲线可以直接应用于煤层气田的试井测试资料分析,压力场分布图对了解煤层气藏的开发状况有积极的意义。

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The Floridan aquifer was found to be principal source of ground water in the area, containing artesian water in the northern part of Columbia County, and being recharged in the southern part of the county. A few wells in the northern part of the county tap water present in sediments that lie above the Floridan aquifer. These shallow waters are generally high in iron and tannic acid. The details on the geology and hydrology necessary to conserve and utilize the water available to the residents of Columbia County are presented in this study. (PDF contains 86 pages)

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The Oakland Park area obtains its water from the Biscayne aquifer, S composed of very permeable and porous, sandy limestones. The per- 3 meability of the aquifer increases with depth, and wells in the area <\ generally obtain water at depths ranging from 60 to 80 feet, or between S 100 and 200 feet, depending on the quantity of water desired. The data presented in this paper can be used for further development of water and wise management of resources in the area. Large quantities S of ground water are still available at Oakland Park, if salt-water encroachment can be controlled. The data in this study provide the necessary information to begin an effective water management program. (PDF has 49 pages)