16,045 research outputs found

    Ecological characterization of the Florida springs coast: Pithlachascotee to Waccasassa Rivers

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    This report covers the upper coast of west-central Florida. This region includes the drainage basins and nearshore waters of the west coast of Florida between, but not including, the Anclote River basin and the Suwannee River basin. The name Springs Coast wash chosen because this area contains a multitude of springs, both named and too small or inaccessible to have been names. Much of the area is karstic limestone. Most recognizable among the springs are the famous Crystal river, Weeki Wachee, and Homosassa. This territory includes large expanses of marsh and wetland and, along its shores, the southern end of the largest area of seagrass beds in the state -- the Florida Big Bend Seagrass Beds preserve. It also possesses numerous spring-fed rivers and streams along the coast, whose constant discharges provide unique, relatively stable estuarine environments. This document is a summary of the available information on the Springs Coast area of Florida, for use by planners, developers, regulatory authorities, and other interested parties. An understanding of the factors affecting their plans and the possibly unexpected impacts of their actions on others will, it is hoped, promote intelligent development in areas capable of supporting it. We have tried to provide a clear, coherent picture of what is currently known about how the physical, chemical, and biological factors of the environment interact. (343 pp.

    The Deuterium to Hydrogen Abundance Ratio Towards a Fourth QSO: HS0105+1619

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    We report the measurement of the primordial D/H abundance ratio towards QSO \object. The column density of the hydrogen in the z≃2.536z \simeq 2.536 Lyman limit system is high, \lnhi =19.422±0.009= 19.422 \pm 0.009 \cmm, allowing for the deuterium to be seen in 5 Lyman series transitions. The measured value of the D/H ratio towards QSO \object is found to be D/H=2.54±0.23×10−5 = 2.54 \pm 0.23 \times 10^{-5}. The metallicity of the system showing D/H is found to be ≃0.01\simeq 0.01 solar, indicating that the measured D/H is the primordial D/H within the measurement errors. The gas which shows D/H is neutral, unlike previous D/H systems which were more highly ionized. Thus, the determination of the D/H ratio becomes more secure since we are measuring it in different astrophysical environments, but the error is larger because we now see more dispersion between measurements. Combined with prior measurements of D/H, the best D/H ratio is now D/H=3.0±0.4×10−5 = 3.0 \pm 0.4 \times 10^{-5}, which is 10% lower than the previous value. The new values for the baryon to photon ratio, and baryonic matter density derived from D/H are η=5.6±0.5×10−10\eta = 5.6 \pm 0.5 \times 10^{-10} and \ob =0.0205±0.0018=0.0205 \pm 0.0018 respectively.Comment: Minor text and reference changes. To appear in the May 10, 2001 issue of the Astrophysical Journa
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