4,745 research outputs found

    An Investigation of Salinity Fluctuations In Soils of a Northern Utah Marshland

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    Ogden Bay Waterfowl Management Area is one of many marshlands bordering the Great Salt Lake that are extremely important as breeding habitats for North American waterfowl. Salinity, both of surface and interstitial waters, is an important factor in maintaining a suitable habitat within the marsh. For this reason, a study was undertaken to determine the factors affecting the salinity of surface and interstitial waters. A small (approx. 100 acre) subunit was studied extensively to determine; 1) variations in surface water salinity with flowrate and water level; and 2) variation in interstitial water salinity with depth and location within the subunit. Field data indicated a substantial increase in salinity (as measured by electrical conductance) with depth in the interstitial waters. Wide variation in interstitial water conductivities was also observed within the study unit. Of major significance were large increases in interstitial water salinities in areas where the soil had dried, due to a low water level, and again re-wetted. This was in contrast to relatively constant soil water salinily observed in areas that were perenially flooded In addition to the field study, a laboratory study, using three 20 cm diameter undisturbed soil cores, was performed to determine the factors affecting the movement of salts through the marsh soils. The surface and bottom of the cores were fed with fresh water and brine, respectively, for a period of three months, while interstitial water samples were taken to monitor changes in soil water conductivities with depth of soil. A computer model was developed to simulate the experiment, as well as to help interpret the experimental results. The comparison between the observed data and data predicted by the model, as well as the results of the field data,\u27 indicated that the major mechanisms affecting fluctuations in soil water salinity in the Ogden Bay marsh system is the movement of water through the soil

    Constraints on the χ_(c1) versus χ_(c2) polarizations in proton-proton collisions at √s = 8 TeV

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    The polarizations of promptly produced χ_(c1) and χ_(c2) mesons are studied using data collected by the CMS experiment at the LHC, in proton-proton collisions at √s=8  TeV. The χ_c states are reconstructed via their radiative decays χ_c → J/ψγ, with the photons being measured through conversions to e⁺e⁻, which allows the two states to be well resolved. The polarizations are measured in the helicity frame, through the analysis of the χ_(c2) to χ_(c1) yield ratio as a function of the polar or azimuthal angle of the positive muon emitted in the J/ψ → μ⁺μ⁻ decay, in three bins of J/ψ transverse momentum. While no differences are seen between the two states in terms of azimuthal decay angle distributions, they are observed to have significantly different polar anisotropies. The measurement favors a scenario where at least one of the two states is strongly polarized along the helicity quantization axis, in agreement with nonrelativistic quantum chromodynamics predictions. This is the first measurement of significantly polarized quarkonia produced at high transverse momentum

    Compressed representation of a partially defined integer function over multiple arguments

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    In OLAP (OnLine Analitical Processing) data are analysed in an n-dimensional cube. The cube may be represented as a partially defined function over n arguments. Considering that often the function is not defined everywhere, we ask: is there a known way of representing the function or the points in which it is defined, in a more compact manner than the trivial one
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