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Histograms work for numeric values as well as categorical ones. For instance, the NUMUNITS column contains the number of different units of a product included in an order and it takes on just a handful of values. How do we know this The following query answers the question: How many different values does NUMUNITS take on

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The travel time of a body wave from earthquake to seismograph is then equal to the sum of the travel times through the individual elements of the model Any lateral velocity variations within the model are then re ected in variations in arrival times with respect to the mean arrival time of undisturbed events Similarly, the dispersion of surface waves across a heterogeneous model differs from the mean dispersion through a radially symmetrical model The method makes use of a simplifying assumption based on Fermat s Principle, which assumes that the ray paths for a radially symmetrical and laterally variable velocity model are identical if the heterogeneities are small and that the differences in travel times are caused solely by heterogeneity in the velocity structure of the travel path This obviates the necessity of computing the new travel path implied by refractions at the velocity perturbations.

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The new workspace remembers what panels you added, rearranged, and removed, so the next time you choose that workspace, all those panels and only those panels appear on-screen. That new workspace is available by choosing Window Workspace workspace name.

gene shuf ing or incremental truncation. Virtually all basic molecular breeding approaches start with a protein that has a desired trait (at least to a small extent) then the aim of the experiment in vitro is to improve or evolve that trait. Such a molecular breeding experiment may be called directed evolution of protein function. Mutant genes are generated and then protein variants are expressed and selected for by a speci c assay designed to provide the arti cial selection pressure. The most improved mutant protein variant is then identi ed and then the whole process is repeated again starting from the gene for the improved mutant protein variant (Figure 10.7).

There are two main approaches to seismic tomography depending upon how the velocity heterogeneity of the model is represented Local methods make use of body waves and subdivide the model space into a series of discrete elements so that it has the form of a threedimensional ensemble of blocks A set of linear equations is then derived which link the anomalies in arrival times to velocity variations over the different travel paths A solution of the equations can then be obtained, commonly using matrix inversion techniques, to obtain the velocity anomaly in each block Global methods express the velocity variations of the model in terms of some linear combination of continuous basic functions, such as spherical harmonic functions Local methods can make use of either teleseismic or local events In the teleseismic method (Fig 211) a large set of distant seismic events is recorded at a.

Burlage, RS, R Atlas, D Stahl, G Geesey, and G Sayler 1998 Techniques in Microbial Ecology Oxford University Press, New York Button, DK, F Schut, P Quang, R Martin, and B Robertson 1993 Viability and isolation of marine bacteria by dilution culture: theory, procedure, and initial results Appl Environ Microbiol 59: 881 891 Capone, DA, JP Zehr, HW Paerl, B Bergman, and EJ Carpenter 1997 Trichodesmium, a globally signi cant marine cyanobacterium Science 276: 1221 1229 Castellan, GW 1983 Physical Chemistry, 3rd edn Addison-Wesley, Reading, MA Chapelle FH, DA Vroblesky, JC Woodward, and DR Lovley 1997 Practical considerations for measuring hydrogen concentrations in groundwater Environ Sci Technol 31:2873 2877 Chang, Y-J, PE Long, R Geyer, et al 2005.

Microbial incorporation of 13C-labeled acetate at the eld scale: detection of microbes responsible for reduction of U(VI) Environ Sci Technol 39: 9039 9048 Chiang, CY, KR Loos, and RA Klopp 1992 Field determination of geological chemical properties of an aquifer by cone penetrometry and headspace analysis Ground Water 30:428 436 Christian, GD 2003 Analytical Chemistry, 6th edn Wiley and Sons, New York Church, M, EF DeLong, HW Ducklow, MB Karner, CM Preston, and DM Karl 2003 Abundance and distribution of planktonic Archaea and Bacteria in the waters west of the Antarctic Peninsula Limnol Oceanograph 48:1893 1902 Clark, FE 1973 Problems and perspectives in microbial ecology In: T Rosswall (ed) Modern Methods in the Study of Microbial Ecology: Proceedings of a symposium, Vol 17, pp 13 16 Bull Ecol Res Committee.

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