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Estimation of fracture zone geometry from steady-state hydraulic head data using iterative sequential cokriging Geophys Res Lett, 23(19):2685 2688, 1996 19 DW Vasco, H Keers, and K Karasaki Estimation of reservoir properties using transient pressure data: an asymptotic approach Water Resour Res, 36(12):3447 3466, 2000 20 VV Vesselinov, WI Illman, Y Hyun, SP Neuman, V Di Federico, and DM Tartakovsky Pronounced permeability and porosity scale-effect in unsaturated fractured tuffs In Proceedings of the Conference Fractured Rock 2001 , Toronto, Canada, March 26 28, 2001 21 C-M Wu, T-CJ Yeh, J Zhu, TH Lee, N-S Hsu, C-H Chen, and AF Sancho Traditional analysis of aquifer tests: comparing apples to oranges Water Resour Res, 41:W09402, 2005 22 T-CJ Yeh Stochastic modeling of groundwater ow and solute transport in aquifers J Hydrol Processes, 6:369 395, 1992.

VBA enables you to easily retrieve, create, and manipulate objects. To get a list of objects, open the Object Browser by clicking Object Browser on the toolbar or choosing View Object Browser. Objects are organized into libraries. All of the objects that you work with in AutoCAD are in the AutoCAD library. To see the list of AutoCAD objects, click the <All Libraries> drop-down list and choose AutoCAD. You can see the result in Figure 37-2.

TYPE v_emp_type IS VARRAY (1000) OF emp%rowtype; emp_varray v_emp_type;

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where R, denotes the estimate at the kth instant of time and x(k) denotes the array signal sample, also known as the array snapshot, at the kth instant of time (t is replaced by kT and the sampling time T is omitted for the ease of notation). The estimate of R, may be updated when the new samples arrive using

The instantaneous current is a function of the static DC voltages and average temperature, and of the instantaneous fast voltages [31, 32]. Several possibilities are available for pulsed I /V curve measurements. A possible scheme is shown in Figure 2.20.

23 T-CJ Yeh Scale issues of heterogeneity in vadose-zone hydrology and practical solutions In G Sposito, editor, Dependence and Scale Invariance in Hydrology Cambridge University Press, 1998 24 T-CJ Yeh, K Hsu, C Lee, J Wen, and C Ting On the possibility of using river stage tomography to characterize the aquifer properties of the Choshuishi Alluvial Fan, Taiwan Presentation at AGU 2004 Fall Meeting 25 T-CJ Yeh and S Liu Hydraulic tomography: development of a new aquifer test method Water Resour Res, 36(8):2095 2105, 2000 26 T-CJ Yeh, S Liu, RJ Glass, K Baker, JR Brainard, DL Alumbaugh, and D LaBrecque A geostatistically based inverse model for electrical resistivity surveys and its applications to vadose zone hydrology Water Resour Res, 38(12):1278, 2002 u 27 T-CJ Yeh and J Sim nek.

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[lo] H. Bolckei, D. Gesbert, and A.J. Paulraj. On the capacity of OFDM-based spatial multiplexing systems, IEEE Trans. Commun., 50(2):225-234, Feb.

History palette tracks the additions you make to your page and what you do to set the object up, writing a history of them in the History palette (Specifically, each history is a page history; that is, changes to any page are tracked, not application-wide actions such as Preference settings) You can move back in this history, to any state of the page, up to 20 steps backwards Each time you save your page or close it, the history begins anew It also clears and begins anew when you switch layout views, such as moving from Layout to Source, or to Outline or Preview (but not when you switch between Layout view and the Source Code window) Site Reports give you the details of your site s health.

Figure 9.1. Two-electron, two-orbital interaction of an alkyl halide s orbital (LUMO) and the nonbonded orbital, n, of a nucleophile: (a) most favorable approach; (b) unfavorable front-side approach on nodal surface.