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We learned in 3 that rates of groundwater ow can be calculated using Darcy s Law (see equation 31) Thus if we know the value of K and the hydraulic gradient in a given portion of an aquifer, we can easily use Darcy s Law to evaluate the in ow and out ow rates in the above equation over any time interval of interestiii Furthermore, if the S value for the aquifer is also known, we can relate the change in volume of storage to changes in water levels within the aquifer (see Section 144).

Conversely, if we have an independent estimate of the volumes of water entering and leaving a given portion of aquifer, then because Darcy s Law and the calculations involving S both involve values of groundwater head, it is possible to calculate head patterns in the aquifer at any point in time as long as K and S are known By the time we have substituted Darcy s Law and S values into the simple mass conservation equation given above, it will have become a complex formula of a type known as partial differential equations While techniques for solving such equations had been developed long before the publication of the work of Hubbert (1940), the laborious nature of the calculations (for all but the most simpli ed versions of the equations; see Section 1042) largely precluded their use outside of research institutions prior to the advent of digital computers.

Neither of these elements would be difficult to implement. The FIELDSET element should surround related fields so they are grouped. The LEGEND element immediately follows the FIELDSET element with a descriptive title for the FIELDSET.

, and Sambanis, A (2001) Effect of oxygen tension and alginate encapsulation on restoration of the differentiated phenotype of passaged chondrocytes Tissue Eng 7: 791 803 Nakahara, H, Bruder, SP, Haynesworth, SE, Holecek, JJ, Baber, MA, Goldberg, VM, Caplan, AI (1990) Bone and cartilage formation in diffusion chambers by subcultured cells derived from the periosteum Bone 11: 181 188 Nakahara, H, Goldberg, VM, Caplan, AI (1991) Culture-expanded human periosteal-derived cells exhibit osteochondral potential in vivo J Orthop Res 9: 465 476 Nishida, S, Endo, N, Yamagiwa, H, Tanizawa, T, Takahashi, HE (1999) Number of osteoprogenitor cells in human bone marrow markedly decreases after skeletal maturation J Bone Miner Metab 17: 171 177 Nishimura, K, Solchaga, LA, Caplan, AI, Yoo, JU, Goldberg, V.

Thereafter, the implementation of powerful numerical methods (Section 1043) rst became feasible (Prickett and Lonnquist 1971) and eventually commonplace (eg Anderson and Woessner 1992) One key attribute of the equations of groundwater ow expounded by Hubbert (1940) is that they encapsulate the application of the fundamental laws of physics to the analysis of groundwater ow For this reason, we refer to models based on the solution of these equations as being physically based In scienti c terms, physically based models represent the gold standard:.

6

Illustrated TCP/IP by Matthew G. Naugle Wiley Computer Publishing, John Wiley & Sons, Inc. ISBN: 0471196568 Pub Date: 11/01/98

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M, Johnstone, B (1999) Chondroprogenitor cells of synovial tissue Arthritis Rheum 42: 2631 2637..

These remarks indicate that I-O psychology may come full circle (from primarily technology to science and research, then back to technology), and the scientist-practitioner distinction will continue to prevail. Thus, it is imperative that for I-O psychologists to continue to make a difference, they need to know their history to understand what was done, what was not done, and why. After reviewing the rst 50 years of the journal Personnel Psychology, editor John R. Hollenbeck (1998) stated, the impact that one has on the future seems to be closely related to one s appreciation of the past. This makes it all the more tting, therefore, to re ect on and study our past. . . . (Editorial).