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fixed-length output that is irreversible. Given the ciphertext, there is no way to produce the original plaintext message. Hash is useful for storing passwords and for digital signatures because there is no key. At this point you may be asking, what good is ciphertext that you can t decrypt Here s how it works. You run a customer password through the hash algorithm. The next time the user goes to log on, the system prompts for a password. The user enters it, and then the password is run through the hash algorithm and compared to the encrypted text. If they match, the user is granted access. If they don t match, the user is denied access. Another use for hash is with digital signatures. A digital signature is added to a document with the sender s private key, so the recipient can use it for nonrepudiation. Signing the entire message with the sender s private key will work, but is very inefficient because asymmetric encryption is very slow. Instead, because hash takes a message and produces a smaller, fixed-length output, it would make sense to run the message through a hash first, then encrypt the smaller output with the sender s private key. The less information that has to be encrypted, the quicker the process will go.

Figure 9-2

Note: These results are given in Magnus (1988) (see also Section 9.5).

boundary is speci ed head conditions (10.2c), because these make it very dif cult to realistically incorporate the moderating effect of ne-grained streambed sediments, they effectively divide the aquifer into two isolated areas (either side of the river), and they can easily give rise to spurious quantities of groundwater in ow/out ow if used carelessly. The coastline along which an aquifer meets the ocean (see Figures 3.5, 7.2). If any boundary merits the speci ed head condition, this is it (Box 10.2). Head-dependent ux conditions are frequently also applicable. Particular care needs to be taken in modeling this type of boundary where salt water intrusion is being considered, in which case density contrasts between fresh and marine groundwaters need to be taken into account (see Sections 3.3.1, 7.2.4 and 9.3.5).

The Inn has the possibility of booking another group of 100 rooms for the nights of Tuesday, Wednesday, Thursday, and Friday of that week at a discounted rate of $60 per room. The Inn s rack rate for transient guests is $80, and its marginal cost per room sold is $15.

Foster, SSD, 1998, Groundwater recharge and pollution vulnerability of British aquifers: a critical overview In: Robins, NS (ed) Groundwater pollution, aquifer recharge and vulnerability Geological Society, London, Special Publications, 130: 7 22 Foster, SSD, Morris, BL, and Lawrence, AR, 1994, Effects of urbanization on groundwater recharge In: Proceedings of the ICE International Conference on Groundwater Problems in Urban Areas Institution of Civil Engineers, London, pp 43 63 Freeze, RA, 1969, The mechanism of natural groundwater recharge and discharge, 1 One dimensional, vertical, unsteady, unsaturated ow above a recharging or discharging groundwater ow system Water Resources Research, 5: 153 171 Freeze, RA, 1972a, Role of subsurface ow in generating surface runoff; 1 base ow contributions to channel ow Water Resources Research, 8: 609 623 Freeze, RA.

they are of the same format: the coarsely ground products are not sausages, since the meat has been cured in a tumbler and stuffed before being cooked in the casing. Between these two extremes are combination products. One type is batter where the meat has been chopped into a grain the size of a couple of millimeters. Another type is produced when the basic batter has been nely chopped, but then larger meat particles (or other foodstuffs) have been added into the basic batter. The linear speed of bowl cutter knives is about 140 m/s. The sharp blades (the at cutting edge is about 20 30 m, i.e., the cutting breadth is about ten times the sarcomere length) cut connective tissue and muscle bers into pieces, but fractioned myo brils can be seen through a microscope. The