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This technique is best suited for low permeability materials (hydraulic conductivity < 01 m/day) fault spring A spring (qv) which arises where a fault brings an aquifer (qv) into contact with an aquitard (qv) at the ground surface feedback A situation in which one attribute of a system (X) affects another (Y), whilst Y in turn affects X ferric iron Ions of iron carrying a net electrical charge of 3+ Usual symbol: Fe3+ ferrous iron Ions of iron carrying a net electrical charge of 2+ Usual symbol: Fe2+ Fick s Law A mathematical formula which describes molecular diffusion (qv) Fickian Any model which follows the mathematical form of Fick s Law (qv), whether or not it is used to model molecular diffusion (qv) eld capacity When an unsaturated soil contains its full speci c retention (qv.

) of water, so that suf cient moisture is available to meet all demands from plants lter pack Sand and/or gravel packed around a screen (qv) to strain ne sediment present in the aquifer (qv) from groundwater (qv) entering a well nite difference methods The most widely used mathematical technique used for obtaining numerical solutions (qv) to the partial differential equations (qv) which describe groundwater (qv) processes nite element methods The second-most popular mathematical technique (after nite difference methods (qv)) used to obtain numerical solutions (qv) to the partial differential equations (qv) which describe groundwater (qv) processes nite volume methods A less common mathematical technique used to obtain numerical solutions (qv).

rock type (i.e. lithology ), then we talk of lithostratigraphy. Where the subdivision is achieved by means of recognizing distinctive fossils then we talk of biostratigraphy. Where the stratigraphic sequence is constrained by reliable estimates of absolute age of the constituent rocks, we talk about chronostratigraphy. Logically, therefore, we can claim to be pursuing hydrostratigraphy when we subdivide sequences on the basis of the ability of the rocks to store and transmit water. Although this practice has a very long pedigree, having been practised by the Father of Stratigraphy himself, William Smith (1769 1839),v the term hydros(a) Chronostratigraphic units System Neogene Age (Ma) Series Miocene and Pliocene

Consider the impossibility of accurately keeping track of bene ts rst Think of the sheer number and variety of bene ts that are likely to be given and received in an intimate relationship for example, between a husband and wife living together in the same home Each day a very large number of household tasks (eg, making beds, doing laundry, picking up clutter, preparing food, shopping for food, putting groceries away, vacuuming, dusting, taking the mail in, feeding pets, changing light bulbs and toilet paper, etc) are done So too are a variety of nonhousehold services (eg, dropping a spouse off at work, picking up take-out food, dropping off dry cleaning, having something framed, visiting relatives, etc) Then there are bene ts that fall within the categories of verbal affection, physical affection, information, instructions, and goods that are given and received.

ow duration curve A cumulative frequency curve showing stream ow rates versus the percentage of time the indicated ow rates were equalled or exceeded at a given measurement point ow lines Lines representing the likely pathways of groundwater (qv) owing through an aquifer (Usually constructed on contour maps of groundwater head (qv)) ow net An assemblage of head (qv) contours and ow lines (qv) delineating groundwater (qv) ow patterns in a particular system ow tube The area enclosed between two adjacent ow lines (qv)..

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session While both network layer and application layer metrics are considered during tree building, whether the overlay network is mesh or nonmesh also signi cantly affects the tree building process After being built, the distribution tree receives ongoing maintenance in order to adapt to changes in network conditions and overlay node availability Tree organization is the most complex and yet critical to the overall success of the system So we will dedicate the next section to tree organization algorithms 3 Content Distribution Once the distribution tree is built, multicast content is transmitted reliably over the distribution tree For real-time streaming, the transmission is relayed by all the overlay nodes instantly and, optionally, stored at certain overlay nodes For latency-insensitive application such as software distribution and content replication, the time and speed of transmission are controlled by session management, which in turn are driven by resource provision policies.

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