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point flow calculations.). A table consists of multiple records. The records, in turn, contain <br />multiple fields. Records can be compared to horizontal 'rows' in a spreadsheet environment, <br />whereas fields are similar to vertical 'columns' in a spreadsheet environment. The width of <br />each field, as well as the type of data to be stored in the field (numeric, character, date), is <br />defined upon creating a table. A computer file which corresponds to a table (database) can be <br />recognized by a .dbf extension on the file name. <br />Figure 1 provides a better understanding of some of the terms listed above. <br />u <br />River <br />knowing Stream Diverting canal <br />or Drainage Ditch or Ditch <br />River Flow Diroct y <br />Below/Above St1IIdUR8 <br />b <br />Channel I V * * * * * * <br />V V t • * * * * <br />V I V * * * * V I <br />Node Gain/Loss <br />Node Gdn/LAea <br />Node Gain/Loss Node <br />A <br />B <br />C D <br />River <br />River <br />River <br />- - - - - - Subreach ------- <br />Subreach _______ <br />:- - - - - -- Subreach ------- i <br />r <br />A -B <br />i <br />B-C <br />C-D <br />i <br />i <br />------------------ <br />- - - - -- River Reach ----------------- - - - - -- <br />Figure 1 - Schematic of Point Flow Software 'river' terminology. <br />Depicted in Figure 1 is a river reach defined by Gauges I and II (points of known river flow). <br />Through the course of the river reach an inflow to and a diversion from the river occurs (at <br />Nodes B and C, respectively). This partitions the river reach into three subreaches (A -B, B -C, <br />and C -D). Bi- directional arrows indicate the gains/losses which are calculated for each subreach. <br />The horizontal line representing the river reach in Figure 1 is encircled at locations in which river <br />flows are calculated (above and below each structure). <br />In the following text the adjective 'river' is often neglected when using words such as channel, <br />flow, reach, and subreach. Unless explicitly noted otherwise, such words are in reference to the <br />main stem river. <br />The point flow computations are based on elementary volume balance theory and are performed <br />in a two step fashion. The first step entails creating a conservation equation (volume) within a <br />defined reach so that total reach gain can be calculated, and subsequently allocated, over the <br />length of the reach. The second step of the point flow calculations utilizes the calculated subreach <br />gains to compute the flows above and below each structure. This two step process and the <br />associated assumptions are outlined in detail below. <br />5 ptflguid.wpd <br />