Collection

2007 Spring ASEE Middle Atlantic Section Conference

Authors

V. Briller; E. Deess; R. Calluori; K. Joshi

female students. See table below from he Fall2006 Entering Students survey. Q-37: Who Most Influenced Your Decision to Apply? by Gender Male (n = 131) Female (n = 40) Parent 43% 38% Guidance counselor 18% 18% Friend 11% 18% High school teacher 9% 8% Alumnus of NJIT 7% 3% Current NJIT student 6% 5% Relative

Collection

2007 Spring ASEE Middle Atlantic Section Conference

Authors

Tom M. Warms; Renee Drobish

node and its contents areinitialized to the indicated values; the trace uses the symbol ADDR0 to represent the new node's address.Thus the value of ADDR0->word is "memory," and the left and right pointers at that location are bothNULL. In addition, ADDR0 is assigned to pnew. When insert is called, root is the actual parametercorresponding to reference parameter q. The statement labeled (1) causes both to be set to ADDR0, sothat root now points to this new node. The "before" and "after" representations of the tree are,respectively, above and below the trace.A second trace shows how the insertion routine can insert an element into its alphabetical position in anon-empty tree. In the following, the root word is "computer"; its right child is

Collection

2007 Spring ASEE Middle Atlantic Section Conference

Authors

Phil Dacunto P.E.; Mike Hendricks

calculate impacts. Due to its flexibility inprogramming applications, and its ability to handle large matrices of data, we chose Matlab to perform thecalculations of downwind plume concentrations. We chose ESRI’s ArcMap 9.1 for visualization andanalysis. We created the custom application so that students would be able to use it without previousexperience with either program.Calculating Downwind Concentrations - MatlabThe algorithm employed in the Matlab application calculated downwind, ground level concentrationsusing the Gaussian plume equation (Cooper and Alley, pg 612)1: ⎛ y2 ⎞ ⎧ ⎛ ( z − H )2 ⎞ ⎛ ( z + H )2 ⎞⎫ C= Q exp