Using The Water Drop Utility To Help With Drainage Design
Introduction
When determining time of concentration for a drainage basin,
it is helpful to be able to track a drop of water from the
upstream end of a drainage basin to its most downstream
point. Not only is the distance traveled useful, knowing the
slope over that distance is necessary as well to accurately
measure the time it takes for the entire basin to contribute
to flow at the downstream point, or outlet. The time of
concentration is then used in a variety of calculations
which help the designer determine peak flow for a particular
basin. The Water Drop Utility in Civil 3D is the perfect
tool for this task.
Applying the Water Drop
Once basin lines have been determined for a surface and the
discharge point has been identified, water drops can be
applied to the surface to show the path water takes from its
highest elevations to its lowest elevations. From the
Surfaces pull-down menu and the Utilities option, begin the
Water Drop command.

A dialog box will now pop up with a few settings to be
applied. The user can decide whether or not to use a marker
at the beginning of the path, what layer to put the path
objects on, and whether the path object is a 2D or 3D
Polyline.

So that the elevation and slope information can be used, 3D
Polyline is the better option here. Then, the user can
select a location at the upstream end of the basin and see
the resulting path drawn across the basin.

It is important to keep in mind the object of the task: to
determine the slowest path water takes across the basin. It
may not necessarily be the longest path as the effects of
slope must be taken into account. For large or oddly shaped
basins, this may require several drops of water and several
runs through the time of concentration calculations to
identify the slowest path water takes across the basin.
Analysis
Now, to obtain full use of the path object, it is helpful
here to turn this 3D Polyline into a Civil 3D Feature Line
as these are far more versatile. This is done from the
Grading pulldown menu and the “Create Feature Lines from
Objects” command. Taking the default values on the
subsequent Feature Line Creation dialog box is fine here
because the path objects will not need to be shown on a set
of plans.
To see the elevation effects on the water path, the user may
now select the Feature Line, right-click and proceed to the
Elevation Editor.

Examining our results, it is easy to see that there is a lot
of unnecessary data here, mainly because of the
triangulation in the surface itself and the relatively short
segments on the Feature Line. The user needs a way to
simplify the object for use in a time of concentration
calculation and we will do this using a Quick Profile and a
“Profile by Layout.”
Again, select the Feature Line, right-click and go to Quick
Profile. Take the defaults on the Create Quick Profile
dialog box. The resulting profile is simple and temporary
but it is all that is needed right now.

Next, use the Profiles pulldown menu and the “Create Profile
by Layout” option to bring up the profile creation toolbar.
On the first button of the toolbar, use the Draw Tangent
option and trace over the profile in 5 representative
sections making sure the first segment is no longer than 100
feet.


We now have simplified distance and slope information for
use in a time of concentration calculation. As an example,
here is an image taken from the time of concentration
calculator from WinTR-55, a USDA program used for hydrology
in small watersheds:

This calculator gives the user the opportunity to enter five
segments along the water’s path, each with its own slope,
distance and stream characteristics. Even with some work to
be done to determine flow area and wetted perimeter for the
“Channel” segments, it is easy to see that the ease of the
water drop utility and the power of the Feature Line made
the whole process easier and made the user more efficient.
Conclusion
Whether you use a program like WinTR-55 or the Hydraflow
solutions now included with a subscription to AutoCAD Civil
3D 2008, here are a couple of notes and things to keep in
mind:
-
The reason the first segment should be limited is that
“Sheet” flow cannot be more than 100 feet.
-
Manning’s “n” value for surface flow can be found in any
good Open Channel Flow Handbook or Engineering Reference
Manual.
-
This is just an approximation and the user will see that
minor variations in these values will likely result in
even smaller fluctuations in the ultimate time of
concentration for the basin.
-
Become familiar with the tools you use for these
calculations and know their limitations.
-
Always remember to use sound engineering judgment in any
design endeavor you undertake. The software itself seems
to grow by leaps and bounds with each release but, in
the end, it is still just a tool in the overall realm of
good practice and design.