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City of Ann Arbor SSWWEP - Citizens Advisory Committee Coordination — City of Ann Arbor

1.36 -C- How are you accounting for soil moisture and rain spikes in calculating volume & rate of flow from footing drains?

Posted by Lori Byron on 20 Dec, 2013
Category: Category 1 - SSWWEP Questions and Presentations

Frank Burdick’s Log Number: N/A
Submitted by: Resident, via email
Category (1,2,3): 1
Status: Closed
Estimated date to address: N/A

Q. The only dispute I have ever had with the volume and rate of footing water is in using either a dry weather number or a wet weather number and extrapolating them beyond the storm event.  If you look at the "spike" chart, the peak might be shown as producing high volume for, say, three minutes. During the event the volume rises from a "normal" flow to that peak then drops back toward that normal level. Yet in almost every instance, the elevated level is multiplied for a duration of an hour or longer. It is the peak/storm duration volumes we have to deal with, and that is what points to short term retention. This can be clarified. It does not make sense to me, to burden over 18,000 households (plus an unknown post disconnect number) with a sump pump penalty instead of retention, if a projection of new water/sanitary/surface customers is considered. We have serious surface water problems. With all the technology available to us, we need to develop a means of determining which business or resident has a high volume footing drain problem, and resolve them and not impose sump pumps in low volume instances. If you recall the initial SSWWE meeting, there were accusations that the CAC's were biased and not necessarily representative of the public. Possibly their responsibility and duties need to be more clearly explained. For this reason I will remain independent. Thank you though for your inclusive mail, especially for your Retention work. 

A. Each sanitary collection system that we have studied is unique and has unique characteristics that drive the cost-effective engineering solution. The engineering options depend on the magnitude of the wet weather flows, the location that wet weather flows are generated, the location of hydraulic bottlenecks in the system, and many other factors.  Examining these characteristics is the next step in the process - hydraulic capacity and alternatives evaluation.  The first step was to quantify the impacts of FDD on the sanitary sewer flow.  We had to understand that impact first, before we can evaluate further alternatives.

Storage is a very common method of addressing peak wet weather flow, and we will be including many examples in our presentation to the Best Practices sub-group of the CAC next week. A few things to keep in mind about storage:
·       As you pointed out, storage can be very effective for systems with “spiky” peak flows and the timing of the peak flows has a tremendous impact on the storage size.  That is why it is very important to understand the flow characteristics of the system (the step we are in now, and will be reporting on Dec 12). 

·       The viability of storage depends on the location of the bottlenecks, relative to the location of the wet weather flow generation.  For example, if high wet weather flows and bottlenecks are upstream in the system, building storage downstream won’t help.  The storage has to be located upstream of the bottlenecks to work.  That is why it is critical that we understand the hydraulic capacity of the system - that’s the next step. 

·       For a traditional storage tank, a large amount of land has to be available near the location the storage is needed (very common for 2-5 acres or more needed). That can be a significant challenge in a built-out area. We understand that it was a concern with the SSO task force in 2001 - we have heard stories of concerns by the task force about putting tanks in parks and wooded areas and negatively impacting these natural resources.  

·       There are other alternatives to traditional storage tanks to store flow - linear storage and storage shafts. Linear storage can be accomplished by constructing an oversized pipe - perhaps on the order of 6-12 feet in diameter for a length of several thousand feet to store the flow.  Often, these are constructed by tunneling, which can reduce the surface impacts. One disadvantage of tunneling is that it can be more expensive than a traditional storage tank.  We will be including several examples of tunnels in our material for the Best Practices group. Some communities have also built deep shafts for storage.  Tunnels and shafts have the added risk of complex, deep underground construction. There are many examples of failed tunnels and storage shafts.

·       Depending on the depth of pipes, and conflicts with other utilities, it may be possible to build linear storage with “open-cut” construction techniques. This has a short-term disturbance to the surface during construction, but can be less costly and have less risks than tunneling.  The viability of this option depends on the location, the depth of the sewer, the presence of conflicting utilities, the extent of surface restoration impacts and other items.

As you can see, evaluating alternatives is complex and entails many competing decisions and values. The City and the OHM team can present engineering costs and impacts, but the optimal engineering solution is not necessarily the best solution for the community.  Hence the need for a Citizens Advisory Committee to weigh these options and recommend what is best for the community to balance the ever competing challenges. These are the types of discussions we plan on having as part of the next step with the CAC.
 

A few technical items to address a few of your other comments:
·       It is fairly straightforward to show that stormwater flows are much, much larger than FDD flows, and that FDD flows are much larger than normal sanitary flow. The conclusion is the same whether the computation is done based on stormwater volume or peak flows. This is not unique to Ann Arbor - it is a very common observation from systems around the Country. I’d be happy to review the basis of this conclusion with you. 

·       In making computations of stormwater volume, the duration should be matched with the duration of the rainfall being applied. Often, for stormwater computations, a peak-hour rainfall is used (something like 1.8-inchs in an hour), and so the volumetric computations are made on an hourly basis.  This is often done to simplify the computations to illustrate basic concepts.  You are correct that the impact depends on the pattern of the rise from the base condition to the peak condition and back to the base again.  This is called a hydrograph. We examine the impact of the full hydrograph on the sewer system, and will often summarize the results in terms of the “peak flow” or hydrograph "volume” to provide some simple metrics for comparison. Underlying these metrics are the detailed hydrographs.  I’d be happy to review the underlying hydrographs with you, or the CAC. We will have hydrographs available for viewing at the Dec 12 CAC meeting if there is interest, and time depending. 

·       The City did indeed target the “wettest" area of the system with the five priority districts for FDD. The metering is showing that these five priority areas had peak flows that were 20-30 times average during wet weather events in 2000 before the FDD, when more common rates are 3-8 times average.  As we presented in the October CAC, the post-FDD flows in these districts from 2013 appear to have been reduced to the more common range of peak flows during large rain events.  On December 12, we will be reviewing the results of the full-evaluation of these flows, including the application of three scientific methods to quantify the impact of the FDD on sanitary flows.

·       We are not aware of a technology that can determine which specific houses or businesses will have high FDD flow.  It is very challenging to meter the flows from an individual footing drain before it is disconnected.  While there are some indicators, the flow variations from house to house are very sporadic.  There are instances of a very high flow FDD right next to a house that is very low. The best technique that we are aware of is to perform flow metering at the neighborhood level, and target those areas with the highest flow. Areas with a high propensity for basement backups are also an obvious target area. Pilot FDD with sump monitoring is then an effective method of verifying the appropriate areas. We understand that these techniques were the basis of the five priority areas identified in 2001.

Please note that I have intentionally kept this message at a summary level. I’d be happy to get into more details, but it is not effective to do so via email. If you would like to get into more details, I would be happy to meet with you. I did this a few weeks ago with Frank Burdick with a pad of paper, pencil and calculator, and I think it was very helpful.    

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