Water supply & consumptive use
How much water the project consumes, against the receiving water's own cited low flows.
A real impact study states how much water Project BOSC consumes at buildout. It sets that figure against the Ottawa River's own cited design low flows, which are the drought floors a permit writer screens every discharge against. This chapter reports as much of that comparison as the record supports. It names what it cannot compute.
Cooling methodevaporative cooling tower (“open loop”) [inference]
baseline
Current municipal loop, no data-center cooling draw.
buildout
Data-center campus cooling draw (evaporative_tower) on the municipal supply.
- The draw is set against the receiving water's cited design low flow as a worst-case, basin-scale bound — a screening comparison, not a withdrawal claim.
The screen above sets the modeled draw against the Ottawa River’s cited 7Q10. That is the drought floor a permit writer screens every discharge against. But Lima’s water does not come out of the river in real time. Read the comparison as a bound, not as a withdrawal claim.
The city holds its raw water in 5 upground reservoirs, off the river channel. Together they store about 14.4 billion gallons. Of that, 10.1 billion is filled from the Auglaize River to the west and 4.3 billion from the Ottawa to the east. Four pump stations fill them, and run only when the rivers are high. Lima therefore never withdraws at the 7Q10. It lives off stored water.
That changes the question this chapter must answer. The binding constraint is not what the river holds on its worst day. It is how far the campus draws the reservoirs down across a dry season, and whether the rivers can refill them afterward.
The number that survives the reframe
The campus buys treated municipal water like any other large customer. Its modeled makeupinput of 3.92 million gallons per day (MGD) is 20.7 % of the 18.92 MGD the plant would then produce. The plant makes about 15 MGD today and is rated for 30 MGD. One customer would take a fifth of the city’s water production.
The consumptive part is harder still. About 3.14 MGD leaves as water vapor from the cooling towers and never returns to the basin. What does return goes downstream to the Ottawa through the treatment plantsrec . None of it goes back into the reservoirs, so the full makeup draws storage down.
Run that against the stored volume and the zero-refill drought reserve falls from 960.9 days to 761.8 days. The campus costs the city 199.1 days of drought reserve.
The refill side is the open question, and it is seasonal. The rivers yield least in the months when the draw is highest, and the seasonal-withdrawal annex maps that month by month. The metered answer sits in two records the study still asks for. One is the campus’s water-service contract. The other is its allocated share into the City of Lima treatment plant. Both are tracked on the leads board.
Learn to read the record behind this chapter → Project BOSC, Chapter 4: What it does to the water
The record behind this chapter
What this chapter stands on: the records it reads, the inputs its modeled figures rest
on, and the reference data behind its baselines — the same pages the record screens
serve, not a second copy. A figure the record does not support stays [open] and links nothing.
- Permits22 records