The property runs entirely on private groundwater — three wells and ~40,000+ gallons of tank storage, no city water. This pulls together what's actually been measured — a certified well test, a basin hydrogeologic study, and (new, Jul 6) Jerry & Don's full service file: well tests back to 2000, the primary well's drilling report, and schematics of the whole water system — what it all means for water capacity, and what's still unproven, with an eye toward eventually running this as a serious ag operation, where good water is non-negotiable.
The verdict. The aquifer under this property is healthy and is not the constraint — and with Jerry & Don's service file now in hand (received 2026-07-06), the extraction picture is far better documented than the disclosure packet suggested. All three wells have been professionally tested at least once: the primary shows 4–10.6 GPM across five tests since 2002; the 168-ft "Weeks" well was the best producer on record (10–11.5 GPM in 2000–01); the old ~100-ft steel well is weak (~2 GPM, sand). Water quality finally has real data too: minerals look fine for irrigation, but the water is hard, the primary has a recurring sulfur smell, and it pulls sand when pumped hard.
The open items have narrowed to three: a current re-test (the backup-well data is 25 years old — J&D is quoting this now), the missing lab results (bacteria, arsenic, boron — sampled repeatedly, never in the file), and reconciling the tank inventory. Still a real, contingency-worthy diligence item — but the unknown just shrank a lot.
The disclosure packet held one formal well inspection — the 2021 yield-certification pump test on the primary (filed as Permit Sonoma's WLS-010 form + Jerry & Don's Well Test Report #1493, commissioned for the prior owner's cannabis application). The service file Jerry & Don's sent on 2026-07-06 shows the real depth of the record: 25 years of professional well work — Weeks Drilling & Pump tested both older wells in 2000, Jerry & Don's tested wells in 2001 (×2), 2003, 2006, 2014 and 2021, and Fisch Bros. Drilling drilled (and completion-reported) the primary in 2002.
Sources: Well Documents — WLS-010 Certification + Well Test Report #1493 (5 pp); Jerry & Don's service-file records (10 pp, received 2026-07-06). Servicing arrangement confirmed in the Seller Property Questionnaire.
This is the site's primary domestic/irrigation well, near the southwest corner of the parcel — the well Ben's records call "the 5″ PVC well drilled in 2002." Here's what the 2021 certification test measured.
| Parameter | Result | Read |
|---|---|---|
| Well type / depth | Drilled 2002 · 296–297 ft | 5″ F480 PVC casing (per the completion report and the 2014 test; the WLS-010's "steel" is a mis-entry), sanitary seal present |
| Location / elevation | 38°19′50″N, 122°50′42″W | SW corner; wellhead ≈130 ft elevation; "in field on hill," equipment in sheds (2014) |
| Pump | 1½ hp 10GS15 | Submersible, set at 280 ft (Goulds 10LS15412 in the 2003–06 tests — replaced along the way; equipment judged "recent" in 2014) |
| Static water level | 48 ft | Below top of casing, at rest — 17–50 ft across every test since 2003 |
| Stabilized pumping level | 88 ft | → drawdown of 40 ft under load |
| Certified yield | 4.0 GPM | Sustained 6 hr 10 min; 8 hr 10 min total test; 2,167 gal pumped |
| Specific capacity | 0.1 gpm/ft | Very low — a tight, fractured-rock well |
| Recovery | 100% Pass | Recovered to ~37 ft within ~49 hr (threshold: ≥90% in 72 hr) |
| Booster / pressure | WX-201 · 130 psi | 3SVB1H5CO booster pump, electrical rated "Good" |
| Water-quality panel | Left N/A in 2021 | The 2021 form skipped it — but the 2014 test ran a real panel (see Water quality below) |
| When | Tester | Yield | Notes |
|---|---|---|---|
| Aug 2002 | Fisch Bros. (completion airlift) | est. 8 GPM | 4-hr airlift, 220 ft drawdown; form itself warns it "may not be representative of long-term yield" |
| Jul 2003 | Jerry & Don's | 7.3 GPM | @ 162 ft pumping level after 4 hr (static 20 ft). Trace sand at start — pump throttled to avoid it; water cloudy, sulfur smell |
| Sep 2006 | Jerry & Don's (draft) | 8 GPM | @ 234 ft after 4 hr (static 17 ft). "Strong sulfur smell," traces of sand |
| May 2014 | Jerry & Don's #1024 | 10.6 GPM | Stabilized @ 256 ft, 50 min constant level, 2 hr 10 min total (static 50 ft). Ran the water panel; equipment "recent"; open sounder port re-plugged for sanitation |
| Sep 2021 | Jerry & Don's #1493 (certified) | 4.0 GPM | Sustained 6 hr 10 min at just 40 ft drawdown (static 48 → 88 ft); 100% recovery in ~49 hr |
How to read the spread — 4.0 vs 10.6 GPM. The certified 2021 test drew the well down only 40 ft and held 4.0 GPM with full recovery — a conservative, compliance-grade number. The 2003–2014 tests pulled the level down 150–200+ ft (the pump sits at 280 ft) and sustained 7.3–10.6 GPM. So deliverable yield depends on how hard you pull: with static at 17–50 ft there's roughly 200 ft of working drawdown above the pump, and the practical ceiling is sand and turbidity when pumped hard (J&D throttled it in 2003 for exactly that), not the certified 4.0. Storage buffers the rest: current ag use (~0.66 ac-ft/yr ≈ 590 gal/day) is a few hours of pumping a day even at 4 GPM. The low specific capacity (~0.04–0.1 gpm/ft across tests) is typical of west-Sonoma bedrock wells. The recurring sulfur smell and trace sand are quality/maintenance notes, not yield problems — see Water quality below.
Sources: Well Documents — WLS-010 form (p. 1), pump-test data log (p. 2), Well Test Report #1493 (pp. 4–5); Jerry & Don's service-file records — DWR completion report № 807042 (p. 1), 2003 test (p. 6), 2006 draft test + cover letter (pp. 4–5), 2014 test #1024 (pp. 9–10).
The storage picture is much clearer now — the hand-drawn system map in Jerry & Don's file shows the whole tank-and-booster chain — but the counts across sources still don't fully agree:
How the water moves (per the system map New): the primary well fills a 4,000-gal concrete tank at the wellhead on a float switch; a booster pushes water up the hill to the bank of 4 steel tanks and a mid-property 10,000-gal concrete (solenoid fill, its own booster), and onward to an upper 10,000-gal concrete with a Cla-Val float valve that gravity-feeds the cottages' own 10,000-gal tank and the horse-barn line (that barn booster is marked "not in use"). Separately, the "olive tree" well (8″ steel, ½-hp submersible — the weak one) runs the houses' pressure system. One well on the map is flagged "well — NOT IN USE."
Storage is doing real work here. Gravity plus boosters plus ~40k gal of buffer is exactly the right architecture for low-yield bedrock wells — the tanks convert a trickle into usable peak flow. It also means tank condition and the true inventory matter: confirm counts, sizes and serviceability with Nathan during the yield test; for an intensive ag plan, expanded storage remains one of the cheaper ways to stretch these wells.
Where the four tanks sit matters. The Transfer Disclosure (§C.7) reports that soil can slump on the west-side slope "below the 4 water tanks" during extreme rain — it's happened "a few times in 24 years," each time cleared with a tractor and the perimeter road rebuilt. So the concrete-tank pad sits above a known, minor, recurring slump zone. Combined with §C.6 (the pad sits on extensive select fill over a former quarry floor), the west-side ground near the storage warrants a geotech look before relying on or expanding that pad.
Sources: Water-system schematics + hand-drawn system maps (received 2026-07-06 — tanks, boosters, gravity feed, "well not in use"); Seller list of Amenities (~45,000 gal, 3 wells); Well Test Report #1493 (the "4 × 5,000-gal concrete" tanks, p. 4); Transfer Disclosure (TDS) §C.6 (fill) and §C.7 (slump below the 4 tanks).
The parcel has three active wells (confirmed in the seller's amenities list and the hydrogeologic study). The service file finally puts numbers on all three — with the caveat that the two backups were last tested 25 years ago:
| Well | Construction | Test history & notes |
|---|---|---|
| SW primary — the 5″ PVC well (Wel 21-0414 / DWR 807042) | Drilled 2002 (Fisch Bros.) · 297 ft · 5″ PVC, perforated 160–297 ft · pump @ 280 ft | est. 8 (2002) → 7.3 (2003) → 8 (2006) → 10.6 (2014) → 4.0 certified, 100% recovery (2021). Recurring sulfur smell + trace sand. Active — fills the main storage chain |
| The "Weeks" well | 168 ft · drilled by Weeks Drilling & Pump · 6⅝″ PVC ("8″ with 6″ liner" per J&D) · perforated 68–128 & 148–168 ft | 10 GPM (2000) · 11.5 GPM (2001) — best producer on record. Pressure tank already bad in 2001; boron sampled. Possibly the map's "well not in use" Re-test |
| The old steel well | ~100 ft · 8″ steel · driller unknown (pre-2000) | 2.5 GPM (2000) · 1.85 GPM (2001). Sand at 70 ft; obstructions at 45/65/82 ft; a 1″ drop pipe found in the casing; pump was off in 2000 w/ 200 ft of wire on the surface. Likely the "olive tree" well on the houses' pressure system Weak |
Well identities are keyed by casing size + depth across the records and the system map — solid for the primary; confirm the two backups with Nathan during the re-test, including which one is the idle well. The backup numbers are 2000–01 vintage and need re-proving; the 168-ft well's DWR completion report (Weeks drilled it) and the old well's are still worth pulling. Sources: service-file records (Weeks tests pp. 7–8; J&D 2001 tests pp. 2–3); Seller list of Amenities; hydrogeologic study (in the permit Initial Study / MND).
Until this file arrived, the record held zero water-quality data. Now there's a real mineral panel — run by Jerry & Don's on the primary well during the 2014 test — plus quality field-notes across two decades. Verdict: good irrigation water, needs treatment for domestic comfort, one important ag number still missing.
| Parameter | 2014 result | Guideline | Read |
|---|---|---|---|
| T.D.S. (salinity) | 160 ppm | < 500 | Excellent — low-salinity irrigation water |
| Nitrates | 0 | < 5 | Clean — notable for a working horse ranch |
| pH | 7.6 | 7.0–8.5 | Fine |
| Iron | 0.2 ppm | < 0.3 | OK, near the limit — can stain fixtures |
| Manganese | Trace | < 0.05 ppm | OK |
| Hardness | 27 gpg | < 3 | Very hard — 9× the guideline; scale on fixtures, heaters, drip emitters Treat |
| Arsenic · coliform · E. coli | Samples taken | — | Sent to the lab in 2014 — results not in the file Chase |
| Boron · sodium | Sampled 2000 · 2001 · 2006 | — | The key ag-suitability number (boron-sensitive crops); results never in the file Chase |
The field notes agree with the chemistry. The primary's water had a sulfur (H₂S) smell in 2003 ("cloudy… sulfur smell") and 2006 ("strong sulfur smell") and pulls trace sand when pumped hard — nuisance/treatment issues common in shale-influenced bedrock wells, not health findings. The old steel well's 2001 test flagged sodium for sampling. And the seller's own engineers designed around all of this: the Carlile Macy infrastructure plan plumbs softened water to every building in the cabin compound, and its margin notes spec a Fleck-valve softener, calcite, UV and R.O. — i.e., hard, sulfurous well water was a known, managed condition here.
What this means: for irrigation, TDS 160 / nitrate 0 water is better than much of west Sonoma — pending the boron number. For a future residence, budget a treatment train (softener ± sulfur oxidation ± UV; R.O. at taps) — a solved, few-thousand-dollar problem, not a red flag. The real gap is paperwork: get the 2014 arsenic/bacteria results and any 2000/2001/2006 lab pages from Ben, and run the full potability + ag panel before close.
Sources: service-file records — 2014 panel (p. 10), sulfur/sand comments (pp. 5–6), sample flags on the 2000–01 tests (pp. 2–3, 7–8); system schematics — softened-water plumbing + treatment notes.
The prior owner's permit work left behind one genuinely useful asset: a basin-wide hydrogeologic study (Hurvitz Environmental, 2022). Its conclusions are about the aquifer, so they hold regardless of what the land is used for — and they're reassuring on the question of whether the resource can support a serious ag draw.
What this means for an ag project. At the resource level there's ample headroom — current use is a rounding error against annual recharge, and even a far heavier draw was judged sustainable with no overdraft and no harm to neighbors. So the basin is a green light. The limiter is purely on-site: how much you can physically extract and store. Scaling water for serious ag here is an infrastructure question (wells + storage), not a question of whether the water is in the ground.
Source: Hydrogeologic study, summarized in the CEQA Initial Study / MND — water-supply narrative and Table 4 (p. 52). The underlying report (Hurvitz Environmental Services, 2022-01-26) isn't in the packet; request it from the listing agent for the full well-interference and drawdown analysis.
As it runs now: the wells and ~40,000+ gal of storage have supported a commercial vegetable farm, a horse-boarding operation, livestock and landscaping for years on roughly 0.66 acre-ft/yr of groundwater, with the certified primary at 4.0 GPM / 100% recovery. The seller discloses no dry-well history (no county drought-tank assistance), no water intrusion, no defects in the well or plumbing, and no restrictions or surcharges on the wells or groundwater. For the current level of use, the water has been sufficient and uneventful.
For a future residence: the same wells should comfortably serve a modest house alongside continued ag use — the binding constraints are storage and treatment (hard water + sulfur are documented; bacteria/arsenic results still unseen), not flow. Budget the treatment train; confirm potability before you trust it.
For a serious ag operation: this is where it gets real. Whether the property can water an intensive, irrigated ag use comes down to combined deliverable yield across all three wells plus storage — and the file now says that could plausibly be 16–24 GPM (vs. the 4-GPM single-well picture) if the backups still perform like 2000–01. Two-thirds of that is 25-year-old data. The aquifer can supply it; the current J&D re-test is what turns "plausible" into "proven."
Sources: Seller Property Questionnaire (SPQ) §§8–10 (no dry-well assistance, intrusion, or well restrictions); Transfer Disclosure (TDS) (water supply = private well; septic).
Don't count on surface water. The Compass listing markets a "year-round creek" for irrigation, but the seller's questionnaire answers No to rivers, streams, springs or high water-table affecting the property (§10.C), and the hydrogeologic study confirms no Class I/II streams on-site — only ephemeral Class III drainages plus the man-made retention pond. Plan irrigation as groundwater + rainwater, not a perennial surface source, until proven otherwise on a site walk.
Sources: SPQ §10.C; hydrogeologic study / Initial Study (no Class I/II streams on-site; ephemeral Class III drainages only).
Every figure on this page traces to one of these — the seller's disclosure packet, the permit-era water studies, and (new) Jerry & Don's service file, mirrored here so you can read the original alongside the finding.
| Document | What it sources here |
|---|---|
| Jerry & Don's service-file records New | Received from Ben Campanile 2026-07-06: the DWR completion report № 807042 for the 2002 primary well, seven well tests (Weeks 2000 ×2 · J&D 2001 ×2, 2003, 2006, 2014), and the 2014 water-quality panel |
| Water-system schematics New | Same delivery: Carlile Macy site-infrastructure plans (softened-water plumbing, treatment margin-notes), the architect's site sheet (tent cabins / bath house / well), and the hand-drawn system maps — tanks, boosters, gravity feed, and the "well not in use" |
| Well Documents — WLS-010 + Well Test Report #1493 | The certified 2021 inspection: who tested it, the certified well's yield and recovery, the tank bank as then recorded, and the quality panel left N/A |
| Seller list of Amenities | ~45,000 gal of storage; 3 wells; "Water and wells" among the studies on file |
| Seller Property Questionnaire (SPQ) | Bi-annual well/pump servicing by Jerry & Don's; no dry-well assistance, water intrusion, streams/springs, or well restrictions disclosed |
| Transfer Disclosure Statement (TDS) | Water supply = private well; fill over the former quarry floor (§C.6); recurring soil slump below the 4 tanks (§C.7) |
| Hydrogeologic study (in the CEQA Initial Study / MND) | Aquifer storage and recharge, sustainability / no-overdraft finding, and the three wells |