Jimboomba Water Hardness & Quality Report (2026)
Water Hardness
~60–119 mg/L
Moderately Hardestimated · not lab-verified
Source
mixed
pH Level
7.3
neutral = 7.0
Lead
0.003 mg/L
✓ Below action level
TDS
169.9 mg/L
Est. Daily Cost
A$0.28
energy & soap waste
Source: BOM National Performance Report & ADWG · Updated 2026
0–60
mg/L
Soft
61–120
mg/L
Moderately Hard
121–180
mg/L
Hard
180+
mg/L
Very Hard
Appliance Damage Report
In Jimboomba, your appliances are currently losing 12% efficiency due to mineral buildup.
| Appliance | In Jimboomba | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 7.5 yrs | 8.5 yrs | -12% |
| Washing Machine | 10.6 yrs | 12 yrs | -12% |
| Water Heater | 13.2 yrs | 15 yrs | -12% |
Regional Water Comparison
How Jimboomba compares to its nearest neighbours
| City | Hardness | Risk | Source |
|---|---|---|---|
| ▶ Jimboomba, Queensland | ≈ 60–119 mg/L | 🟡 Moderately Hard | mixed |
| Crestmead, Queensland | ≈ 60–120 mg/L | 🟡 Moderately Hard | mixed |
| Regents Park, Queensland | ≈ 120–179 mg/L | 🟠 Hard | mixed |
| Marsden, Queensland | ≈ 60–120 mg/L | 🟡 Moderately Hard | mixed |
| Kingston, Queensland | ≈ 60–120 mg/L | 🟡 Moderately Hard | mixed |
National Benchmark
How Jimboomba compares to the Australia average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Jimboomba | ≈ 60–119 mg/L | 🟡 Low |
| Australia National Avg | 125 mg/L | 🟠 Moderate |
| Boronia Top Rated | 5 mg/L | 🟢 None |
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What Makes Jimboomba's Water Unique?
Local geology and source profile
Residents of Jimboomba, situated in the Logan City Council area southeast of Brisbane, receive their drinking water through a collaborative effort involving Logan City Council, Seqwater, and Urban Utilities. The primary water supply originates from Wivenhoe, Somerset, and North Pine reservoirs, channeled through the South East Queensland Water Grid. During periods of high demand, this surface water is supplemented by local groundwater drawn from the Logan River alluvial aquifer. Water treatment is primarily handled at Seqwater's major facilities, such as Mt Crosby and North Pine, before Logan City Council manages the final distribution to homes and businesses across Jimboomba township and the adjacent rural-residential areas nestled in the foothills of the Scenic Rim.
The water's journey begins in the catchment areas feeding the tributaries of the Brisbane, Stanley, and Logan Rivers. These headwaters originate in the Main Range and McPherson Range, areas characterized by basalt-capped peaks. The underlying geology consists of Cainozoic basalts and rhyolites overlying Mesozoic sandstones. Additionally, alluvial aquifers along the Logan River contribute groundwater with a similar chemical profile. This geological makeup results in water that is moderately mineralized, placing it between the softer supplies from protected, forested catchments to the south and the harder waters found in basins dominated entirely by limestone. The presence of dissolved calcium and magnesium from these geological formations contributes to its moderately hard classification.
This moderately hard water can lead to the gradual buildup of limescale in common household items like kettles and showerheads, typically becoming noticeable within two to five years. Homeowners might also observe occasional spotting on glassware and find their skin or hair feels drier after washing. Appliances that operate with heat, such as hot water systems and coffee machines, are often the most affected by scale formation. Regular monthly cleaning with vinegar can help manage this buildup, and an annual check of your hot water service is advisable. While a water softener is an optional addition for most households, it may be beneficial if you live in areas known for higher mineral content or if you have particularly sensitive appliances. The water quality consistently meets the Australian Drinking Water Guidelines, with the Logan City 2022/23 report showing 100% compliance for E. coli, and typical pH levels ranging from 7.2 to 8.0 due to lime dosing for corrosion control.
Geology & Source: Mesozoic Great Artesian Basin sediments; Cainozoic alluvial deposits, basalt and rhyolite flows; limestone-influenced watersheds; moderate hardness from calcium and magnesium
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