THE V-FAN
HEATING LAB.
Forget the brochure. This is the absurdly nerdy version: how a 1.95kW Vortex Air TP09-1PRO actually warms a cold room, why the air warms in minutes but the room takes hours, what 20°C really means, when oscillation helps, how much heat leaks away, and what it costs while all of that is happening.
More photos. More graphics. Same heating-first story.
The house baseline is the interesting bit: central heating keeps the whole home at 19.5°C, and the Vortex picks up the slack in the living room, nudging the occupied comfort zone to about 20–21°C when you want extra warmth exactly where you sit.
The V-Fan in context
A warm visual of the black Vortex doing what it is best at: topping up comfort in the living room rather than trying to heat the entire house from cold.
The core NIX strategy
Let the central heating maintain the efficient 19.5°C background, then use the Vortex as a zone heater to lift the living-room comfort bubble only where it matters.
That distinction changes the entire economics. The central heating establishes the 19.5°C whole-house baseline; the Vortex becomes a precision comfort tool rather than a substitute boiler.
Watch the Vortex Air Cleanse TP09-1 Pro in use.
For a proper look at the real machine, controls and physical size, this independent review is a useful companion to the NIX heating analysis.
Heating the air is easy. Heating the room is the hard bit.
Take a perfectly ordinary living room measuring 4m × 4m × 2.4m. That is 38.4m³ of air. Start at a chilly 14°C and aim for 20°C: a 6°C rise.
Almost nothing compared with the energy absorbed by the room itself.
That is the theoretical time to heat the air if nothing else absorbed heat and no heat escaped.
Which immediately proves that the expensive bit is not the air.
The room behaves like a thermal battery with a hole in it.
A useful first-order heating model treats the room as one effective thermal mass. The heater charges that thermal mass while the building continuously loses heat to outside.
C is effective thermal capacitance in kWh/K. P is heater power in kW. H is whole-room heat-loss coefficient in kW/K. Tₒ is outdoor temperature.
The model is deliberately simple, but it exposes the physics brilliantly: as the room warms, the temperature difference to outside increases, so the losses get larger. The last degree takes longer than the first.
14°C → 20°C, 5°C outside, 1.95kW heater.
Below are three plausible modelled rooms of the same size. The heater is identical; the building changes.
| Room | Heat loss H | Thermal mass C | Predicted time to 20°C | Warm-up energy | Warm-up cost |
|---|---|---|---|---|---|
| Good | 48 W/K | 0.45 kWh/K | ~1.97 h | ~3.85 kWh | ~£1.01 |
| Average | 90 W/K | 0.55 kWh/K | ~3.92 h | ~7.65 kWh | ~£2.01 |
| Draughty | 140 W/K | 0.72 kWh/K | Cannot reach 20°C | — | — |
Every heater has a temperature it simply cannot beat.
At steady state, heater output equals room heat loss:
Purely theoretical steady-state ceiling at 5°C outside. The thermostat would stop heating long before this.
Enough spare capacity to reach and hold 20°C, but warm-up is not instant.
Full power still cannot overcome the building's losses at a 15°C indoor/outdoor difference.
Every extra degree costs more than the previous one.
Once the room is warm, the heater only needs to replace the heat leaving the room. For the average 90W/K example with 5°C outside:
| Target | ΔT to outside | Heat loss | Average electrical demand | Approx running cost/hour |
|---|---|---|---|---|
| 18°C | 13K | 1.17kW | 1.17kW | 30.8p |
| 19°C | 14K | 1.26kW | 1.26kW | 33.2p |
| 20°C | 15K | 1.35kW | 1.35kW | 35.5p |
| 21°C | 16K | 1.44kW | 1.44kW | 37.9p |
| 22°C | 17K | 1.53kW | 1.53kW | 40.3p |
In this model, each extra degree adds about 90 watts of continuous heat demand. At 26.32p/kWh that is around 2.37p per hour per extra degree while that outside temperature persists.
Running costs at a glance
A visual summary of the real-world numbers: cheap in fan mode, meaningful cost at full heat, and a more interesting middle ground once the thermostat begins cycling.
Quick-start heating cheat sheet
Central heating baseline 19.5°C, Vortex target 20°C, oscillation ON for whole-room warm-up, stronger airflow to start, then let the thermostat cycle.
Oscillation does not create more heat. It makes the heat more useful.

The heater still has the same maximum 1.95kW whether it oscillates or not. The gain is distribution.
A robust worked example with no scripts required.
For a 4m × 4m × 2.4m room, starting at 14°C, target 20°C, outside 5°C, and using the average-room assumptions from this article:
| Metric | Result |
|---|---|
| Room volume | 38.4 m³ |
| Air-only energy to raise 14→20°C | 0.078 kWh |
| Modelled room heat-loss coefficient | 90 W/K |
| Modelled effective thermal mass | 0.55 kWh/K |
| Predicted warm-up time | ≈3.9 hours |
| Warm-up energy at full heater output | ≈7.6 kWh |
| Warm-up cost at 26.32p/kWh | ≈£2.01 |
| Heat needed to hold 20°C at 5°C outside | ≈1.35 kW |
| Estimated heater duty cycle at steady 20°C | ≈69% |
| Estimated holding cost per hour | ≈35.5p |
These are modelled values, not a promise of exact performance. Actual results vary with wind, glazing, draughts, adjacent-room temperatures, solar gain, central heating contribution and thermostat position.
Where the V-Fan sits changes how quickly the room feels warm.
Give the lower intake clean access to room air. Do not bury it behind a sofa or curtain.
Aim across the occupied zone so the airflow crosses the room rather than immediately striking a nearby wall.
During cold starts, oscillation helps destroy stratification and spreads the heat load across surfaces more evenly.
The NIX cold-room routine.
51.3p/hour is the ceiling, not necessarily the normal bill.
At the Ofgem October–December 2026 average electricity unit rate of 26.32p/kWh, a continuous 1.95kW draw costs:
But once the thermostat cycles, the relevant number is average duty cycle. In the average-room example at 20°C with 5°C outside, the room needs about 1.35kW to hold temperature, or roughly 69% of maximum output. That is around 35.5p/hour in the model.
And why that is useful.
Solar gain
Sun through glass can add hundreds of watts. A bright winter afternoon can make the heater appear magically efficient.
People and appliances
A resting adult is a small heater. TVs, computers and cooking also reduce the electrical heat the V-Fan must provide.
Air leakage
Wind can radically increase infiltration. The same room can behave like a different building on a gusty night.
Thermostat position
If the V-Fan senses its own warm discharge, it can cycle early. Good mixing and sensible placement reduce that error.
Central heating
If radiators are already adding heat, this model over-attributes the temperature rise to the V-Fan.
Thermal lag
Furniture and walls do not instantly become the same temperature as the air, so a one-node model can never reproduce every transient perfectly.
The house does the heavy lifting. The Vortex picks up the slack.
My house is already centrally heated to a background temperature of 19.5°C. That matters, because the Vortex is not being asked to drag a stone-cold room all the way from winter temperatures up to comfort on its own.
Instead, the central heating establishes the thermal baseline for the whole house, while the Vortex acts as a local comfort heater in the living room. Its job is to pick up the slack: take the occupied zone from roughly 19.5°C to around 20–21°C, improve air movement, reduce local cold spots and make the room feel properly comfortable without turning the whole-house thermostat up.
This also changes the economics dramatically. If the room only needs another half to one degree of lift, the Vortex is working as a targeted trim heater rather than a primary heating system. In practical terms, that is exactly where a portable electric heater makes the most sense: heat the occupied room a little more, rather than heating every room in the house more.
20°C + oscillation is not a magic setting. It is a very sensible engineering compromise.
Central heating: 19.5°C baseline. Vortex: living-room top-up to 20–21°C. That is the operating philosophy behind this entire test.
The V-Fan has enough power to be a serious room heater, but whether it can actually heat a room depends on the room's heat loss. In a decent room, 1.95kW gives useful reserve capacity. In a very leaky room on a cold day, it can spend all day at maximum and still lose the fight.
That is why my default strategy is 20°C, oscillation ON, unrestricted intake, open throw across the occupied area, and then watch whether the thermostat begins cycling. Cycling means the heater has moved from “catch-up” into “maintenance”. That is the point where comfort and cost finally become predictable.
We can estimate the room’s real heat loss from its own behaviour.
The earlier sections use assumed heat-loss coefficients. The next step is much better: measure the room and infer H from real data. You do not need laboratory equipment. A reasonably stable indoor temperature sensor, an outside temperature reading, a clock and the V-Fan are enough to get surprisingly useful results.
Method A — steady-state duty-cycle test
This is the cleanest method if the room has already reached a stable temperature. Suppose the room is holding 20.0°C, outside is 5.0°C, and over a measured hour the heater is actually energised for 42 minutes.
That one experiment would put the room almost exactly into the “average” example used earlier. It also means that every additional 1°C of indoor/outdoor temperature difference costs roughly another 91 watts continuously.
The heater is delivering 70% of its rated output on average.
That is the power actually balancing the building at that moment.
A genuinely useful number that can be reused at other outdoor temperatures.
The same room becomes a completely different heating problem as the weather changes.
Using an inferred room heat-loss coefficient of 91W/K, we can predict the average heat required to hold 20°C:
| Outside | Indoor target | ΔT | Heat required | V-Fan duty cycle | Approx cost/hour |
|---|---|---|---|---|---|
| 15°C | 20°C | 5K | 0.46kW | 23% | 12.0p |
| 10°C | 20°C | 10K | 0.91kW | 47% | 24.0p |
| 5°C | 20°C | 15K | 1.37kW | 70% | 35.9p |
| 2°C | 20°C | 18K | 1.64kW | 84% | 43.2p |
| 0°C | 20°C | 20K | 1.82kW | 93% | 47.9p |
| -2°C | 20°C | 22K | 2.00kW | 103% | Impossible at steady state |
At around -1.4°C outside, a 91W/K room needs the full 1.95kW simply to hold 20°C. Below that, the V-Fan alone mathematically cannot maintain 20°C indefinitely.
This number is hugely useful because it turns the appliance from a vague “1.95kW heater” into something you can match against the actual building.
One degree sounds trivial. Thermally, it is not.
For a 91W/K room, raising the target from 20°C to 21°C adds about 91W of continuous load. At 26.32p/kWh:
That does not mean “never use 21°C”. Comfort matters. It means you can now see the trade in real units: if 20°C is comfortable, there is no engineering reason to run 21°C. If 21°C materially improves comfort, the price of that extra degree is measurable rather than mysterious.
A heater does not heat a perfectly mixed box.
The thermostat display might say 20°C while your ankles are at 18°C and the air above head height is 22°C. That is stratification. Portable fan heaters reduce it, but they do not abolish it.
Too close to the V-Fan
The sensor may see the warm recirculation plume and cycle the heater before the sofa area is truly warm.
Too near a window
The sensor can read artificially low due to cold downdraughts from glazing.
Too high
Warm air rises. A sensor at 1.8m can overstate the temperature experienced by a seated person.
For room testing, a separate thermometer around seated chest height, away from direct discharge, windows, doors and radiators, gives a much better representation of lived comfort.
Oscillation is really about reducing temperature variance.
When oscillation is ON, the average room heat input does not rise. What can improve is the spatial distribution of that heat.
| Situation | Oscillation OFF | Oscillation ON |
|---|---|---|
| Cold start | Fast local warming, larger gradients | Better whole-room mixing |
| One person at a desk | Strong personal comfort | Less concentrated sensation |
| Whole-room thermostat control | Higher chance of local warm bubble | More representative mixed air |
| Several people around a room | One hot zone | Better coverage |
| Very draughty room | May protect one comfort zone | Can spread limited heat more thinly |
This is why my default remains oscillation ON for room heating. The exception is deliberate personal heating, where concentrating the jet can produce more perceived warmth for the same electrical input.
Usually no. It changes delivery, not the electrical heater rating.
The PTC element has a finite electrical input. Higher airflow can carry that heat away from the element faster, so the outlet air may feel less scorching while the total heat delivered to the room remains broadly governed by the heater power and its controls.
Best for cold starts and mixing. Faster air exchange between the warm outlet stream and the room.
Often a good compromise once the room is approaching target.
Useful for quieter maintenance or local comfort, provided the thermostat still controls the heat sensibly.
The important point is that “hotter-feeling air” is not necessarily “more watts into the room”. A slower jet can feel hotter because each kilogram of air receives a larger temperature rise.
Where does the first few kilowatt-hours actually go?
Imagine our average room uses around 7.6kWh during a long 14→20°C recovery. The air itself only accounts for about 0.08kWh. The rest is a mixture of:
| Destination | Physical mechanism | Why it matters |
|---|---|---|
| Walls / plaster | Sensible heat storage | Large mass; initially colder than target air |
| Floor | Sensible heat + conduction | Can be a substantial cold sink, especially over unheated spaces |
| Furniture | Sensible heat storage | Sofas, timber, books and cabinets all absorb energy |
| Windows | Conduction + radiation | Continually dump heat outdoors |
| Ventilation / infiltration | Warm air replaced by cold air | Can dominate on windy nights |
| Adjacent rooms | Conduction / air exchange | Your warm room often heats the rest of the house a little too |
This is why the first warm-up after a house has been cold for a day can be dramatically slower than reheating the same room after a short setback.
14°C to 20°C is a different job from 18°C to 20°C.
Using the same average-room model, the second situation requires far less stored energy to be replaced.
| Start | Target | Outdoor | Modelled recovery | Indicative energy |
|---|---|---|---|---|
| 14°C | 20°C | 5°C | ~3.9h | ~7.6kWh |
| 16°C | 20°C | 5°C | ~2.7h | ~5.3kWh |
| 18°C | 20°C | 5°C | ~1.5h | ~2.9kWh |
| 19°C | 20°C | 5°C | ~0.8h | ~1.6kWh |
That is the engineering logic behind background heating. It is not necessarily cheaper to keep everything warm all day, but avoiding a very deep setback can massively reduce the time required for a portable heater to restore comfort.
A repeatable protocol, not random temperature screenshots.
Turn the heat off and watch the house reveal itself.
When internal heating is off, the simplified room model becomes:
The room's temperature difference to outside decays approximately exponentially. If we already have an estimate of thermal capacitance C, the cool-down curve can estimate H. Or if H is known from a steady-state heater test, the curve can estimate C.
For example, if the room falls from 20°C to 18°C over two hours while outside stays close to 5°C, the decay ratio is:
That is not enough by itself to completely characterise the building, but paired with a heater-duty test it becomes extremely powerful.
A dirty filter does not make electricity disappear, but it can wreck airflow.
The V-Fan draws room air through the lower intake and filter before pushing it through the heating system. As filter resistance rises, airflow can fall. That changes how effectively the machine mixes the room and can alter outlet temperature and internal control behaviour.
For heating, the practical maintenance rule is simple:
Inspect the intake and filter regularly for visible dust loading.
A change in airflow noise at the same setting can be useful evidence.
If warm-up becomes slower under similar weather, filter condition belongs on the suspect list.
This is where electric resistance heat can make strategic sense.
A 1.95kW resistive heater does not beat another 1.95kW resistive heater by some secret efficiency trick. Almost all of the electrical energy consumed in the room ends up as heat. The economic advantage comes from where and when you choose to heat.
If the alternative is raising several rooms by 1–2°C just to make one occupied living room comfortable, a local heater can sometimes win despite expensive electricity because it avoids heating unnecessary space.
WEATHER ↗A–Z