EvapMargin

The layer water-loss nomograph

The layer water-loss nomograph reads how much water leaves the top of a fresh layer before the next layer covers it. It gives that as a loss in grams per square metre, read against two thresholds for the bond. This guide says why the loss sets the bond, how to read the figure, what to measure and how far to trust the number.

Background

The top of a layer loses its sheen while the nozzle is away. By the time the nozzle comes back round, the top is matt and cool to the touch, and the next layer lands on it. The joint that forms there is the weakest place in a printed wall, and its strength follows how much water that top has lost.

Sanjayan et al. (2018) tied the strength of that joint to the moisture on the surface the next layer meets. Keita et al. (2019) measured it against the water the top had lost as a share of the mix water. A loss of 0.1 % left the strength unchanged, and 1 % cut it by about 40 %. They traced the loss to a dry skin on the top, where the cement finds too little water to harden and the paste stays porous. The bond follows a quantity of water, and a quantity is a rate times a time.

The ACI 305 tool reads the rate, the evaporation rate E in kilograms per square metre per hour. This tool multiplies the rate by the layer cycle, the time the top stands open. That product has a name on this tool: the water loss per layer, W, in grams per square metre. It is an upper bound: a wet top loses water as fast as the air can take it, and a drying top loses less. The question at the printer is how long the cycle can be, and the fifth panel answers in minutes.

What the next layer meets The printed wall in section at two moments of one layer cycle, side by side over a time axis. On the left the wall is four layers high and the fresh layer on top stands open: arrows show water leaving its top, and arrows on both flanks of every layer show that the wall loses water sideways as well. On the right, one layer cycle later, a next layer covers that top and makes the joint, and the flanks of all five layers still lose water. A bracket under the two moments marks the one layer cycle between them. Water leaves the open top Fresh layer Layers below The next layer makes the joint Next layer Fresh layer Layers below The flanks lose water too, every layer One layer cycle Time
Figure 01.1What the next layer meets. The printed wall in section at two moments of one layer cycle. Every face stands open, and the water the top loses before the next layer covers it sets the strength of the joint.

How to read it

The nomograph is five panels, read clockwise from the top left, and one construction line threads all five. The top half is the ACI 305 nomograph's top half with its index turned into a measurement. The air moisture level A is the vapour the air already holds, and the moisture deficit D is how much more a saturated top holds. Both are in grams per cubic metre.

Two things differ from the ACI 305 nomograph. The tool draws the air movement rays at the set temperatures, because a warm face drives more of its own air than a cool one. The W axis along the foot is logarithmic and increases leftward. On it the bond threshold, 10 g/m², and the bond limit, 100 g/m², stand a decade apart. The verdict key under the figure names the three tints: Pass below 10, Bond risk 10 to 100, High bond risk 100 and above.

Each panel also draws both thresholds in its own input. A threshold curve is the dashed member of the panel's family that puts the reading exactly on the threshold, with the other four as set. In the layer cycle panel "10 · 6.2 min" says that a cycle longer than about six minutes crosses the bond threshold. Between the curves the panel is tinted with the verdict that value of its input would read. Every curve moves when any input moves, the ambient temperature included. Each panel answers one question: how far its input can move before the verdict changes.

The five panels and the three carriers The five panels of the nomograph as boxes, in the two-by-two grid the figure itself uses. Top left is the ambient temperature panel, which control 1, the ambient temperature, and control 2, the relative humidity, govern. Top right is the surface temperature panel, control 3. Bottom right is the air movement panel, control 4, drawn at the set temperatures. Bottom left is the layer-cycle panel, control 5. The water-loss bar lies along the foot of that panel; no control sets it, because it carries the reading. A dashed arrow runs right out of the ambient panel into the surface panel with the air moisture level A, which is the vertical axis of both. A second runs down out of the surface panel into the air movement panel with the moisture deficit D, the horizontal axis of both. A third runs left out of the air movement panel into the layer-cycle panel with the evaporation rate E, the vertical axis of both. A fourth drops out of the layer-cycle panel onto the bar with the water loss W, the horizontal axis of both, and W is the reading. Each pair of panels shares an axis, so the line hands each value on and the reader carries no number. Air moisture level A the vertical axis of both panels Moisture deficit D the horizontal axis of both panels Evaporation rate E the vertical axis of both panels W, the reading 1 Ambient temperature 2 Relative humidity 3 Surface temperature 4 Air movement at the set temperatures 5 Layer cycle Water loss no control sets it Each pair of panels shares an axis: A, then D, then E, then W. The line hands each value on, so you carry no number.
Figure 02.1The five panels and the three carriers. The panels as boxes and the carriers as arrows, in the order the construction line meets them, so the loop closes on the water-loss bar.

What to measure

Five inputs, in the order the line reads them. Take the first three as the ACI 305 tool takes them: at the fresh layer, not at the wall of the hall. As the wall rises, the sensor has to rise with it. Air movement is in metres per second, the unit an indoor anemometer reads. The layer cycle is the time from laying a layer at a place to covering it there with the next.

Table 03.1The five inputs. Each input with its unit, its range, where to take the reading, and what each air-movement preset means.
Input Unit Range Where to take the reading What the tool accepts
Step 1Ambient temperature °C 5 to 40 In the air beside the printhead, at the height of the fresh layer. None. Enter the temperature you measured.
Step 2Relative humidity % 20 to 100 In the same air as the temperature, clear of the door and of the mixer. None. Enter the relative humidity you measured.
Step 3Surface temperature °C 5 to 40 On the top of the layer just laid, with an infrared thermometer. The printing temperature, as the control asks. Enter the infrared reading where you have one: a top 3 °C under the air loses about a third less.
Step 4Air movement m/s 0.10 to 1.00 At printhead height, in the air that crosses the face, with a hot-wire anemometer. Still 0.10 m/s, a closed hall.
Ventilated 0.20 m/s, the ventilation running.
Fan or open door 0.50 m/s, air moved on purpose.
Step 5Layer cycle time min 0.5 to 60 Time the nozzle from one pass to the next at the same place on the wall, or take the pause. The perimeter divided by the print speed, where you cannot time it.

Two questions before you read. Question one: did the surface temperature come off the top of the layer, or is it the printing temperature? Question two: was the cycle timed at the wall, or taken from the perimeter and the print speed? Each answer moves the line.

The model

The rate on this tool is the evaporation from a vertical wet face in a hall, where the air moves at 0.1 to 1 m/s. Menzel (1954) fitted the ACI 305R equation to open water in the open air, and Uno (1998) gave it its closed form. Its air movement term reads as if air at 4 km/h always crossed the face. In a still hall that floor puts the ACI value 25 to 40 % above this model, and from 0.5 m/s up the two draw together. The ACI 305 tool keeps the ACI value. This one reads the hall.

The chain in Figure 04.1 has five steps, M1 to M5. Buck (1981) gives how much vapour saturated air holds at each temperature, and from it come the air moisture level, M1, and the moisture deficit, M2. M3 is the transfer coefficient, the speed at which the air beside the face carries that vapour away, in two parts. Water vapour is lighter than dry air, so the moist air at a wet face rises on its own: that is buoyancy. A warm face adds to it. Churchill and Chu (1975) give that part from the density difference between the hall's air and the air at the face, over the wet height. The wet height is the wall below the fresh layer that is still wet. The laminar plate, the rate for smooth flow along a flat surface, gives the part the hall's ventilation drives. Churchill (1977) joins the two by the cube rule, the cube root of the sum of their cubes, so the larger part leads. M4 is the rate E, and M5 is the loss W: E times the layer cycle.

Neither part can be dropped indoors. In still air the face's own air carries everything: at 25 °C, 55 % and a face at air temperature, the model reads 0.067 kg/m²/h. At 1 m/s the hall's air leads and the face reads 0.192. A face cooler than the hall by more than about 1.5 °C drives its air downward instead. The model reads the size of the density difference, not its sign, so the chain does not change. Where the two cancel the face's own air nearly stops, and the control's floor at 0.10 m/s keeps that dip to about a tenth. ASHRAE Standard 55 treats slower air as still.

Table 04.1Symbols and formulas. Each input, constant, property law and step in the order the model runs them, with its formula, its unit and where it enters. The verdict rule and the threshold curves close it.
Symbol Meaning and formula Unit Where it enters
The five inputs and the three settings
Ta Ambient temperature: the air temperature in the printspace, set by control 1. °C M1 and M3
RH Relative humidity of the printspace air, set by control 2. The formulas take it as r, the relative humidity divided by 100. % M1 and M3a
Ts Surface temperature of the fresh layer, set by control 3 as the printing temperature, its proxy. °C M2 and M3
u Air movement: the speed of the air over the face, set by control 4 or by one of its presets. m/s M3b
tc Layer cycle: how long the top stands open before the next layer covers it, set by control 5. min M5
W₁ Bond threshold: the loss at which the bond begins to suffer. An advanced setting, 10 by default. g/m² Verdict
W₂ Bond limit: the loss at which about 40 % of the interlayer strength is gone. An advanced setting, 100 by default. g/m² Verdict
L Wet height: the wall below the fresh layer that is still wet, the length the air runs along. An advanced setting, 0.5 by default. m M3, all three boxes
Constants
g Gravity.
9.81
m/s² M3a
R Gas constant.
8.314462
J/mol/K M1, M2 and M3a
Mv Molar mass of water vapour.
0.018015
kg/mol M1, M2 and M3a
Ma Molar mass of dry air.
0.028965
kg/mol M3a
P Air pressure.
101 325
Pa M3a
Sc Schmidt number: the viscosity of air over the diffusivity of water vapour in it, constant by construction.
0.62
none M3a and M3b
Property laws
p_sat(T) Saturation vapour pressure: the pressure of the vapour over water at temperature T, after Buck (1981).
p_sat(T) = 611.21 · exp(
(18.678 − T/234.5) · T/(257.14 + T) )
Pa M1, M2 and M3a
ρv(T, r) Vapour density: the mass of vapour in a cubic metre of air at temperature T and relative humidity r.
ρv(T, r) = r · p_sat(T) · Mv
/ (R · (T + 273.15))
kg/m³ M1 and M2
ρa(T, r) Density of humid air. It carries the buoyancy of the temperature and of the vapour together, with their sign.
ρa(T, r) = ((P − r·p_sat(T)) · Ma
+ r·p_sat(T) · Mv)
/ (R · (T + 273.15))
kg/m³ M3a
ν(Tf) Kinematic viscosity: the air's resistance to flow, at the film temperature.
ν(Tf) = 1.55·10⁻⁵
· ((Tf + 273.15)/298.15)^1.75
m²/s M3a and M3b
Dv(Tf) Diffusivity: how fast water vapour spreads through still air, at the film temperature.
Dv(Tf) = 2.50·10⁻⁵
· ((Tf + 273.15)/298.15)^1.75
m²/s M3c
Tf Film temperature: the mean of the ambient and the surface temperature, at which the air's properties are taken.
Tf = (Ta + Ts)/2
°C M3
The five steps, M1 to M5
A Air moisture level: the vapour density of the printspace air. In grams per cubic metre on the nomograph.
A = ρv(Ta, r)
kg/m³ M1
D Moisture deficit: the vapour density at the saturated top, less A. A negative deficit reads zero.
D = ρv(Ts, 1) − A
kg/m³ M2
Δρa The density difference between the hall's air and the air at the face. Positive when the air at the face is lighter.
Δρa = ρa(Ta, r) − ρa(Ts, 1)
kg/m³ M3a
Gr Grashof number: the buoyancy of that difference over the wet height, against the viscosity.
Gr = g · Δρa · L³
/ ( ½(ρa(Ta, r) + ρa(Ts, 1)) · ν² )
none M3a
Ra Rayleigh number. It may be negative, and the free branch takes its size, not its sign.
Ra = Gr · Sc
none M3a
Sh_f Free Sherwood number: the transfer the face's own air gives, after Churchill and Chu (1975).
Sh_f = { 0.825 + 0.387 · |Ra|^(1/6)
/ [1 + (0.492/Sc)^(9/16)]^(8/27) }²
none M3a
Re Reynolds number: the hall's air over the wet height, against the viscosity.
Re = u · L / ν
none M3b
Sh_p Forced Sherwood number, the laminar plate: the transfer the hall's air gives. Re stays under 500 000 across the tool's ranges.
Sh_p = 0.664 · Re^(1/2) · Sc^(1/3)
none M3b
Sh Sherwood number of the face: the two branches joined by the cube rule, after Churchill (1977).
Sh = ( Sh_f³ + Sh_p³ )^(1/3)
none M3c
hm Transfer coefficient: the speed at which the air takes vapour off the face.
hm = Sh · Dv(Tf) / L
m/s M3c
E Evaporation rate: the water leaving a square metre of the wet face in an hour.
E = 3600 · hm · D
kg/m²/h M4
W Water loss per layer: the reading, and an upper bound on the loss over one cycle.
W = 1000 · E · tc / 60
g/m² M5
Verdict and margin
Verdict The three-way judgement on W. A value exactly on a threshold takes the verdict above it.
Pass: W < W₁
Bond risk: W₁ ≤ W < W₂
High bond risk: W ≥ W₂
none Readout
Margin The distance in W from the operating point to the next threshold above it. Above the bond limit, it is measured back to the limit.
Pass: W₁ − W
Bond risk: W₂ − W
High bond risk: W − W₂
g/m² Readout
Threshold curves
E* The evaporation rate a threshold W* needs at the set layer cycle, found for the bond threshold and for the bond limit.
E* = W* / (1000 · tc / 60)
kg/m²/h Every panel
tc* The layer cycle at which the operating point sits on the threshold. Infinite when E is zero.
tc* = W* / (1000 · E / 60)
min Layer cycle panel
u* The air movement at which the operating point sits on the threshold, in closed form. When still air already exceeds the threshold there is no ray, and with no deficit no air movement reaches it.
Sh* = E* · L / (3600 · Dv · D)
Sh_p* = (Sh*³ − Sh_f³)^(1/3)
u* = (Sh_p* / (0.664 · Sc^(1/3)))²
· ν / L
m/s Air movement panel
Ts* The surface temperature at which E crosses E*: the first crossing from the set value outward. Outward is toward more loss below the threshold and toward less above it.
E(Ts) = E*
°C Surface panel
RH* The relative humidity at which E crosses E*, the first crossing from the set value outward, as for Ts*.
E(RH) = E*
% Ambient panel
Ta* The ambient temperature at which E crosses E*, the first crossing from the set value outward, as for Ts*.
E(Ta) = E*
°C Ambient panel, Ta axis
From five inputs to the water loss per layer The model as five steps in seven boxes, read downward, and each box carries its identifier above it. Step M1 is the air moisture level A. Control 1, the ambient temperature, and control 2, the relative humidity, enter it on dashed arrows. It gives A as the vapour density at the ambient temperature and that humidity, which is r times the saturation vapour pressure, times the molar mass of water, over the gas constant times the temperature in kelvin. A solid arrow hands A down to step M2, the moisture deficit D. Control 3, the surface temperature, enters it. It gives D as the vapour density at the surface temperature and saturation, less A. A negative deficit reads zero. Buck gave the saturation vapour pressure in 1981. Step M3 is the transfer coefficient, and it is three boxes in one tone. Box M3a, the free branch, on the left, takes the humid air density difference between the room and the face, gives the Grashof number from it with the wet height and the kinematic viscosity, multiplies by the Schmidt number for the Rayleigh number, and gives the free Sherwood number by Churchill and Chu, 1975. Box M3b, the forced branch, on the right, takes control 4, the air movement, on a dashed arrow from above, gives the Reynolds number from it with the wet height, and gives the forced Sherwood number by the laminar plate. The two branches join in box M3c below, where Churchill's cube rule adds their cubes and takes the cube root, and the transfer coefficient hm is that Sherwood number times the vapour diffusivity over the wet height. The viscosity and the diffusivity are taken at the film temperature, the mean of the ambient and the surface temperature. The wet height enters M3c on a dashed arrow and carries no disc, because it is a setting; it sets the length in all three boxes of the step. A solid arrow hands hm down to step M4, the evaporation rate E, which is 3600 times hm times D. The deficit reaches M4 on its own solid arrow, down the right of the coefficient, because it does not enter the coefficient. A solid arrow hands E down to step M5, the water loss per layer W. Control 5, the layer cycle, enters it. W is 1000 times E times the cycle over 60, and it is the reading, in grams per square metre. 1 Ambient temperature 2 Relative humidity 3 Surface temperature 4 Air movement Wet height L a setting 5 Layer cycle A Buck (1981) gives p_sat, here and in D. D D goes to E, not to the coefficient. Sh_f Sh_p hm E M1 M2 M3a M3b M3c M4 M5 Air moisture level A A = ρv(Ta, r), r = RH / 100 ρv(T, r) = r · p_sat(T) · Mv / (R · (T + 273.15)), in kg/m³ Moisture deficit D D = ρv(Ts, 1) − A A negative deficit reads zero. Both densities are in kg/m³. Free branch: the face's own air Δρa = ρa(Ta, r) − ρa(Ts, 1) Gr = g · Δρa · L^3 / (ρa,mean · ν^2) Ra = Gr · Sc Sh_f = {0.825 + 0.387 · |Ra|^(1/6) / [1 + (0.492/Sc)^(9/16)]^(8/27)}^2 Churchill and Chu (1975). Forced branch: the hall's air Re = u · L / ν Sh_p = 0.664 · Re^(1/2) · Sc^(1/3) The laminar plate. Re stays below 5 · 10^5. Sc = ν / Dv = 0.62 at every temperature. Transfer coefficient hm Sh = (Sh_f^3 + Sh_p^3)^(1/3) hm = Sh · Dv / L, in m/s Churchill (1977), the cube rule, n = 3. ρa is the humid air density. ν is the viscosity and Dv the diffusivity, both at (Ta + Ts) / 2. Evaporation rate E E = 3600 · hm · D In kg/m²/h. Water loss per layer W W = 1000 · E · tc / 60 The reading, in g/m².
Figure 04.1From five inputs to the water loss per layer. Each step of the model as one box with its formula, from the vapour densities through the transfer coefficient to the loss over one cycle.
Note 04.1Set-on-demand printing

Set-on-demand printing doses an accelerator at the nozzle, so a layer stiffens within seconds and sets within minutes. Three things in the chain move with it. The heat first: cement that hardens in minutes gives off its heat in minutes, and the top runs warmer than the hall. Enter the infrared reading as control 3. At 25 °C, 55 % and 0.20 m/s, a top at 30 °C loses 0.208 kg/m²/h against 0.097 at air temperature. A 5-minute cycle then reads 17.4 g/m² instead of 8.1, past the bond threshold. The bound second: the model assumes capillary flow, the pull of the fine pores, keeps the top wet for the whole cycle. A layer that sets binds that water into its paste instead, so W stays an upper bound and becomes a wider one. The joint third: both thresholds come from bond measured against water lost, and a set top makes a joint this tool does not read. A Pass says the air took little water from the top, and nothing about whether the set top accepts the next layer. Bond against loss, with the accelerator in the mix, would place the thresholds for that material.

Accuracy and limits

The reading is an estimate of the environment, not a measurement of the concrete. It does not replace ACI 305R, the mix design or the engineer's judgement. W is an upper bound: E times the layer cycle, from a top that stays wet for the whole cycle. A cast slab bleeds and keeps a film of water on its face. ACI 308R-23 says the ACI rate matches the concrete only under that film. A printed layer has no film, so its top stays wet from below: capillary flow feeds it as long as the body can supply water (Scherer 1990; Lehmann, Assouline and Or 2008). That lasts until the top's pores empty, at the air-entry value Slowik, Schmidt and Fritzsch (2008) measured. Al-Fadhala and Hover (2001) saw the loss from cast concrete fall away from the free-water rate over hours, not minutes. So over a cycle of minutes the top loses at most W.

The largest doubt is in M3, the transfer coefficient: about a factor of 1.5 on E either way, and most of it is geometry. The model takes the top of the layer to lose water like the face below it. It takes one wet height for the whole wall, and air that moves along the wall at one speed. The top is a strip a few centimetres wide, and air that crosses the wall reaches it differently from air that runs along it. Published measurements are of horizontal surfaces or of faces under a fan, and nobody has measured the vapour's buoyancy at fresh mortar. Shah (2014, 2022), still-air evaporation from pools, is the coarse check on that corner: it catches a factor of two and nothing finer. The wet height is the setting you guess: across its range, 0.1 to 3 m, E moves by more than a factor of 3. The surface temperature is the input the model is steepest in: a top 3 °C under the air loses about a third less. A wet top in moving air runs cooler than the air.

The thresholds carry a different doubt. Keita measured the decade between them, a factor of 10. Where it sits on the W axis is not measured, because the conversion runs through the water per unit of exposed area in Keita's specimens. So both defaults are round numbers, and you can move both. Sanjayan et al. (2018) add a caution. In a mortar that bleeds, the bond did not fall steadily as the top stood open longer, because bleed water kept arriving. A printing mortar bleeds almost nothing, so the model assumes the fall is steady, and Vertico's calibration has to confirm it.

Note 05.1Method: what would place the thresholds

Four measurements, in the order of what they fix. First, weigh the water leaving the top of a printed layer against time in a chamber, with the air along the wall and then across. That tests W as an upper bound within a cycle and pins the wet height. Second, break the bond after a measured loss rather than a measured time, which places both thresholds for Vertico's mortar. Third, read the surface temperature by infrared in every run, so the coefficient does not absorb the cooling. Fourth, read the air movement with a hot-wire anemometer at printhead height, and log its direction. Until then the thresholds are provisional, and the tool says so where you set them.

Lengthen the cycle and the line moves left, toward the bond threshold, and a shorter cycle brings it back. The reading is one input to the decision to print. What follows it, the mix, the cover, the curing and the wait, is the engineer's call.

Sources

Every number on this page comes from one of these sources or from the model at the worked example. Several figures are quoted as reported, and the originals are listed so that you can check each one.

  • Keita, E., Bessaies-Bey, H., Zuo, W., Belin, P. and Roussel, N. (2019). Weak bond strength between successive layers in extrusion-based additive manufacturing: measurement and physical origin. Cement and Concrete Research 123: 105787. The two points that place both thresholds, and the dry skin behind them.
  • Sanjayan, J. G., Nematollahi, B., Xia, M. and Marchment, T. (2018). Effect of surface moisture on inter-layer strength of 3D printed concrete. Construction and Building Materials 172: 468-475. Bond follows the moisture on the surface the next layer meets, and does not fall steadily where the mortar bleeds.
  • ACI 305R, Guide to Hot Weather Concreting. American Concrete Institute. The rate this model is compared with, and the tool beside this one.
  • Menzel, C. A. (1954). Causes and prevention of crack development in plastic concrete. Portland Cement Association. The equation behind the ACI 305 nomograph.
  • Uno, P. J. (1998). Plastic shrinkage cracking and evaporation formulas. ACI Materials Journal 95(4): 365-375. The closed form of that equation, and what it was fitted to.
  • ACI 308R-23, Guide to Curing Concrete. American Concrete Institute. The ACI rate is evaporativity, the rate from free water, and it stands for the concrete's loss only under bleed water.
  • Buck, A. L. (1981). New equations for computing vapor pressure and enhancement factor. Journal of Applied Meteorology 20: 1527-1532. How much vapour saturated air holds at each temperature, in this model.
  • Churchill, S. W. and Chu, H. H. S. (1975). Correlating equations for laminar and turbulent free convection from a vertical plate. International Journal of Heat and Mass Transfer 18: 1323-1329. The air the face moves itself.
  • Churchill, S. W. (1977). A comprehensive correlating equation for laminar, assisting, forced and free convection. AIChE Journal 23(1): 10-16. The cube rule that joins the face's air and the hall's.
  • Scherer, G. W. (1990). Theory of drying. Journal of the American Ceramic Society 73(1): 3-14. Capillary flow keeps a drying surface wet.
  • Lehmann, P., Assouline, S. and Or, D. (2008). Characteristic lengths affecting evaporative drying of porous media. Physical Review E 77: 056309. How long a porous body can feed its surface.
  • Slowik, V., Schmidt, M. and Fritzsch, R. (2008). Capillary pressure in fresh cement-based materials and identification of the air entry value. Cement and Concrete Composites 30(7): 557-565. The air-entry value: the pressure at which the surface pores empty.
  • Al-Fadhala, M. and Hover, K. C. (2001). Rapid evaporation from freshly cast concrete and the Gulf environment. Construction and Building Materials 15(1): 1-7. The loss from cast concrete falls away from the free-water rate over hours.
  • Shah, M. M. (2014). Methods for calculation of evaporation from swimming pools and other water surfaces. ASHRAE Transactions. And (2022), Science and Technology for the Built Environment. Still-air evaporation from pools, the coarse check on the still-air corner of this model.
  • ASHRAE Standard 55. The convention that air below 0.1 m/s is still.