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Green Building Bible, Fourth Edition
Green Building Bible, fourth edition (both books)
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    •  
      CommentAuthorfostertom
    • CommentTimeNov 10th 2015
     
    Does anyone know in plain language the theoretical basis of the P/A floor reistance method in EN 13370? Can anyone slip me a copy?

    What does it assume about the isotherm-shape of temp distribution at depth below GL, with seasonal variation, in the subsoil - both under surrounding varying-temp surface of surrounding open ground, and under the constant-temp floor surface of heated building?

    There are 2 components to heat loss through floors - the perimeter heat loss and the straight-down heat loss. P/A ratio seems a good basis for calculating the perimeter heat from around the edge of the slab, going down, curving outward and back up to the cold surrounding ground surface. But seems unhelpful in calculating the straight-down heat loss, which should depend straightforwardly on A alone.

    The perimeter heat loss is proportional to delta-t - the temp difference between inside and out.
    But what is the temp difference to apply to the straight-down heat loss? What is the temp, and at what depth in the subsoil, that heat is being lost straight-down to?
    • CommentAuthortony
    • CommentTimeNov 10th 2015
     
    How long has the house in question been there days, weeks, months or years?
    • CommentAuthorbxman
    • CommentTimeNov 10th 2015 edited
     
    No expert but not very much I almost certain

    have a look at this

    https://www.youtube.com/watch?v=Jxd6eCmbuW8

    not certain he is an expert either but I am sure has more knowledge than me .
    •  
      CommentAuthorfostertom
    • CommentTimeNov 10th 2015
     
    The great teacher Bill, father of Permaculture! Not sure if I can sit still for 1.5hrs tho!

    Tony, extg house 1920s cavity wall semi detached cottage, uninsulated solid slab on clay, extension not built yet. Why do you ask?
    • CommentAuthortony
    • CommentTimeNov 10th 2015
     
    The ground under a house will warm up to the average temperature of the house, this can take several years and will follow a seasonal temperature sine wave offset by some weeks or months depending on the insulation levels of the house.

    A point under the middle of the slab will loose very little heat as the escape path is the longest, points on the perimeter will loose the most, similar to walls but likely more as any insulation tends to stop too high up.

    The p/a is a rough and ready method of determining how little insulation to put under a floor, not for us that. We used to put more under the edges and led under the middle, not so easy as it sounds but more effective use of materials. For very large slabs (commercial) no insulation is needed under the middle the ground has sufficient thermal resistance and ir warms up too.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 11th 2015
     
    I agree on those general principles tony - there's something of that in the P/A method and I'd like to know how they implimented those principles - whether the formula is just theoretically derived, if so, making what assumptions - or based emprically on field measurements - etc.

    If I'm working out how to use Therm to get more realistic results, then at least, to convince Building Inspectors, I have to be able to reproduce the P/A result in Therm by inputting the P/A method's assumptions - and go on from there.
    • CommentAuthorTimber
    • CommentTimeNov 11th 2015
     
    I use the PA method a fair amount when calculating floor U-Values but I must confess that I use a bit of software to do it and so don't fully understand the maths behind it. I have a copy of that standard you mention so I can check and see if it actually gives a formula.

    I also have an excel spreadsheet that I got on the AECB therm course many years ago which allows you to calc the PSI value of a solid ground floor to wall junction based on the PA calc.

    I know that definitely makes all sorts of assumptions that may or may not accurately reflect the real building - those may be same as the official U-Value software I use for floors. If I get a spare minute this week I will have a look into it.
    •  
      CommentAuthordjh
    • CommentTimeNov 11th 2015
     
    Posted By: fostertomthe P/A floor reistance method in EN 13370

    Just for pedants, I think you mean ISO 13370. (or EN ISO 13370:2007 with 2009 addendum to give it a more impressive moniker). BS EN 13370 is about waste!
  1.  
    Here's an old NRCan paper on basement heatloss with real-world measurements and calculation: http://web.mit.edu/parmstr/Public/NRCan/nrcc23378.pdf

    Here's a useful list of tools for building simulation too: https://www.canadianarchitect.com/asf/enclosure_design_tools/digital_tools/digital_tools.htm

    NRCan used to provide "Basecalc" as a tool for basement heatloss modelling - it's not available separately anymore but is built into hot2000

    Paul in Montreal.
    • CommentAuthormike7
    • CommentTimeNov 11th 2015 edited
     
    Posted By: fostertomThe perimeter heat loss is proportional to delta-t - the temp difference between inside and out.
    But what is the temp difference to apply to the straight-down heat loss? What is the temp, and at what depth in the subsoil, that heat is being lost straight-down to?


    I found - and lost - a site that compared various tools for these calculations and IIRC they mostly assumed a constant temp of 10C at 15m. I suspect you will be itching to find the difference between this and a really deep boundary! I think the answer will depend a lot on the slab size - I saw one case where they calculated for a 40m slab, and so of course most of the central area loss went pretty straight down to the 'deep' boundary. My simulations are with an 8m slab with a deep boundary at 10m depth, so I get more spreading of the heat flow lines close to the centre, and then the lines further out curve round even more to terminate either at the far vertical boundary or curve on up to the ground like the perimeter ones, only further out.

    With an effectively infinitely deep boundary only the centre flux line will go on down indefinitely. Eventually all other flux lines will curve round and -if there's also an infinite far vertical boundary - they will all eventually curve up to the ground. Although their path lengths will be very long this does not mean the heat loss will be reduced proportionate to their length. This is because the divergence of the flux lines entails a reduction of the temperature gradient. Thus the far reaches of the path length have a very small temperature drop along them, meaning a bigger temperature drop along the flux lines close to the slab than you might be expecting. I have a tendency to explain things in a way that only people who already understand can understand, and if that's the case here let me know and I'll try to clarify.

    Re the delta-t thing - a good point, and it seems clear to me that talk of a u-value for the centre floor area, to be bundled in with u-values and areas for other building components is not sensible. I think the best approximation, if one is making the initial rough approximation of a perimeter area and a centre area being distinctly different, would be to use the deep ground or year average ambient temp for the centre area, and add the resulting constant year-round rate of heat loss to the other more seasonally/daily variable losses/gains for the building.
    • CommentAuthorEd Davies
    • CommentTimeNov 11th 2015
     
    For any who've not heard the obvious caveat before: water. Specifically, the highest water table for the year.
    • CommentAuthorringi
    • CommentTimeNov 11th 2015
     
    Remember you are also trying to stop condensation on the floor in summer.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Thanks Timber
    Posted By: TimberI have a copy of that standard you mention so I can check and see if it actually gives a formula.
    The end-result formula itself is readily available - U = 0.05 + 1.65P/A - 0.6(P/A)^2
    Posted By: TimberI also have an excel spreadsheet that I got on the AECB therm course many years ago which allows you to calc the PSI value of a solid ground floor to wall junction based on the PA calc.

    I know that definitely makes all sorts of assumptions that may or may not accurately reflect the real building - those may be same as the official U-Value software I use for floors.
    That'll be the one(s) in http://www.peterwarm.co.uk/?dl_id=2 ? I agree with yr 2nd para comment.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Thanks gents for splendid responses - you never (well, rarely) fail.

    Any more?
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Thanks Paul, esp for http://web.mit.edu/parmstr/Public/NRCan/nrcc23378.pdf .

    I guess the basement model (fig 1) is valid to use for slab-on-grade (N Am parlance) by setting certain terms to zero or as appropriate?

    It depends on
    'lower thermal boundary at a constant temperature equal to the mean ground temperature'
    and
    'assumes that there is sufficient groundwater flow to maintain a constant temperature at some depth below the basement floor'.
    What do we think of the latter - a bit odd?

    Posted By: Ed DaviesFor any who've not heard the obvious caveat before: water. Specifically, the highest water table for the year.
    I've been thinking about that, and wonder whether it's an exagerated threat.
    http://www.homeintheearth.com/tech_notes/basics-of-earthsheltering/earth/soil-properties/soil-temperature-experiment
    shows negligible difference in ground temps at depth, whether surface-sheltered from rain or not. As he says:
    'Note: this result is significant because it contradicts the theory found in many earth sheltered umbrella books!'

    Not about ground water, I know, but ... Actually it's not just vertical rise and fall of water table that could carry stored heat away, but also horizontal flow of underground water. How to guess what's happening with water in the subsoil beneath your site? Maybe it's not so critical.

    First, precipitration - rain and snow-melt percolating down through open ground surrounding the building, which is important because surrounding surface and subsoil temps are what drives the major edge-loss from a slab, esp a high-P/A domestic-size slab as opposed to a low-P/A warehouse-size slab.

    First, snow is an excellent insulator, till it melts.
    Next, what is the mean temp of rainwater, over the heating season? Above 0C, by definition, and I suspect considerably higher.
    Then, what is the rainwater's thermal capacity, totalled over the heating season? How many inches of water? A fraction of the vertical height of the subsoil block that we're interested in. Even allowing that water has 5(?)x the volumetric specific heat of subsoil, by how much will percolating rainfall actually cool the subsoil?

    Once water is deep in the subsoil, the stuff of underground horizontal flow and water table vertical movement, why should its temp be any different from the soil it's in? The deeper its source and the longer in the ground, the warmer it should be - it's horribly hot down a mine!
    • CommentAuthorringi
    • CommentTimeNov 12th 2015
     
    If you have UFH this all changes as the floor is then warmer then the air in the building.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Well, getting the U-value right becomes critically important - but doesn't change anything in principle?

    Posted By: ringiRemember you are also trying to stop condensation on the floor in summer.
    Say more?
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015 edited
     
    Here's a fantastic resource
    https://www.pik-potsdam.de/services/climate-weather-potsdam/climate-diagrams/ground-temperature
    Anyone know of similar closer to home? I must go see what ST's favourite Plymouth data has to offer.

    At Potsdam, the 12m deep temp seems not all that stable - in fact the 4m deep one seems most constant.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015 edited
     
    From
    http://www.greenbuildingforum.co.uk/newforum/comments.php?DiscussionID=11674&page=1#Comment_231973
    (and elsewhere)
    Posted By: fostertomunder open ground at depth of 1.5 to 3m (varies depending on local subsoil density (or rather, volumetric thermal capacity) and conductivity), the steady year-round temp will equilibriate at the annual average air temp above
    That, I realise, is wrong - more like 10-12m deep. At 1-2m, it's diurnal fluctuations that disappear
    https://www.pik-potsdam.de/services/climate-weather-potsdam/climate-diagrams/ground-temperature
    Sorry to have propagated that, better late than never, hope it's not misled anyone.
    • CommentAuthormike7
    • CommentTimeNov 12th 2015
     
    Posted By: fostertomThe end-result formula itself is readily available - U = 0.05 + 1.65P/A - 0.6(P/A)^2


    Shome mishtake shurley? The units don't work, and where is the ground conductivity?
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Just empirical curve-fitting?
    • CommentAuthorEd Davies
    • CommentTimeNov 12th 2015
     
    Posted By: fostertomI've been thinking about that, and wonder whether it's an exagerated threat.
    http://www.homeintheearth.com/tech_notes/basics-of-earthsheltering/earth/soil-properties/soil-temperature-experiment
    Interesting link, thanks. Rest of the site looks worth a read, too - bookmarked.

    But that's still with the water table deep down and just precipitation soaking through the ground. What about the cases where the water table is close to, at or even above ground levels?

    Actually it's not just vertical rise and fall of water table that could carry stored heat away, but also horizontal flow of underground water.
    Absolutely - that's mostly what I'd worry about.

    How to guess what's happening with water in the subsoil beneath your site?
    Well, if it pisses out of the ground on the downhill side of your house and runs across the road that's a bit of a hint. :wink:

    OK, northern part of Scotland tends to be a bit of an extreme case but, for example, lots of Norfolk and Lincolnshire would be similar with more-or-less continuous water a metre or so down with a steady horizontal flow towards the nearest drainage ditch.
      dsc00076-small.jpg
    • CommentAuthorEd Davies
    • CommentTimeNov 12th 2015
     
    Posted By: mike7Shome mishtake shurley? The units don't work, and where is the ground conductivity?
    I think you have to pretend that the constants have units appropriate to conversion of 1/m or 1/m² to W/m²·K. If you measure P in feet and A in square feet then you have to use different constants. If you measure P in metres and A in square feet you're on your own.
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015 edited
     
    Sure, all of that Ed. But what about
    Posted By: fostertomwhat is the rainwater's thermal capacity, totalled over the heating season? How many inches of water? A fraction of the vertical height of the subsoil block that we're interested in. Even allowing that water has 5(?)x the volumetric specific heat of subsoil, by how much will percolating rainfall actually cool the subsoil?
    If rainwater's not that cold, and doesdn't cool the ground that much, then what makes it supposedly colder than the ground it's in, once it's joined the water table and/or is flowing horizontally underground?
    Posted By: fostertomOnce water is deep in the subsoil, the stuff of underground horizontal flow and water table vertical movement, why should its temp be any different from the soil it's in? The deeper its source and the longer in the ground, the warmer it should be - it's horribly hot down a mine!
    • CommentAuthormike7
    • CommentTimeNov 12th 2015
     
    Posted By: Ed Davies
    Posted By: mike7Shome mishtake shurley? The units don't work, and where is the ground conductivity?
    I think you have to pretend that the constants have units appropriate to conversion of 1/m or 1/m² to W/m²·K. If you measure P in feet and A in square feet then you have to use different constants. If you measure P in metres and A in square feet you're on your own.

    I can see that makes sense re. the metres, but the constant adjustment to sort out the watts bit would need to be ..er .. the conductivity. Otherwise it would be a formula only for a conductivity of 1W/mK - woodnit?
    •  
      CommentAuthorfostertom
    • CommentTimeNov 12th 2015
     
    Posted By: mike7a conductivity of 1W/mK
    Not so far off correct.
    •  
      CommentAuthorSteamyTea
    • CommentTimeNov 12th 2015 edited
     
    I would think that rain water is pretty close to the air temperature. You can see this affect when comparing sea surface temperature to near shore temperature (don't tell the surfers as they will pretend to be even harder in the winter).
    I feel a data collecting project coming on.

    If rainwater is close to air temperature at the time of rainfall, then ground temperature will affect temperature once it starts to percolate.

    What Plymouth data is that then?
    •  
      CommentAuthordjh
    • CommentTimeNov 12th 2015 edited
     
    Posted By: fostertomOnce water is deep in the subsoil, the stuff of underground horizontal flow and water table vertical movement, why should its temp be any different from the soil it's in? The deeper its source and the longer in the ground, the warmer it should be - it's horribly hot down a mine!

    The point is that it's the same temperature as the soil that's not underneath your building, so if it's only 1 m under your building then all you've got between the bottom of your floor and 4°C is a metre of damp earth in winter. You don't get any heating of the earth under your building; it's a thermal short-circuit.
    • CommentAuthorEd Davies
    • CommentTimeNov 12th 2015
     
    Posted By: mike7but the constant adjustment to sort out the watts bit would need to be ..er .. the conductivity. Otherwise it would be a formula only for a conductivity of 1W/mK - woodnit?
    Aren't they just assuming the conductivity of the ground, which might be 1 W/mK or might be something else; it's buried in with all the other assumptions leading to those magic numbers?
   
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