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Update general loads 3
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book/design_workflow/general_loads/Images/Emergency overflow.jpg
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book/design_workflow/general_loads/Images/Snow loading.jpg
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@ -4,9 +4,66 @@
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"cell_type": "markdown",
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"metadata": {},
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"source": [
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"# Variable loads 3: rain and snow\n",
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"# Variable loads 3: rain and snow"
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]
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},
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{
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"cell_type": "markdown",
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"metadata": {},
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"source": [
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"## Loading by rainwater\n",
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"Loads by rainwater are the result of accumulating water due to for example\n",
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"hogging of adjacent roof parts or clogging of the drainage systems.\n",
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"The most practical way of dealing with these actions is converting the snow\n",
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"load to a layer of water (e.g.: 0,56 kN/ m2 equals 56 mm water on the roof)\n",
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"and preventing the water from rising above this amount by designing for\n",
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"emergency overflow. Furthermore, always design a roof with a small pitch (general loads, general)\n",
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"\n",
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"\n"
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"```{figure} Images/Emergency overflow.jpg\n",
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"---\n",
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"scale: 100%\n",
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"---\n",
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"Emergency overflow by means of a so called \"mailbox\"\n",
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"```\n",
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"\n",
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"```{figure} Images/Emergency overflow 2.jpg\n",
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"---\n",
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"scale: 100%\n",
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"---\n",
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"```"
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]
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},
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{
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"cell_type": "markdown",
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"metadata": {},
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"source": [
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"## Snow loads\n",
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"Snow can cause considerable loads, as it doesn’t run off like rain. It is therefore important to check whether a load combination containing snow\n",
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"loads is leading. For different parts of Europe the value of the snow load can differ greatly (e.g.: compare the Mediterranean Coast to the Alps). In\n",
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"the Dutch National Annex of NEN-EN 1991-1-3 the complex calculations are substituted by one value for the whole country (sk = 0,7 kN/m2). For other areas NEN-EN 1991-1-3 must be consulted."
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]
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},
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{
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"cell_type": "markdown",
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"metadata": {},
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"source": [
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"## Determining the snow loading\n",
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"\n",
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"$s = μ_i · C_e · C_t · s_k$\n",
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" \n",
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"$s$ = Characteristic value of the snow load on the ground [$kN/m^2$] ($0,7 kN/m^2$ in\n",
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"the Netherlands) \n",
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"$μ_i$ = Shape coefficient, dependend on roof angle α \n",
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"$C_e$ = Exposure coefficient (1,0 for most cases) \n",
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"$C_t$ = Thermal coefficient (1,0 for most cases) \n",
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" \n",
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"The shape coefficient can be determined with the shown diagram. Note that μ2 is only applicable where snow accumulation can occur. For complex roof shapes and more information, see NEN-EN 1991-1-3.\n",
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"\n",
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"```{figure} Images/Snow loading.jpg\n",
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"---\n",
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"scale: 100%\n",
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"---\n",
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"```"
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]
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},
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{
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