Difference between revisions of "OPSS aggregates"
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Of the standard granular materials in the standard OPSS.MUNI 1010 only '''Granular O''' is recommended as a substitute for [[reservoir aggregate| clear stone]]. | [[File:Aggregates Highway 7.jpg|thumb|The fines can clearly be seen on these piles of standard OPSS aggregates for road reconstruction]] | ||
{{Textbox|1= Where Granular O is substituted for clear stone in underground reservoir structures, the | <onlyinclude>Of the standard granular materials in the standard [http://www.raqsb.mto.gov.on.ca/techpubs/ops.nsf/0/0b9aa4d966cac4f9852580820062909e/$FILE/OPSS.MUNI%201010%20Nov%2013.pdf OPSS.MUNI 1010] only '''Granular O''' is recommended as a substitute for [[reservoir aggregate| clear stone]] in LID construction. | ||
Examples of BMPs with underground reservoirs include [[Underdrains]], [[infiltration trenches]], [[permeable | {{Textbox|1= Where Granular O is substituted for clear stone in underground reservoir structures, the porosity used in design calculations shall be '''0.3''' unless laboratory testing proves otherwise.}} | ||
Examples of BMPs with underground reservoirs include [[Underdrains]], [[infiltration trenches]], [[permeable pavements]], [[infiltration chambers]], [[exfiltration trenches]]. | |||
All other mixes must be avoided for free drainage or storage as they are permitted to contain a higher enough proportion of fines to reduce permeability below 50 mm/hr. | |||
</onlyinclude> | |||
===Justification=== | |||
{| class="wikitable" | {| class="wikitable" | ||
Line 40: | Line 43: | ||
| 0.15 || || 15 || || || || || || || || || || || 2 || 65 | | 0.15 || || 15 || || || || || || || || || || || 2 || 65 | ||
|- | |- | ||
| 0.075 || 2 || 8 || 0 || 8 || 0 || 10 || 0 || 8 || 2 || 8 || 0 || 5 || 0 || 25 | | 0.075 || 2 || 8 || 0 || 8 || 0 || 10 || 0 || 8 || 2 || 8 || 0 || 5 || 0 ||style='color: red'|25 | ||
|- | |- | ||
| d<sub>60</sub> || 13 || 6 || 35 || 0.25 || 25 || 6 || 40 || 1.2 || 10 || 5 || 15 || 7 || 35 || 0.15 | | d<sub>60</sub> || 13 || 6 || 35 || 0.25 || 25 || 6 || 40 || 1.2 || 10 || 5 || 15 || 7 || 35 || 0.15 | ||
|- | |- | ||
| d<sub>10</sub> || 0.7 || 0.1 || 1 || 0.08 || 1.2 || 0.075 || 1.2 || 0.085 || 0.6 || 0.09 || 2.5 || 0.3 || 1.2 || | | d<sub>10</sub> || 0.7 || 0.1 || 1 || 0.08 || 1.2 || 0.075 || 1.2 || 0.085 || 0.6 || 0.09 || 2.5 || 0.3 || 1.2 ||style='color: red'|NaN | ||
|- | |- | ||
| Content Uniformity || 19 || 60 || 35 || 3 || 21 || 80 || 33 || 14 || 17 || 56 || 6 || 23 || 29 || | | Content Uniformity || 19 || 60 || 35 || 3 || 21 || 80 || 33 || 14 || 17 || 56 || 6 || 23 || 29 || | ||
|- | |- | ||
| | | Porosity (Vukovic) || 0.26 || 0.26 || 0.26 || 0.40 || 0.26 || 0.26 || 0.26 || 0.27 || 0.27 || 0.26 || 0.34 || 0.26 || 0.26 || | ||
|- | |- | ||
! Mean | ! Mean porosity (Vukovic) | ||
!colspan = "2" align = center| 0.26 | !colspan = "2" align = center| 0.26 | ||
!colspan = "2" align = center| 0.33 | !colspan = "2" align = center| 0.33 | ||
Line 59: | Line 62: | ||
!colspan = "2" align = center| 0.26 | !colspan = "2" align = center| 0.26 | ||
|- | |- | ||
| K<sub>(Hazen)</sub>(mm/hr) || 1764 || 36 || 3600 || 23 | | K<sub>(Hazen)</sub>(mm/hr) || 1764 ||style='color: red'|36 || 3600 ||style='color: red'|23 || 5184 ||style='color: red'|20 || 5184 ||style='color: red'|26|| 1296 ||style='color: red'|29|| 22500 || 324 || 5184 ||style='color: red'|NaN | ||
|- | |- | ||
! Mean K<sub>(hazen)</sub>(mm/hr) | ! Mean K<sub>(hazen)</sub>(mm/hr) | ||
Line 68: | Line 71: | ||
!colspan = "2" align = center| 663 | !colspan = "2" align = center| 663 | ||
!colspan = "2" align = center| 11412 | !colspan = "2" align = center| 11412 | ||
!colspan = "2" align = center| | !colspan = "2" align = center style='color: red'|NaN | ||
|} | |} | ||
Porosity values were calculated based on the coefficient of uniformity (''C<sub>U</sub>'')<ref>Vuković, Milan and Soro, Andjelko Determination of hydraulic conductivity of porous media from grain-size composition. Water Resources Publications, Littleton, Colo, 1992.</ref><ref>Odong, J. (2007). Evaluation of Empirical Formulae for Determination of Hydraulic Conductivity based on Grain-Size Analysis. Journal of American Science, 3(3). Retrieved from http://www.jofamericanscience.org/journals/am-sci/0303/10-0284-Odong-Evaluation-am.pdf</ref><ref>Zhang, S. (2017). Relationship between Particle Size Distribution and Porosity in Dump Leaching. the University of British Columbia. Retrieved from https://open.library.ubc.ca/collections/ubctheses/24/items/1.0357233</ref>: | |||
<math> | <math>n=0.255\left ( 1+0.83^{C_{U}} \right )</math> | ||
Where coefficient of uniformity is the ratio of the 60th and 10th percentile grain sizes: | Where coefficient of uniformity is the ratio of the 60th and 10th percentile grain sizes: | ||
<math>C_U=\frac{d_{60}}{d_{10}}</math> | <math>C_U=\frac{d_{60}}{d_{10}}</math> | ||
Line 78: | Line 81: | ||
Permeability (''K'') was estimated from the 10th percentile grain size using the [[Hazen]] formula. | Permeability (''K'') was estimated from the 10th percentile grain size using the [[Hazen]] formula. | ||
---- | ---- | ||
[[Category: Materials]] |
Latest revision as of 18:36, 6 August 2020
Of the standard granular materials in the standard OPSS.MUNI 1010 only Granular O is recommended as a substitute for clear stone in LID construction.
Where Granular O is substituted for clear stone in underground reservoir structures, the porosity used in design calculations shall be 0.3 unless laboratory testing proves otherwise.
Examples of BMPs with underground reservoirs include Underdrains, infiltration trenches, permeable pavements, infiltration chambers, exfiltration trenches.
All other mixes must be avoided for free drainage or storage as they are permitted to contain a higher enough proportion of fines to reduce permeability below 50 mm/hr.
Justification[edit]
Sieve size (mm) | A | B type I | B type II | B type III | M | O | SSM | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
High | Low | High | Low | High | Low | High | Low | High | Low | High | Low | High | Low | |
150 | 100 | 100 | 100 | 100 | 100 | 100 | ||||||||
106 | 100 | 100 | ||||||||||||
37.5 | 100 | 100 | ||||||||||||
26.5 | 100 | 100 | 50 | 100 | 50 | 100 | 50 | 100 | 95 | 100 | 50 | 100 | ||
19 | 85 | 100 | 100 | 100 | 80 | 95 | ||||||||
13.2 | 65 | 90 | 75 | 95 | 60 | 80 | ||||||||
9.5 | 50 | 73 | 32 | 100 | 55 | 80 | 50 | 70 | ||||||
4.75 | 35 | 55 | 20 | 100 | 20 | 55 | 20 | 90 | 35 | 55 | 20 | 45 | 20 | 100 |
1.18 | 15 | 40 | 10 | 100 | 10 | 40 | 10 | 60 | 15 | 40 | 0 | 15 | 10 | 100 |
0.3 | 5 | 22 | 2 | 65 | 5 | 22 | 2 | 35 | 5 | 22 | 5 | 95 | ||
0.15 | 15 | 2 | 65 | |||||||||||
0.075 | 2 | 8 | 0 | 8 | 0 | 10 | 0 | 8 | 2 | 8 | 0 | 5 | 0 | 25 |
d60 | 13 | 6 | 35 | 0.25 | 25 | 6 | 40 | 1.2 | 10 | 5 | 15 | 7 | 35 | 0.15 |
d10 | 0.7 | 0.1 | 1 | 0.08 | 1.2 | 0.075 | 1.2 | 0.085 | 0.6 | 0.09 | 2.5 | 0.3 | 1.2 | NaN |
Content Uniformity | 19 | 60 | 35 | 3 | 21 | 80 | 33 | 14 | 17 | 56 | 6 | 23 | 29 | |
Porosity (Vukovic) | 0.26 | 0.26 | 0.26 | 0.40 | 0.26 | 0.26 | 0.26 | 0.27 | 0.27 | 0.26 | 0.34 | 0.26 | 0.26 | |
Mean porosity (Vukovic) | 0.26 | 0.33 | 0.26 | 0.26 | 0.26 | 0.3 | 0.26 | |||||||
K(Hazen)(mm/hr) | 1764 | 36 | 3600 | 23 | 5184 | 20 | 5184 | 26 | 1296 | 29 | 22500 | 324 | 5184 | NaN |
Mean K(hazen)(mm/hr) | 900 | 1812 | 2602 | 2605 | 663 | 11412 | NaN |
Porosity values were calculated based on the coefficient of uniformity (CU)[2][3][4]: Where coefficient of uniformity is the ratio of the 60th and 10th percentile grain sizes:
Permeability (K) was estimated from the 10th percentile grain size using the Hazen formula.
- ↑ OPSS. (2013). Material Specficiation for Aggregates - Base, Subbase, Select Subgrade, and Backfill Material. Retrieved from http://www.raqsb.mto.gov.on.ca/techpubs/ops.nsf/0/0b9aa4d966cac4f9852580820062909e/$FILE/OPSS.MUNI%201010%20Nov%2013.pdf
- ↑ Vuković, Milan and Soro, Andjelko Determination of hydraulic conductivity of porous media from grain-size composition. Water Resources Publications, Littleton, Colo, 1992.
- ↑ Odong, J. (2007). Evaluation of Empirical Formulae for Determination of Hydraulic Conductivity based on Grain-Size Analysis. Journal of American Science, 3(3). Retrieved from http://www.jofamericanscience.org/journals/am-sci/0303/10-0284-Odong-Evaluation-am.pdf
- ↑ Zhang, S. (2017). Relationship between Particle Size Distribution and Porosity in Dump Leaching. the University of British Columbia. Retrieved from https://open.library.ubc.ca/collections/ubctheses/24/items/1.0357233