| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.870078 |
| 003 | CaOODSP |
| 005 | 20221107163025 |
| 006 | m o d f |
| 007 | cr nn||||||||| |
| 008 | 190318t19721973onca obt f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 041 | |aeng|bfre |
| 043 | |an-cn--- |
| 086 | 1 |aM38-1/254-1972E-PDF|zM38-1/254 |
| 100 | 1 |aWhaley, H. |
| 245 | 14|aThe derivation of plume dispersion parameters from measured three-dimensional data / |cH. Whaley, Canadian Combustion Research Laboratory, Fuels Research Centre. |
| 264 | 1|aOttawa : |bDepartment of Energy, Mines and Resources, Mines Branch, |cNovember 1972. |
| 264 | 4|c©1973 |
| 300 | |a1 online resource (v, 14, [5] pages) : |bfigures. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aResearch report ; |vR 254 |
| 500 | |aCover title. |
| 500 | |aDigitized edition from print [produced by Natural Resources Canada]. |
| 500 | |a"November 1972." |
| 504 | |aIncludes bibliographical references (pages 12-13). |
| 520 | 3 |a"It is well known that atmospheric diffusion models, however sophisticated and rigorous they may be mathematically, can only be as accurate as the input data used for model calibration and verification. In this paper, the method of finite differences is used to determine both the plume rise and the standard deviations of plume spread from three-dimensional data acquired by aerial probing. Comparisons are also made with corresponding values estimated by accepted empirical methods"--Abstract, page i. |
| 546 | |aIncludes abstract in French. |
| 693 | 4|aAtmospheric diffusion |
| 710 | 1 |aCanada. |bDepartment of Energy, Mines and Resources. |
| 710 | 1 |aCanada. |bMines Branch. |
| 710 | 2 |aFuels Research Centre (Canada) |
| 830 | #0|aResearch report (Canada. Mines Branch)|vR 254.|w(CaOODSP)9.855660 |
| 856 | 40|qPDF|s1.41 MB|uhttps://publications.gc.ca/collections/collection_2019/rncan-nrcan/m38-1/M38-1-254-1972-eng.pdf |