| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.873013 |
| 003 | CaOODSP |
| 005 | 20241203113648 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 190515s1988 oncd #ot f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 041 | |aeng|bfre |
| 043 | |an-cn--- |
| 086 | 1 |aEn13-5/88-88E-PDF |
| 100 | 1 |aJerome, John H. |q(John Harvey)|eauthor. |
| 245 | 10|aDetermination of scalar irradiation available for photolysis in natural waters / |cby J.H. Jerome, R.P. Bukata and J.E. Bruton. |
| 264 | 1|aBurlington, Ontario : |bNational Water Research Institute, |c1988. |
| 300 | |a1 online resource (25 pages) : |bcharts. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aNWRI contribution ;|vno. 88-88 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 500 | |a"May 1988." |
| 504 | |aIncludes bibliographical references. |
| 520 | |a"Multiplicative factors are derived which enable the conversion of incident radiation (either above or below the air/water interface) into the subsurface daily scalar irradiation available for photolysis. These multiplicative factors are presented as functions of the volume reflectance of the water and illustrate that for volume reflectances in the range 0.0 to 0.14, the actual subsurface daily scalar irradiation available for photochemical and photobiological reactions varies between 1.1 and 2.1 times that value of subsurface daily irradiation generally considered available for such reactions"--Abstract. |
| 546 | |aIncludes abstract in French. |
| 692 | 07|2gccst|aWater management |
| 700 | 1 |aBukata, R. P., |eauthor. |
| 700 | 1 |aBruton, J. E., |eauthor. |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 2 |aNational Water Research Institute (Canada). |bRivers Research Branch. |
| 830 | #0|aNWRI contribution ;|vno. 88-88.|w(CaOODSP)9.844121 |
| 856 | 40|qPDF|s1.59 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-88-88-eng.pdf |