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Record #88902:
- #88902
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MARC recordThe comparative fluxes of strong-acid anions in melting snowpacks and surface waters during spring melt in a boreal forest / Yves Bédard, H.G. Jones.
| Title: | The comparative fluxes of strong-acid anions in melting snowpacks and surface waters during spring melt in a boreal forest / Yves Bédard, H.G. Jones. |
| Author(s): | Bédard, Yves. Jones, H. G. |
| Date: | 1987. |
| In: | Eastern Snow Conference. Proceedings. (1987.), Vol. 43rd [1986] Annual Meeting (1987) |
| Abstract: | As first step in study of acid pulse in Lac Laflamme watershed, Quebec, during snowmelt, contribution was determined of total strong-acid anion load, which had accumulated in snowpack during winter before beginning of spring melt and from rain-on-snow events during melt period, to strong-acid anion flux in surface runoff. Difference between measured loads in snowpack (plus precipitation) and in surface waters was then used to determine extent to which soil-subsurface water system acts as sink or reservoir of strong-acid anions during spring melt period. |
| Notes: | Eastern Snow Conference. Proceedings. Vol. 43rd [1986] Annual Meeting :45-54 (1987). |
| Keywords: | 551.579.2 -- Water supply from snow. 551.578.46 -- Snow cover and snow patches. 54 -- Chemistry. 551.578.462 -- Snow cover, ablation. E11 -- Glaciology: glaciohydrology. (*41) -- Canada. (*424) -- Quebec. |
| SPRI record no.: | 88902 |
LDR 01592naa#a2200000#a#4500 001 SPRI-88902 005 20230327175541.0 007 ta 008 230327s1987####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-88902 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBédard, Yves. 245 14 ‡aThe comparative fluxes of strong-acid anions in melting snowpacks and surface waters during spring melt in a boreal forest /‡cYves Bédard, H.G. Jones. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 45-54 :‡bdiags., tables, map. 500 ## ‡aEastern Snow Conference. Proceedings. Vol. 43rd [1986] Annual Meeting :45-54 (1987). 520 3# ‡aAs first step in study of acid pulse in Lac Laflamme watershed, Quebec, during snowmelt, contribution was determined of total strong-acid anion load, which had accumulated in snowpack during winter before beginning of spring melt and from rain-on-snow events during melt period, to strong-acid anion flux in surface runoff. Difference between measured loads in snowpack (plus precipitation) and in surface waters was then used to determine extent to which soil-subsurface water system acts as sink or reservoir of strong-acid anions during spring melt period. 650 07 ‡a551.579.2 -- Water supply from snow.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a54 -- Chemistry.‡2udc 650 07 ‡a551.578.462 -- Snow cover, ablation.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*424) -- Quebec.‡2udc 700 1# ‡aJones, H. G. 773 0# ‡7nnas ‡tEastern Snow Conference. Proceedings. ‡gVol. 43rd [1986] Annual Meeting (1987) ‡wSPRI-23848 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230327