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008190117s2003    onc    #ot   f|0| 0 eng d
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn---
0861 |aEn13-5/03-180E-PDF
24500|aGeochemical stability of phosphorus solids below septic system infiltration beds |h[electronic resource] / |cM. A. Zurawsky ... [et al.].
260 |a[Burlington, Ont.] : |bEnvironment Canada, |c[2003]
300 |a[28] p. : |bfigures.
4901 |aNWRI contribution ; |vno. 03-180
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
504 |aIncludes bibliographic references.
520 |a"In a recent review of 10 mature septic system plumes, it was recognized that precipitation of phosphorus (P) commonly occurred in close proximity to the infiltration pipes, resulting in discrete narrow intervals enriched in P by a factor of 2-4 (Robertson et al., 1998; Zanini et al., 1998). Although these attenuation reactions appeared to be sustainable, questions have arisen regarding the potential for remobilization of this P mass, should geochemical conditions change"--Abstract.
546 |aAbstracts in French and English.
69207|2gccst|aGeochemistry
69207|2gccst|aSediments
7001 |aZurawsky, M. A.
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada)
830#0|aNWRI contribution ;|vno. 03-180.|w(CaOODSP)9.844121
85640|qPDF|s1.25 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/En13-5-03-180-eng.pdf