A Laboratory Study on the Role of Stream Sediment in Nitrogen Loss from Water

1977 ◽  
Vol 6 (3) ◽  
pp. 274-278 ◽  
Author(s):  
Pritam Sain ◽  
J. B. Robinson ◽  
W. N. Stammers ◽  
N. K. Kaushik ◽  
H. R. Whiteley
1998 ◽  
Vol 145 (1) ◽  
pp. 39-44 ◽  
Author(s):  
T. Falk ◽  
J.‐E. Svensson ◽  
L.‐G. Johansson

1985 ◽  
Vol 60 (4) ◽  
pp. 673-677 ◽  
Author(s):  
HAROLD E. CARLSON ◽  
HARRIS L. WASSER ◽  
ROGER D. REIDELBERGER

Diabetes ◽  
1959 ◽  
Vol 8 (1) ◽  
pp. 57-62 ◽  
Author(s):  
O. H. Gaebler ◽  
R. Glovinsky ◽  
T. Vitti ◽  
T. G. Maskaleris
Keyword(s):  

Soil Science ◽  
1974 ◽  
Vol 118 (2) ◽  
pp. 78-81 ◽  
Author(s):  
W. H. PATRICK ◽  
S. GOTOH
Keyword(s):  

2004 ◽  
Author(s):  
J.E. Altoe F. ◽  
P. Bedrikovetsky ◽  
A.G. Siqueira ◽  
A.L. Souza ◽  
F.S. Shecaira
Keyword(s):  

2010 ◽  
Vol 457 ◽  
pp. 52-57 ◽  
Author(s):  
Iker Asenjo ◽  
Jacques Lacaze ◽  
Peio Larrañaga ◽  
Susana Méndez ◽  
Jon Sertucha ◽  
...  

Parameters that affect chunky graphite formation in heavy-section castings have been studied in previous works which showed that inoculation and cerium addition both increase the tendency for this degenerate graphite. This suggested that laboratory study on chunky graphite formation could be performed on small castings by over-treating the melt. Though the role of silicon was not ascertained, it appeared of potential interest to also investigate its effect in relation with the carbon equivalent of the iron and the nucleation potential of the melt. Keel-blocks were thus cast using Ce or Ce-Mg treated melts, with increased silicon content (up to 4.0 wt.%) and inoculation rate as compared to usual practice. It was observed that chunky graphite systematically appeared in more or less extended areas centred on the upper part of the keel-blocks. The as-cast microstructure (graphite shape and distribution) has then been studied in relation to melt composition and additions (Ce treatment and inoculation) in both affected and non-affected areas. Finally, microanalysis of oxides and other minor phases showed them to be similar to those appearing in heavy-section castings. It may then be concluded that chunky graphite appears in light-section castings in the same way than in heavy-section castings when using over-treated melts.


1975 ◽  
Vol 10 (1) ◽  
pp. 110-117 ◽  
Author(s):  
N.K. Kaushik ◽  
J.B. Robinson ◽  
P. Sain ◽  
H.R. Whiteley ◽  
W. Stammers

Abstract With a view to determining nitrogen sink processes, if any, in streams and the factors that govern these processes, nitrogen transport was studied in a 2 km-long, perennial, spring-fed stream during the summer months of 1973 and 1974. Concentrations of ammonium, nitrite and Kjeldahl nitrogen were small but those of nitrate nitrogen were unusually high. However, as the water moved downstream it progressively lost nitrate N. This loss represented 59.4% and 46.7% of the respective inputs during 1973 and 1974. The decrease in the concentration of nitrate N could neither be attributed to dilution nor to nitrogen immobilization during decomposition of organic matter nor to the uptake by aquatic macrophytes. Laboratory experiment showed that the stream sediments have significant, capacity for denitrification of nitrate in water overlying them, even when the water is thoroughly oxygenated. Although the role of riparian plants in the uptake of nitrogen has not been fully elucidated, it seems that denitrification in the stream sediment may act as an important permanent nitrogen sink.


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