scholarly journals Adsorption/Desorption Characteristics of Phosphate Ion onto Calcined Boehmite Surface

2005 ◽  
Vol 3 ◽  
pp. 63-69 ◽  
Author(s):  
Mineaki Kabayama ◽  
Naohito Kawasaki ◽  
Takeo Nakamura ◽  
Seiki Tanada
2003 ◽  
Vol 36 (4) ◽  
pp. 499-505 ◽  
Author(s):  
Mineaki Kabayama ◽  
Tohru Sakiyama ◽  
Naohito Kawasaki ◽  
Takeo Nakamura ◽  
Mamiko Araki ◽  
...  

1971 ◽  
Vol 68 ◽  
pp. 29-33 ◽  
Author(s):  
Bernard Weber ◽  
Albert Cassuto

1983 ◽  
Vol 139 (4) ◽  
pp. 736
Author(s):  
V.N. Ageev ◽  
E.Ya. Zandberg ◽  
N.I. Ionov ◽  
A.Ya. Tontegode

2015 ◽  
Vol 14 (1) ◽  
pp. 66-72 ◽  
Author(s):  
Seo-Hyun Pak ◽  
◽  
Myung-Seop Shin ◽  
Hyun-Jung Kim ◽  
Yong-Woo Jeon

2016 ◽  
Vol 10 (4s) ◽  
pp. 621-629
Author(s):  
Valentina Pidlisnyuk ◽  
◽  
John Harrington JR ◽  
Yulia Melnyk ◽  
Yuliya Vystavna ◽  
...  

The article focuses on examining the influence of fluctuations in annual precipitation amount on the quality of surface waters. Water quality was estimated with data on BOD, COD and phosphate–ion concentration within five selected regions of Ukraine. Analysis of the precipitation data (1991 – 2010) showed different regional trends. Using the statistics, determination of the interconnection between precipitation amount and water resources quality were done. The obtained regularities and associated uncertainties can be used for prediction of changes in water resource quality and as a guide for future adaptation to possible climate change.


2011 ◽  
Vol 26 (2) ◽  
pp. 149-154 ◽  
Author(s):  
Fei XIE ◽  
Yan Li WANG ◽  
Liang ZHAN ◽  
Ming GE ◽  
Xiao-Yi LIANG ◽  
...  

2003 ◽  
Vol 67 (3) ◽  
pp. 765 ◽  
Author(s):  
Jesper Gamst ◽  
Per Moldrup ◽  
Dennis E. Rolston ◽  
Torben Olesen ◽  
Kate Scow ◽  
...  

1992 ◽  
Vol 23 (1) ◽  
pp. 13-26 ◽  
Author(s):  
W. H. Hendershot ◽  
L. Mendes ◽  
H. Lalande ◽  
F. Courchesne ◽  
S. Savoie

In order to determine how water flowpath controls stream chemistry, we studied both soil and stream water during spring snowmelt, 1985. Soil solution concentrations of base cations were relatively constant over time indicating that cation exchange was controlling cation concentrations. Similarly SO4 adsorption-desorption or precipitation-dissolution reactions with the matrix were controlling its concentrations. On the other hand, NO3 appeared to be controlled by uptake by plants or microorganisms or by denitrification since their concentrations in the soil fell abruptly as snowmelt proceeded. Dissolved Al and pH varied vertically in the soil profile and their pattern in the stream indicated clearly the importance of water flowpath on stream chemistry. Although Al increased as pH decreased, the relationship does not appear to be controlled by gibbsite. The best fit of calculated dissolved inorganic Al was obtained using AlOHSO4 with a solubility less than that of pure crystalline jurbanite.


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