Interstitial Water and Sediment Chemistry of Two Cores from Florida Bay

Author(s):  
Jeffrey K. Rosenfeld (2)
1975 ◽  
Vol 19 (1) ◽  
pp. 367-371
Author(s):  
Dennis R. Sasseville ◽  
Stephen A. Norton ◽  
Ronald B. Davis

2015 ◽  
Vol 15 (2) ◽  
pp. 77-82
Author(s):  
Małgorzata Włodarczyk ◽  
Hanna Siwek ◽  
Anna Buchwał ◽  
Edyta Rafacz

Abstract The purpose of the paper was to assess the changes in the concentration of selected metals in the bottom sediment and interstitial water of the River Chotla in northwest Poland. The research was conducted on the river section flowing through Zaspy Małe and a salmonid fish breeding farm. Samples of water and bottom sediment were taken in four control and measurement points, located above and below the village and on a backwater above the trouteries and below the fish breeding ponds. The pH and the concentration of the metals potassium, iron, calcium, manganese and zinc were determined in the water and sediment samples. The lowest concentrations of the metals were found in the samples collected above and below Zaspy Małe, while the highest concentrations of metals in the water and sediment were found in the samples taken in the backwater, above the fish breeding ponds. Exceptions were calcium and potassium, with the highest concentrations of metals in the water being found in the samples taken below the fish breeding ponds. The content of metals in sediments of the analysed section of the River Chotla was mainly determined by the content of organic matter, which varied as it is dependent on water accumulation processes and the operation of nearby fishery facilities. The slightly alkaline pH facilitated long-lasting accumulation of metals in sediments.


2011 ◽  
Vol 74 (2) ◽  
pp. 351-360 ◽  
Author(s):  
Cristina Pulido ◽  
Kaj Sand-Jensen ◽  
Esther C. H. E. T. Lucassen ◽  
Jan G. M. Roelofs ◽  
Klaus P. Brodersen ◽  
...  

2017 ◽  
Vol 75 (6) ◽  
pp. 1455-1465 ◽  
Author(s):  
Shengnan Zhao ◽  
Xiaohong Shi ◽  
Changyou Li ◽  
Sheng Zhang ◽  
Biao Sun ◽  
...  

Overlying water and sediment samples were collected from 11 locations in Ulansuhai Lake in June of 2012 to determine the concentration of dissolved inorganic phosphorus (DIP) in the interstitial water, overlying water and sediment and to estimate the diffusion flux of DIP at the sediment–water interface. The DIP levels in overlying water were 0.004–0.185 mg/L (average = 0.062 mg/L), while they were 0.05–0.25 mg/L (average = 0.124 mg/L) in the interstitial water in the 0–2 cm surface sediment. Moreover, the annual mean exchange flux of DIP in the sediment was between −0.092 mg/m2·d and 0.053 mg/m2·d, and this occurred via internal source action in most areas. After area weighting, it is estimated that the exchange capacity of DIP at the sediment–water interface of the Ulansuhai Lake is 1.30 t/a. These findings indicate internal loading of phosphorus in sediment of the Ulansuhai Lake; thus, the diffusion of DIP in the interstitial water has effects on the lake, with a degree of influence of 2.7% to 81.5%.


2009 ◽  
Vol 43 (3) ◽  
pp. 463-474 ◽  
Author(s):  
Jianting Ju ◽  
Li-ping Zhu ◽  
Junbo Wang ◽  
Manping Xie ◽  
Xiaolin Zhen ◽  
...  

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