Fróðskaparrit - 01.01.2009, Qupperneq 174

Fróðskaparrit - 01.01.2009, Qupperneq 174
172 CHEMICAL SEDIMENT VARIABLES FROM THE FAROE AREA: ORGANIC CONTENT, NITROGEN, PHOSPHORUS, ZINC, AND COPPER fect when compared to untreated samples. In un-sieved samples it is reasonable to ex- pect a high content of large, non-organic particles to influence the result, as well as large numbers of small tube dwelling worms (e.g„ Myriochele sp. and Phoronida sp.) or just a few specimens of large bodied animals (e.g., Arctica islandica). Seaweed would also in- fluence the result. Sieving eliminates the vari- ability of samples and makes comparison re- sults more reliable. There is no information on any sieving of the sediment before analy- sis by other authors so it is reasonable to ex- pect the analyses to be done on untreated sediments. Some of the sites in this study are re- peatedly sampled. There are a few replicates. some are sampled more than once a year and many are sampled about yearly. In such cases, it should be possible to get a crude chemical picture of the natural variance at the site. Comparison between sites should therefore be done with caution, especially because there is so little information about the samples and sampling procedures. The stability of organic content (LOI values) One of the interesting questions this study could help answer is how stable or change- able is the organic content in the upper lay- ers of the seabed. Is it constant at the same site or does the organic content change tem- porarily according to sources of organic input? Due to various reasons, it is diflicult to collect sufficient quality data on organic content from the same site over a long pe- riod of time. In Table 12, all available data from two of the stations from Skálafjørður, SK05 and SK07 are shown. SK05 is in the middle of the fjord at the deepest part at a depth of about 67 m and SK07 about 2 km north of SK05. Both are soft bottom locali- ties. The data from these two stations are from untreated samples. There are 24 samples from SK05 and 13 from SK07 (Bloch et al„ 1986; Gaard, 1990; Hoydal and Dam, 2004 and Johansen, 2006). In 1985 and 1987, several samples were taken during the summer period (no replicates). In 1997, three replicates were analyzed from SK05 and, in 2005, two replicates. In the years 2000, 2001 and 2003, one single sample was analyzed at each site. The overall lowest value from SK05 was 5.5 % and the highest was 13.9 %. At station
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