Sentence examples for sediments exceeds from inspiring English sources

Based on the maximum As concentration determined in the oxida-tive extractions of the sediments and assuming that the As content of sulfide minerals present in the sediments exceeds 1.3 μmol/g (100 ppm), the lower limit for pyrite,[1] sulfide minerals should be present at less than 0.4% by weight of the sediment.

As can be noticed in Table  4, the average value of 239+240Pu in the soil is about 200 mBq/kg; the concentration of plutonium in lake sediments exceeds this value by 10 times; however, in river sediments it is about 4 times lower.

For such elements as Cr, Co, Mo, Ad and Pb, the contents in sediments exceeds that in water by four orders of magnitude, while the contents of Fe, Ni, Cu, Ga, Cd, Sn, Sb, Te, Hg and U were five orders of magnitude greater.

Some of the mercury levels in these sediments exceeded New York State screening values.

Nevertheless, the concentration of Mo, Mn and Zn in sediments exceeded reference levels for ecosystem protection and can lead to deficiency problems for on-site vegetation and to soil and water pollution off-site.

In the Ganges-Brahmaputra cone, sediments exceed 7 miles (11 km) in thickness and extend to latitude 10° S. Little sediment has accumulated along the southern Sunda Islands, probably because the Java Trench acts as a sediment trap; instead, silicic volcanic ash is found there.

Instead, erosion of surface sediments exceeded deposition from the tsunami.

The peak amplitudes at KR02 and KR04, which are located on sediments, exceed 450 cm/s2.

Measured concentrations of Cd, Cr, Cu, Mn, and Pb in the sediments exceed the sediment quality guideline for the lowest effect levels (LEL), while the concentrations of Cd and Pb are also higher than the effects range low (ERL) values, manifesting occasional adverse biological effects to the surrounding flora and fauna.

Given that the MMHg flux via sedimentation exceeds that due to resuspension at our study sites, it is possible that external MMHg sources deposited in the sediment via settling particles may provide a viable alternative explanation for the observed offsets in δHg between IHg (sediment) and the bioaccumulated MMHg.

Where sediment exceeded 25 cm depth, gullies formed allowing their banks and adjacent margins to drain faster than the surrounding sediment.