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841.
Abstract. Benthic metabolism and standing stocks were investigated in the deep Red Sea between 21o and 27o N, Activity was assessed by the determination of respiration rates with a shipboard method and by calculating oxygen consumption from the activity in the electron transport system. We attempted to compare results from different latitudes within the warm Red Sea and with data from cold Atlantic environments. Our investigations were part of an environmental risk assessment to evaluate future mining of metalliferous sediments from the Atlantis II Deep. 相似文献
842.
843.
Kinetic studies have been carried out on the dissolution of 10μm beads of silica and of the siliceous tests of two species of diatoms (Thalassiosira fluviatus andSkeletonema costatum) in sea water at 10–50°C and over the pH range 6–9. At all temperatures dissolution of the biogenous silica occurred most
rapidly at pH 8 and most slowly at pH 6. First order kinetics were closely followed when the silica was present in a considerable
excess over that required for saturation, the rate being proportional to the area of the silica. Apparent deviation from this
type of kinetics occurred when there was insufficient silica to bring about saturation. This was undoubtedly due to the progressive
decrease in the surface area which takes place as the particle dissolves. Application of the rather simplistic model developed
by Kamataniet al. (1980), which makes allowance for this decrease, gave a close correspondence with the data until ∼ 90% of the silica had
dissolved. 相似文献
844.
845.
846.
847.
The mode of capsize of a discus buoy in breaking waves is discussed. The results of model tests are given; these show that a judicious choice of mooring design can substantially reduce the chance of capsize. A comparison is made with the performance of the buoy on station. 相似文献
848.
Methods developed earlier, based on hydration numbers for individual ionic species, have been extended to the calculation of ionic activity coefficients in aqueous systems of two electrolytes MX and NX2 with a common unhydrated anion (X−). The data required include the mean activity coefficients of MX and NX2 in the mixtures, together with the osmotic coefficient. The procedure is illustrated by a calculation of γNa, γMg, and γCl in a mixture of NaCl and MgCl2 closely approximating the composition of seawater with salinity of 35‰. 相似文献
849.
Simultaneous wind, wave, and current data during 21 storms spanning four winters at Tromsøflaket (230 m depth) were analysed to determine joint probabilities of occurrence. Waves were measured with a Waverider Buoy, winds with a recording anemometer onboard a vessel and currents at up to five depths with Aandera RCM-4 current meters. Measured currents were filtered to separate tidal currents from residual currents. In most of the statistical analyses, the actual current profiles were replaced with a simplified “equivalent” profile (constant above 50 m depth) whose magnitude was chosen to give the same drag load on a single pile as the actual profile when both profiles were combined with wave orbital velocities. The data suggest that the equivalent current is weakly correlated with the wave height. Within the range of the data analysed, an in-line equivalent residual current of 30 cm sec−1 is adequate for design drag force calculations.The data presented here are used to illustrate a procedure for data analysis and are not suitable for use as design criteria. 相似文献
850.
R. Von Herzen 《Applied Ocean Research》1985,7(3):175-176