southampton water
Recently Published Documents


TOTAL DOCUMENTS

102
(FIVE YEARS 3)

H-INDEX

21
(FIVE YEARS 0)

Author(s):  
Alex Montgomery

Abstract The use of conventional offshore containment boom is a recognised way of containing and recovering oil spilt at sea. However, there are various operational and logistical challenges with their use. One of the largest being that their containment becomes ineffective when towed through the water at speeds of greater than 0.75 knots. Containment and collection of oil using high speed systems allows for greater tow speeds (2–3 knots) without failure and can be operated with a paravane as a single ship system. Oil Spill Response Limited (OSRL) have had numerous requests from its members to supply offshore containment and recovery systems suitable for a single vessel deployment. The reason for this was to help with the challenges of low availability of vessels suitable for offshore operations and to reduce high costs. OSRL have used manufacturers guidance to advise its members on the best options however wished to have its own data to further support this guidance and provide user-validated recommendations to its members. OSRL have investigated the viability of using a paravane with a conventional offshore boom using field tests. These tests focused on vessel tow speed, current speed, boom containment effectiveness and encounter area. A number of deployments were carried out using conventional inflation boom and a medium sized paravane in Southampton Water, UK in 2018 (Figure 1). Observations were gathered to identify the point of boom failure when towed at different speeds and whether a suitable encounter area could be achieved. This poster will provide the detail on the feasibility of towing a conventional offshore boom with a single vessel and paravane, see boom configuration in Figure 2. It will outline specifications and parameters which make for a successful / unsuccessful deployment of conventional boom with paravane and provide recommendations for Tier 1 single vessel deployment equipment.


2013 ◽  
Author(s):  
J. BUBEER ◽  
B.COOPER ◽  
D.W.RYCROFT AND D.CLARKE

WINCHESTER COLLEGE 41 This discrepancy is assumed to be an abatement off the contract price as in 1815 and two entries of 1s. 9 1/2d. have been adjusted to 1s. 91/4d. and 1s. 8d. per bu. respectively. The entry in the first year of the series shows the chal­ dron at this date to be equal to 32 bu. and in 1683 the entry 8 ch. 4 bu. at 1s. 2d. per bu. = £15 17s. 8d. probably involves a 32-bu. chaldron and includes a charge for car­ riage. Calculations involving chaldrons and bushels in 1675, 1681 and 1699 have therefore been based on a 32-bu. chaldron. In all other years during this period, and later, except for coal for the Sickhouse from 1795, purchases are recorded by the bushel. In 1766 288 bu. are stated to be equal to 8 ch. (i.e. the London chaldron of 36 bu.) and in 1791 also the chaldron works out at 36 bu. Chaldron prices for the Sickhouse from 1795, by comparison with other prices per bu., are clearly for 36 bu., and in three years the alternative price per bu. is given at 1/36 of the price per ch. Hence it seems clear that coal was at first sup­ plied by local measure, i.e. by the bushel of 9 gals. with therefore only 32 bu. to a chaldron, and later by London measure—probably from the date when contracts were made with local dealers obtaining coal via Southampton Water, re-shipped from London and therefore by London measure. In tabulating, the 32-bu. chaldron in early years has been accepted as comparable with the later 36–bu. chaldron ; bushel prices up to 1710 have been translated to the chaldron by 32 : 1 and from 1739 by 36 : 1, i.e. the bare London chaldron throughout. The bushel quota­ tions indicate small purchases at a time and it is not deemed appropriate to raise prices by 21 : 20 to the full-pay ch., i.e. to 1/20 of the London score of 21 ch. The annual purchase rose from an average 91/2 ch. at the beginning of the series to about 30 ch. by the end. In addition, the Sickhouse received 1 ch. each year in 1792–94 and generally 2 ch. annually thereafter. The purchase for the Library from 1806 was 36 bu. annually. The quality is never specified. 1394–1657. Gross 264, Net 220. 1714–38. Gross 25, Net 18. 1771–1816. Gross 46, Net 45. These prices are for free purchases until about 1524,

2013 ◽  
pp. 103-103

2011 ◽  
Vol 1 (32) ◽  
pp. 50
Author(s):  
Elizabeth Chellew ◽  
Kate Rossington ◽  
Ian Townend ◽  
Carl Amos ◽  
Stephen Richardson

The influence of seawalls in modifying the equilibrium form of a shoreline has previously caused extensive debate. A numerical model was used to predict the equilibrium form of muddy intertidal profiles, along a shoreline in Southampton Water, UK. It was found that the profile containing a seawall had a very different profile form to the undefended sites, and that this seawall profile could not be accurately represented in the model. The model was extended to include wave reflection from the seawall, producing a new prediction with a much improved resemblance of the observed profile. It was concluded that the likely cause of the different profile form at the site of the seawall in this case, is due incident and reflected wave interaction.


2010 ◽  
Vol 90 (5) ◽  
pp. 1019-1023 ◽  
Author(s):  
Alastair Brown ◽  
Olaf Heilmayer ◽  
Sven Thatje

Metabolism and growth rate of the hard clam, Mercenaria mercenaria, were investigated in a population invasive to Southampton Water, southern England. An individual metabolic model expressed as a function of soft tissue dry mass was fitted to data of 18 individuals (log (VO2) = −1.952 + 0.543 • log (DM); F1,16 = 201.18, P < 0.001, r2 = 0.926). A von Bertalanffy growth function was fitted to 227 size-at-age data pairs of 18 individuals (Ht = 80.13 • (1 − e−0.149 • (t−0.542)); r2 = 0.927). Individual age-specific somatic production was calculated, demonstrating increase with age to a maximum of 3.88 kJ y−1 at ten years old followed by decrease, and individual age-specific annual respiration was calculated, demonstrating asymptotic increase with age to 231.37 kJ y−1 at 30 years old. Results found here lie within the physiological tolerances reported across the biogeographical range, suggesting that the species' biogeographical limitation in the UK to Southampton Water results from ecological rather than physiological factors.


Sign in / Sign up

Export Citation Format

Share Document