Benthic lander
Abenthic landeris anautonomousobservational platform that sits on theseabedorbenthic zoneto record physical,chemicalor biological activity.[1]
Benthic landers have deployment durations from a few days (forbiologicalstudies) to several years (forphysical oceanographystudies). In these studies they conduct a variety of underwater measurements, and thus different lander configurations exist to meet differing needs for different measurements.
Purpose[edit]
Samples that are brought up from the seabed undergo large changes intemperatureandpressure,thus changing their physical and chemical composition and properties.[2]This change in properties means that any measurements taken from samples brought to the surface do not provide accurate data.[2]In order to avoid this, it is best that the measurements are taken directly at the seabed level, without moving the samples. Initially, to prevent altering samples,diverswould go to the sea bed and carry out the experiments.[2]However, divers have a very small range of depth and a short time under water and cause a large disturbance to the sea bed, thereby introducing more error into the measurements.[2]These shortcomings are improved by using benthic landers as they have a much larger depth and time capacity than divers and can be designed to cause minimal disturbance to the sea floor.[2]Some common uses for the collected seabed data include studyingcurrents,tides,andmicroseismicandmagnetic fieldactivity and monitoringmarine life.[2]
Variations[edit]
Benthic landers come in a variety of shapes and sizes depending upon theinstrumentationthey carry, and are typically capable of working at any ocean depth.[3]One type of instrumentation that is often used on benthic landers is aneddy correlationinstrument that measures oxygenflux.[2]Different types of landers are used depending on the length and nature of the mission. Longer duration mission landers are typically equipped withultrasonic sensors,LiDAR,andcamerasin order to intelligently navigate the seabed.[3]Additionally, depending on what measurements the mission is intended to take, the lander can be configured to disrupt the environment in different ways enabling for higher precision of certain data sets at the tradeoff of others.[3]New technologies are constantly being developed to improve lander data collection, one example beingholography,which is meant to be utilized to take measurements of the seabed far from the lander.[3]
See also[edit]
References[edit]
- ^Freiwald, André (2005-05-20).Cold-Water Corals and Ecosystems.Springer Science & Business Media.ISBN978-3-540-24136-2.
- ^abcdefgTengberg, A.; De Bovee, F.; Hall, P.; Berelson, W.; Chadwick, D.; Ciceri, G.; Crassous, P.; Devol, A.; Emerson, S.; Gage, J.; Glud, R.; Graziottini, F.; Gundersen, J.; Hammond, D.; Helder, W. (January 1995)."Benthic chamber and profiling landers in oceanography — A review of design, technical solutions and functioning".Progress in Oceanography.35(3): 253–294.doi:10.1016/0079-6611(95)00009-6.ISSN0079-6611.
- ^abcdViollier, E; Rabouille, C; Apitz, S.E; Breuer, E; Chaillou, G; Dedieu, K; Furukawa, Y; Grenz, C; Hall, P; Janssen, F; Morford, J.L; Poggiale, J.-C; Roberts, S; Shimmield, T; Taillefert, M (February 2003)."Benthic biogeochemistry: state of the art technologies and guidelines for the future of in situ survey".Journal of Experimental Marine Biology and Ecology.285–286: 5–31.doi:10.1016/s0022-0981(02)00517-8.hdl:21.11116/0000-0001-D24F-A.ISSN0022-0981.
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