德国HYDRO-BIOS公司多通道沉积物捕集器

MST德国HYDRO-BIOS公司多通道沉积物捕集器

参考价: 面议

具体成交价以合同协议为准
2018-05-14 09:00:00
873
产品属性
关闭
青岛水德仪器有限公司

青岛水德仪器有限公司

免费会员
收藏

组合推荐相似产品

产品简介

多通道沉积物捕集器/多通道沉积物捕获器--Multi Sediment Trap

多通道沉积物捕集器的设计主要用于对相对垂直颗粒流较大的湖泊、大陆架和水栖环境的沉积物的自动采集。在北极、南极、热带、亚热带等环境中,经过无数次的*野外操作,已经证明了它的可靠性。

详细介绍

名称: 德国HYDRO-BIOS公司多通道沉降物捕集器
类别: 多通道沉降物捕集器
型号: MST
关键字: 多通道沉降物捕集器,近海沉降物捕集器,沉降物捕获器
产品简介: 多通道沉降物捕集器用于对相对垂直颗粒流较大的湖泊、大陆架和水栖环境的沉降物的自动采集。
供应商: 青岛水德仪器有限公司
详细介绍

多通道沉降物捕集器
Multi Sediment Trap


多通道沉降物捕集器的设计主要用于对相对垂直颗粒流较大的湖泊、大陆架和水栖环境的沉降物的自动采集。在北极、南极、热带、亚热带等环境中,经过无数次的*野外操作,已经证明了它的可靠性。这款仪器不需要很重的固定线缆,它在较小的船上也可以很容易地安置和收回。多通道沉降物捕集器的控制装置可以执行为期一年多的时间依赖性工作。为了防止捕集到的沉降物从收集筒的上部被冲走,每个收集器在开口处都安装一个可拆卸的软皮网格,捕集器内部*不含金属。当多通道沉降物捕集器的采集瓶不工作时,它们与周围环境是隔离的。在布放和回收操作期间,收集筒底部是开放的,允许水流自动流过收集筒腔体。

整个系统由3节长时间锂电池供电。根据不同的需求,不同多通道沉降物捕集器的收集瓶数量可以是6、12、24,而且同时都有两种型号可供选择:

经济型:
经济型捕集器由一个电池供电的手持终端进行编程,允许操作人员对每个收集瓶的采样间隔预先设定,所有采样瓶的采样间隔都相等。

豪华型:
豪华型多通道沉降物捕集器通过PC机上的一个HYDRO-BIOS软件进行预编程,允许用户实时(年、月、日、时、分)对每个收集瓶的采样间隔单独预先设定,从1分钟至8760小时。豪华型采样器可通过增加各种参数的不同传感器进行升级,数据存储器容量可达4M。

经济型多通道沉降物捕集器规格:
框架材质:钛合金
采样间隔设定:通过手持终端编程
开口面积:0.015平方米
沉降筒长:560mm
圆锥筒夹角:40度
沉降筒直径与长度比例:1:4
zui大操作深度:3000米(6000米可选)

经济型多通道沉降物捕集器订购指南:

      类型 尺寸  高度  空气中重量  水中重量
444 100     6瓶 直径420mm 1000mm 12kg 5kg
444 120     12瓶 直径520mm 1040mm 25kg 10kg
444 140     24瓶 800×800mm 1000mm 45kg 20kg






豪华型多通道沉降物捕集器规格:
框架材质:钛合金
采样间隔设定:通过带OceanLab软件的电脑编程
开口面积:0.015平方米
沉降筒长:560mm
圆锥筒夹角:40度
沉降筒直径与长度比例:1:4
zui大操作深度:3000米(6000米可选)

豪华型多通道沉降物捕集器订购指南:
      类型 尺寸  高度  空气中重量  水中重量
444 101     6瓶 直径420mm 1000mm 12kg 5kg
444 121     12瓶 直径520mm 1040mm 25kg 10kg
444 141     24瓶 800×800mm 1000mm 45kg 20kg






444 150     备用收集瓶,容积250ml,24个/套
444 160     备用锂电池,3节/套

代表文献:
1.Jürgen Lenz, Alvaro Morales, Judith Gunkel,1993.Mesozooplankton standing stock during the North Atlantic spring bloom study in 1989 and its potential grazing pressure on phytoplankton: a comparison between low, medium and high latitudes.Deep Sea Research Part II: Topical Studies in Oceanography.40(1-2):559–572.
2.Dethleff, Dirk, Nürnberg, Dirk, Reimnitz, Erk, Saarso, Maart and Savchenko, Y.P.,1993.East Siberian Arctic Region Expedition '92: The Laptev Sea - its significance for Arctic sea-ice formation and transpolar sediment flux.Reports on Polar Research.120:3-48.
3.Bloesch Jürg,1996.Towards a new generation of sediment traps and a better measurement/understanding of settling particle flux in lakes and oceans: A hydrodynamical protocol.Aquatic Sciences.58(4):283-296.
4.A. Accornero, A. Bergamasco, A. Monaco, S. Tucci,1999.Particle Fluxes at the Edge of the Ross Ice Shelf: the Role of Physical Forcing.Oceanography of the Ross Sea Antarctica.177-195.
5.David N. Thomas, Hilary Kennedy, Gerhard Kattner, Dieter Gerdes, G. S. Dieckmann, Carl Gough,2002.Biogeochemistry of plaet ice: its influence on particle flux under fast ice in the Weddell Sea, Antarctica.Ecological Studies in the Antarctic Sea Ice Zone.169-179.
6.A. ACCORNERO, C. MANNO, K.R. ARRIGO, A. MARTINI and S. TUCCI,2003.The vertical flux of particulate matter in the polynya of Terra Nova Bay. Part I. Chemical constituents.Antarctic Science.15 (1): 119–132.
7.Alessandra Accornero, Marcia M. Gowing,2003.ANNUAL SEDIMENTATION PATTERN OF ZOOPLANKTON FECAL PELLETSIN THE SOUTHERN ROSS SEA: WHAT FOOD WEBS AND PROCESSESDOES THE RECORD IMPLY?.BIOGEOCHEMISTRY OF THE ROSS SEA ANTARCTIC RESEARCH SERIES.78:261-278.
8.P. Moreira-Turcq, J.M. Jouanneau, B. Turcq, P. Seylerd, O. Weber, J.L. Guyot,2004.Carbon sedimentation at Lago Grande de Curuai, a floodplain lake in the low Amazon region: insights into sedimentation rates.Palaeogeography, Palaeoclimatology, Palaeoecology.214(1–2):27–40.
9.V. Ramaswamy, M.M. Sarin, R. Rengarajan,2005.Enhanced export of carbon by salps during the northeast monsoon period in the northern Arabian Sea.Deep Sea Research Part II: Topical Studies in Oceanography.52(14-15):1922–1929.
10.J. C. Colombo, N. Cappelletti, J. Lasci, M. C. Migoya, E. Speranza, and C. N. Skorupka,2006.Sources, Vertical Fluxes, and Equivalent Toxicity of Aromatic Hydrocarbons in Coastal Sediments of the Río de la Plata Estuary, Argentina.Environmental Science & Technology.40(3), 734–740.
11.L. Roselli, C. Manno & G. Spezie ,2007.Inertial oscillations and particle flux interactions in a marine protected area in Gulf of Naples.Chemistry and Ecology.23(2):177-190.
12.C. Manno , S. Sandrini, L. Tositti, A. Accornero ,2007.First stages of degradation of Limacina helicina shells observed above the aragonite chemical lysocline in Terra Nova Bay (Antarctica).Journal of Marine Systems.68(1-2):91–102.
13.Jan Michels, Gerhard S. Dieckmann, David N. Thomas, Sigrid B. Schnack-Schiel, Andreas Krell, Philipp Assmy, Hilary Kennedy, Stathis Papadimitriou, Boris Cisewski,2008.Short-term biogenic particle flux under late spring sea ice in the western Weddell Sea.Deep Sea Research Part II: Topical Studies in Oceanography.55(8-9):1024–1039.
14.C. Manno1, V. Tirelli, A. Accornero and S. Fonda Umani,2009.Importance of the contribution of Limacina helicina faecal pellets to the carbon pump in Terra Nova Bay (Antarctica).Journal of Plankton Research.32(2):145-152.
15.Andreas Kleeberg, Christiane Herzog, Michael Hupfer,2013.Redox sensitivity of iron in phosphorus binding does not impede lake restoration.Water Research.47(3):1491–1502.


更多关键字: 多通道沉降物捕集器,近海沉降物捕集器,沉降物捕获器, 时间序列沉降物捕集器,Sediment Trap

上一篇:如何保证空气浮游菌采样器的采样效率? 下一篇:智能颗粒物中流量采样器的工作原理是什么?
热线电话 在线询价
提示

仪表网采购电话