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德國HYDRO-BIOS公司 積分采水器
類(lèi)別: 積分采水器
型號: 436 601
關(guān)鍵字: 水體采樣,積分采水器,采水器,柱狀水體采樣,簡(jiǎn)易采水器
供應商: 青島水德科技有限公司
產(chǎn)品簡(jiǎn)介:

積分采水器用于對水體進(jìn)行柱狀積分采樣。

積分采水器可以對期望深度進(jìn)行編程,并將數據通過(guò)手持終端或電腦的OceanLab 3軟件存儲在采水器中。采水器的推薦下降速度會(huì )顯示在手持終端的顯示器上,然后采水器在水中下降,電子器件會(huì )自動(dòng)調節因船體的不穩定或海面的不平靜導致的采水器下降速度不穩定所帶來(lái)的采樣誤差。當采水器到達結束深度后,采水器中的樣品含量為2.5L或5L時(shí)被拉起,由于采樣深度可以自由設定,可以獲得不同深度的柱狀水樣。

詳細介紹

德國HYDRO-BIOS公司——第三代積分采水器

IWS III- Integrating Water Sampler

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積分采水器的設計,是為了與歐盟水框架指令提出的要求相一致,積分采水器用于對柱狀水體進(jìn)行積分采樣。


積分采水器的特點(diǎn):

  • 采水器外部電源配備單獨的外殼

  • 快速啟動(dòng)按鈕-啟動(dòng)采水器,使用之前編程的采樣深度

  • 協(xié)議-集成在OceanLab3軟件中

  • 采水器可自由設定深度范圍

積分采水器的新特點(diǎn):

  • 采水器的手持終端或電腦可以用藍牙連接

  • 采水器無(wú)需連接電纜即可對現場(chǎng)采樣預編程

  • 時(shí)間-積分采樣(例如可以對水平采樣過(guò)程設定起始時(shí)間和結束時(shí)間)

 

采水器由內置的壓力傳感器和電子控制單元來(lái)控制,頂端還配備了小型的馬達單元,確保對整個(gè)柱狀水樣在期望的深度進(jìn)行完整的采樣。采水器的供電由可充電的LiFePo4蓄電池來(lái)提供。

IWS III采水器使用起來(lái)非常簡(jiǎn)單:

積分采水器可以對期望深度(開(kāi)始深度和結束深度可自由設定)進(jìn)行編程,并將數據通過(guò)手持終端或電腦的OceanLab 3軟件存儲在采水器中。采水器的推薦下降速度會(huì )顯示在手持終端的顯示器上,然后采水器在水中下降,電子器件會(huì )自動(dòng)調節由于船體的不穩定或海面的不平靜,使得采水器的下降速度不穩定所帶來(lái)的采樣誤差。當采水器到達結束深度后,采水器中的樣品含量為2.5或5L時(shí)被拉起,由于采樣深度可以自由設定,可以獲得不同深度的柱狀水樣。

圖片15.png           圖片16.png      圖片17.png圖片18.png

積分采水器技術(shù)參數:

長(cháng)度: 720或880mm                                              

容積: 2.5或5.0L

材質(zhì):POM,丙烯酸塑料,鈦合金,不銹鋼

空氣中重量:7kg或8kg

操作:一組電池可以執行約20次完整采樣工作

耐壓深度: 100m

 

積分采水器的選配:

深海版本:耐壓深度3000m

在線(xiàn)版本:通過(guò)手持終端或者PC進(jìn)行控制和深度讀?。≧S232-傳輸距離約50米或FSK單芯電纜,傳輸距離無(wú)限制)

多通道采樣系統:安裝到多通道水樣采集器上,可以同時(shí)進(jìn)行多個(gè)不同深度的采樣

 

積分采水器訂購信息:

436 601  第三代積分采水器,2.5 L,100m

436 602  第三代積分采水器,2.5 L,3000m
436 606  第三代積分采水器,5.0 L,100m

436 607  第三代積分采水器,5.0 L,3000m

 

代表文獻:

1.Edwin T.H.M. Peeters, Jean J.P. Gardeniers, Albert A. Koelmans,2000.Contribution of trace metals in structuring in situ macroinvertebrate community composition along a salinity gradient.Environmental Toxicology and Chemistry.19(4):1002-1010.

2.K. G. Schulz, R. G. J. Bellerby, C. P. D. Brussaard, J. Büdenbender, J. Czerny, A. Engel, M. Fischer, S. Koch-Klavsen, S. A. Krug, S. Lischka, A. Ludwig, M. Meyerh?fer, G. Nondal, A. Silyakova, A. Stuhr, and U. Riebesell,2012.Temporal biomass dynamics of an Arctic plankton bloom in response to increasing levels of atmospheric carbon dioxide.Biogeosciences Discussions.9:12543-12592.

3.Czerny, Jan, Schulz, Kai G., Boxhammer, Tim, Bellerby, R. G. J., Büdenbender, Jan, Engel, Anja, Krug, Sebastian, Ludwig, Andrea, Nachtigall, Kerstin, Nondal, G., Niehoff, B., Siljakova, A. and Riebesell, Ulf,2012.Element budgets in an Arctic mesocosm CO2 perturbation study.Biogeosciences Discussions.9 (8):11885-11924.

4.S. D. Archer, S. A. Kimmance, J. A. Stephens, F. E. Hopkins, R. G. J. Bellerby, K. G. Schulz, J. Piontek, and A. Engel,2012.Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters.Biogeosciences Discussions.9:12803-12843.

5.Leu, E., Daase, M., Schulz, Kai G., Stuhr, Annegret and Riebesell, Ulf,2012.Effect of ocean acidification on the fatty acid composition of a natural plankton community.Biogeosciences Discussions.9 (7):8173-8197.

6.M. Sperling, J. Piontek, G. Gerdts, A. Wichels, H. Schunck, A.-S. Roy, J. La Roche, J. Gilbert, L. Bittner, S. Romac, U. Riebesell, and A. Engel,2012.Effect of elevated CO2 on the dynamics of particle attached and free living bacterioplankton communities in an Arctic fjord.Biogeosciences Discussions.9:10725-10755.

7.Kluijver, A. de,2012.Carbon flows in natural plankton communities in the Anthropocene.Geowetenschappen Proefschriften.1-118.

8.K. G. Schulz, U. Riebesell,2012.Diurnal changes in seawater carbonate chemistry speciation at increasing atmospheric carbon dioxide.Marine Biology.DOI 10.1007/s00227-012-1965-y.

9.J. Hua, W.H. Hwang,2012.Effects of voyage routing on the survival of microbes in ballast water.Ocean Engineering.42:165-175.

10."T. Tanaka, S. Alliouane, R. G. B. Bellerby, J. Czerny, A. de Kluijver, U. Riebesell6, K. G. Schulz,

A. Silyakova, and J.-P. Gattuso",2013.Effect of increased pCO2 on the planktonic metabolic balance during a mesocosm experiment in an Arctic fjord.Biogeosciences(BG).10:315–325.

11.A. de Kluijver, K. Soetaert, J. Czerny, K. G. Schulz, T. Boxhammer, U. Riebesell, and J. J. Middelburg,2013.A 13C labelling study on carbon fluxes in Arctic plankton communities under elevated CO2 levels.Biogeosciences(BG).10:1425-1440.

12.Czerny, Jan, Schulz, Kai G., Ludwig, Andrea and Riebesell, Ulf,2013.A simple method for air–sea gas exchange measurements in mesocosms and its application in carbon budgeting.Biogeosciences(BG).10 (3):11989-12017.

13.F. E. Hopkins, S. A. Kimmance1, J. A. Stephens, R. G. J. Bellerby, C. P. D. Brussaard, J. Czerny, K. G. Schulz, and S. D. Archer,2013.Response of halocarbons to ocean acidification in the Arctic.Biogeosciences(BG).10:2331-2345.

14.Czerny, Jan, Schulz, Kai G., Boxhammer, Tim, Bellerby, R. G. J., Büdenbender, Jan, Engel, Anja, Krug, Sebastian, Ludwig, Andrea, Nachtigall, Kerstin, Nondal, G., Niehoff, B., Silyakova, A. and Riebesell, Ulf,2013.Implications of elevated CO2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach.Biogeosciences(BG).10 (5):3109-3125.

15.R. Zhang, X. Xia, S. C. K. Lau, C. Motegi, M. G. Weinbauer, and N. Jiao,2013.Response of bacterioplankton community structure to an artificial gradient of pCO2 in the Arctic Ocean.Biogeosciences(BG).10, 3679–3689, 2013.


更多關(guān)鍵詞:水體采樣,積分采水器,采水器,底部采水器,深度積分采水器,柱狀水體采樣,簡(jiǎn)易采水器

資料下載:

德國HYDRO-BIOS公司第三代積分采水器介紹.pdf

水德產(chǎn)品冊.pdf

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