603403

YSI 3403 Glass Dip Conductivity Cell

YSI 3403 Glass Dip Conductivity Cell

Description

3403 glass dip cell, cell constant = 1.0/cm, 4 ft. cable

Free Shipping on this product
List Price
$590.00
Your Price
$560.50
Usually ships in 3-5 days

Shipping Information
Return Policy
Why Buy From Fondriest?
Image Part # Product Description Price Stock Order
YSI 3403 Glass Dip Conductivity Cell 603403 3403 glass dip cell, cell constant = 1.0/cm, 4 ft. cable
$560.50
Usually ships in 3-5 days

In The News

What is Conductivity?

UPDATE : Fondriest Environmental is offering their expertise in conductivity through their new online knowledge base. This resource provides an updated and comprehensive look at conductivity and why it is important to water quality. To learn more, check out: Conductivity, Salinity and TDS . Salinity and conductivity  measure the water's ability to conduct electricity, which provides a measure of what is dissolved in water. In the SWMP data, a higher conductivity value indicates that there are more chemicals dissolved in the water. Conductivity measures the water's ability to conduct electricity. It is the opposite of resistance. Pure, distilled water is a poor conductor of electricity.

Read More

Weeks Bay NERR offers glimpse into ancient estuaries along the northern Gulf of Mexico

Mike Shelton, natural resources planner for Weeks Bay National Estuarine Research Reserve (NERR), has spent 17 years at the Reserve. The Reserve was founded in 1986 and is located in the Alabama and Florida coastal region. “It’s a great place for outdoor enthusiasts. Places like this are why we live on the coast,” he enthuses. “There’s also a lot of history here. It’s one of the first areas settled by the Europeans after they arrived in America. The city of Pensacola was the second city built in the U.S.,” adds Scott Phipps, research coordinator for Weeks Bay NERR. Weeks Bay NERR monitoring follows the same System Wide Monitoring Program (SWMP) as the other 28 NERRs, which includes deploying data-gathering sondes throughout the Bay.

Read More

Reconstructing Past Ocean Temperatures with Samples of Antarctic Ice

Part of the secret to knowing just how much Earth's oceans have warmed as its climate has changed in the past—and might change in the future—might be locked in the ice of Antarctica. A research team has discovered a way to use noble gas ratios to calculate the average temperature of the oceans of our past. Geoscientist and study author Dr. Jeff Severinghaus and teammates from Scripps Oceanography and other institutions in Japan and Switzerland worked together on the tricky problem of measuring ocean temperatures of the past. Until now, the distribution of different water masses around the globe has made determining changes in the average temperature of the world's oceans nearly impossible.

Read More