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Related Concept Videos

Water and Mineral Acquisition02:34

Water and Mineral Acquisition

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Specialized tissues in plant roots have evolved to capture water, minerals, and some ions from the soil. Roots exhibit a variety of branching patterns that facilitate this process. The outermost root cells have specialized structures called root hairs that increase the root surface, thus increasing soil contact. Water can passively cross into roots, as the concentration of water in the soil is higher than that of the root tissue. Minerals, in contrast, are actively transported into root cells.
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Aquaporins or AQPs are a family of integral membrane proteins whose primary function is to transport water, while some called aquaglyceroporins also transport glycerol. In addition, aquaporins have also been suspected to be involved in transporting volatile substances, such as carbon dioxide and ammonia, across membranes. Such AQPs that act as gas channels are often highly expressed in cells involved in the gaseous exchange, such as red blood cells, epithelial cells, and pulmonary capillaries.
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Inductively coupled plasma (ICP) is the most widely used plasma source in atomic emission spectroscopy (AES), also known as Inductively Coupled Plasma Optical Emission Spectroscopy (ICP-OES). The ICP source, or torch, consists of three concentric quartz tubes with argon gas flowing through them. A spark from a Tesla coil initiates the ionization of argon, generating a high-temperature plasma.
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When cells are placed in a hypotonic (low-salt) fluid, they can swell and burst. Meanwhile, cells in a hypertonic solution—with a higher salt concentration—can shrivel and die. How do fish cells avoid these gruesome fates in hypotonic freshwater or hypertonic seawater environments?
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Related Experiment Video

Updated: Sep 24, 2025

Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds
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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds

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Idaho's Eastern Snake Plain Aquifer Managed Aquifer Recharge Program.

Wesley Hipke, Paul Thomas1, Noah Stewart-Maddox2

  • 1IDWR Contractor via Boise State University, Boise, ID, USA.

Ground Water
|May 10, 2022
PubMed
Summary
This summary is machine-generated.

The Eastern Snake Plain Aquifer (ESPA) recharge program has successfully replenished the aquifer, adding an average of 0.3207 km³ per year. This cost-effective managed aquifer recharge (MAR) program utilizes existing infrastructure and natural water rights.

Area of Science:

  • Hydrology and Water Resource Management
  • Environmental Engineering
  • Sustainable Water Management

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Background:

  • The Eastern Snake Plain Aquifer (ESPA) in Idaho, a critical water resource, has faced significant depletion since the 1950s.
  • Declining ESPA levels are attributed to climate change, increased water demand, and evolving irrigation practices.
  • The Idaho Water Resource Board (IWRB) initiated the ESPA Comprehensive Aquifer Management Plan (CAMP) to address aquifer decline.