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Related Concept Videos

Temperature Measurement Sites01:14

Temperature Measurement Sites

1.7K
A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
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Rapidly Varying Flow01:24

Rapidly Varying Flow

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Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
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Assessing Body Temperature - Temporal Artery01:19

Assessing Body Temperature - Temporal Artery

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Here is a stepwise guide to assessing the body temperature at the temporal artery using a temporal artery thermometer
Step 1: Perform hand hygiene and don a fresh pair of gloves to prevent cross-infection and ensure patient safety.
Step 2: Explain the procedure to the patient to establish trust. Clear communication establishes trust with the patient, ensures they understand what to expect, promotes cooperation, and enhances comfort during the procedure.  
Step 3: Assess the patient's...
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Related Experiment Video

Updated: Jul 9, 2025

Design, Instrumentation and Usage Protocols for Distributed In Situ Thermal Hot Spots Monitoring in Electric Coils using FBG Sensor Multiplexing
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Active-distributed temperature sensing dataset beneath a braided river.

Alice J Sai Louie1, Leanne K Morgan1, Eddie W Banks2

  • 1Waterways Centre for Freshwater Management, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand.

Data in Brief
|November 29, 2023
PubMed
Summary
This summary is machine-generated.

Active-distributed temperature sensing (A-DTS) effectively measured groundwater recharge fluctuations in braided rivers. This new method offers crucial insights into temporal changes in riverbed water infiltration.

Keywords:
Alluvial aquiferFiber opticsGroundwater rechargeHeat as a tracerRiver

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Area of Science:

  • Environmental Science
  • Hydrology
  • Geophysics

Background:

  • Braided rivers are vital for groundwater replenishment.
  • Current methods lack the spatiotemporal resolution to accurately measure recharge in these dynamic systems.
  • Understanding temporal recharge variations is crucial for water resource management.

Purpose of the Study:

  • To evaluate the efficacy of active-distributed temperature sensing (A-DTS) for quantifying groundwater recharge in braided rivers.
  • To assess temporal changes in groundwater recharge rates.
  • To address the limitations of traditional methods in complex riverine environments.

Main Methods:

  • Utilized active-distributed temperature sensing (A-DTS) with a fiber optic cable.
  • Conducted twelve consecutive A-DTS surveys to a depth of 5 meters.
  • Monitored the Waikirikiri Selwyn River over a period of stable river stage and flow.

Main Results:

  • Demonstrated the capability of A-DTS to detect and quantify temporal variations in groundwater recharge.
  • Successfully measured groundwater fluxes beneath the braided river system.
  • Provided high-resolution data on recharge dynamics.

Conclusions:

  • Active-distributed temperature sensing (A-DTS) is a viable and effective technique for studying groundwater recharge in braided rivers.
  • The study highlights the potential of A-DTS for improving our understanding of hydrological processes in complex river systems.
  • This method offers a significant advancement over traditional techniques for measuring groundwater recharge.