Skip To Main Content
Julie Albaric on Muck Rack

Julie Albaric

As seen in: Wiley Online Library
Is this you? As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work. Claim your profile

Get in touch with Julie

Contact Julie, search articles and posts on X, monitor coverage, and track replies from one place.

Learn more about Muck Rack

Actions

Share this page

Is this you?

As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.
Claim your profile

Articles

Monitoring Heat Transfer and Recharge Mechanisms in a Karst System Using Fiber Optic Distributed Temperature Sensing

|
By Anthony Nader, Jean-Philippe Malet, Julie Albaric
| Wiley Online Library Verified
Introduction Karst systems are formed by the dissolution of soluble rocks, such as limestone, resulting in characteristic geomorphological and hydrogeological features (Figure 1). A karst aquifer constitutes the water-bearing component of a karst system, which is typically divided into an upper unsaturated zone (or vadose zone) and a lower saturated zone. Karst reservoirs exhibit a bimodal porosity structure, consisting of matrix and fracture–conduit.
Open in Who Shared Issue with article?
See all 1 articles