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The Ogallala Aquifer, a vast but shallow component of the High Plains deposit, supplies about 30 percent of all irrigation water in the United States.
Structure of search calls was variable, including shallow-modulated signals interspersed with mixed signals composed of a steeper frequency-modulated (FM) element and a shallow component (Fig. 1).
Insertion of the two types of barriers (Fig. 2D: solid barrier and Supplementary Fig.S5: 16-hole barrier) highlighted this effect, with rats using paths with a strong initial shallow component (solid barrier) and the lowest hole (16-hole barrier: hole 16) to reach the goal significantly more often.
The present study has provided evidence that rodent navigation in 3D space involves strong horizontal biases, with rats using a "layer strategy" during foraging (i.e., preferring to complete foraging at a given height above ground before moving to a new level), and preferring routes to a goal in which the easier, shallow component of the route occurs first.
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The experimental results indicate that CP Ti sheets could be formed into shallow components at room temperature, although the formability is limited in cold forming.
The shallow-inclination component can probably be attributed to tilting associated with the development of the rhyolite dome.
Deposits have a packstone to grainstone texture and contain abundant planktonic and benthic foraminifers together with lithoclasts and shallow water components such as Halimeda flakes (Fig. 6e).
These observations are interpreted to demonstrate that the shallow-inclination component cannot be attributed to the slope of the flow structure, and in some cases to its associated anisotropy.
In contrast, the randomization produces an ITF with twice as many edges than actually observed, with a correspondingly reduced ICE, so a shallower IN component.
When two possible routes to reach a goal were presented on the pegboard, by introducing a symmetrically placed barrier around which rats had to detour, the animals quickly developed a preference for the route having a strong shallow-first component over that in which the initial leg was steep.
We proposed a reservoir-model to take into account slow and fast components in the shallower part of the aquifer and a saline intrusion in the deeper one.
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