2017
DOI: 10.1061/(asce)hy.1943-7900.0001342
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Extended Theory of Hydraulic Hysteresis in Open-Channel Flow

Abstract: The occurrence of hysteresis in a supercritical, open-channel flow approaching an obstacle has been recognized and investigated both experimentally and theoretically over the last few decades. However, the available theory and experimental investigations in the literature do not include the case when subcritical flow, controlled from downstream, can establish across the obstacle. The present work fills this gap by proposing a new theory that includes this occurrence and shows that two different steady flow sta… Show more

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Cited by 15 publications
(6 citation statements)
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“…When a positive surge propagates upstream on a steep slope over an incoming supercritical flow, it progressively decelerates and asymptotically tends toward a stationary hydraulic jump [10]; when, instead, a positive surge propagates upstream on a mild slope over an incoming subcritical flow, the wavefront progressively reduces its height until the surge vanishes. Interestingly, the latter occurrence has never been reported and discussed in the literature and, as it happens, solutions to open channel flow problems never ceases to amaze by showing unexpected behaviours even within simple and schematic frameworks (e.g., [14][15][16][17][18][19][20]).…”
Section: Introductionmentioning
confidence: 99%
“…When a positive surge propagates upstream on a steep slope over an incoming supercritical flow, it progressively decelerates and asymptotically tends toward a stationary hydraulic jump [10]; when, instead, a positive surge propagates upstream on a mild slope over an incoming subcritical flow, the wavefront progressively reduces its height until the surge vanishes. Interestingly, the latter occurrence has never been reported and discussed in the literature and, as it happens, solutions to open channel flow problems never ceases to amaze by showing unexpected behaviours even within simple and schematic frameworks (e.g., [14][15][16][17][18][19][20]).…”
Section: Introductionmentioning
confidence: 99%
“…The coexistence of multiple steady states for supercritical flows approaching a contraction is called hydraulic hysteresis (Defina andViero 2010, Viero andDefina 2017). In the early studies (Akers andBokhove 2008, Defina andViero 2010), it was assumed that this phenomenon depended on the upstream flow conditions and on the contraction characteristics, assuming that critical conditions were established at the downstream end of the channel contraction in the flow configurations E1 and E3 (classic hydraulic hysteresis).…”
Section: Multiple Solutions and Hydraulic Hysteresismentioning
confidence: 99%
“…In the early studies (Akers andBokhove 2008, Defina andViero 2010), it was assumed that this phenomenon depended on the upstream flow conditions and on the contraction characteristics, assuming that critical conditions were established at the downstream end of the channel contraction in the flow configurations E1 and E3 (classic hydraulic hysteresis). Viero and Defina (2017) have recently generalized the classic hydraulic hysteresis concept to the case that a subcritical downstream boundary condition may have a role in determining the flow characteristics through the channel contraction (generalized hydraulic hysteresis).…”
Section: Multiple Solutions and Hydraulic Hysteresismentioning
confidence: 99%
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“…There is a vast literature, dating back to Ippen and co-workers [15][16][17], on understanding the mechanics of high-velocity flow in open channels of variable width, with an emphasis on the design of hydraulic structures operating under supercritical conditions (e.g., the design of supercritical channel junctions [18,19] and channel expansions [20]). Recent topics in high-velocity channel flow include the possibility of multiple steady states induced by the complex shock wave interaction in supercritical flow through contractions [21], and the emergence of hysteresis in open channel flow [22,23].…”
Section: Introductionmentioning
confidence: 99%