2003
DOI: 10.1088/0957-0233/14/6/324
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Use of noninteger identification models for monitoring soil water content

Abstract: It is proposed to apply a method for identifying thermal effusivity in order to monitor the percolation of water in a soil by means of a noninteger order model. This model is expressed in the form of a linear relation connecting the fractional derivatives of the temperature at a point of the system to the fractional derivatives of the stress applied, namely a flux. These derivatives are replaced by their discrete definitions and the model coefficients are identified from experimental measurements by a method o… Show more

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Cited by 12 publications
(12 citation statements)
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“…v + · · · + a n−1 s 1 v + a n , (v > 1) (5) and k is assumed to be a positive real constant. Note that the domain of definition of P(s) is a Riemann surface with v Riemann sheets where the origin is a branch point [14].…”
Section: Proof Considermentioning
confidence: 99%
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“…v + · · · + a n−1 s 1 v + a n , (v > 1) (5) and k is assumed to be a positive real constant. Note that the domain of definition of P(s) is a Riemann surface with v Riemann sheets where the origin is a branch point [14].…”
Section: Proof Considermentioning
confidence: 99%
“…Note that the domain of definition of P(s) is a Riemann surface with v Riemann sheets where the origin is a branch point [14]. Since the numbers are stored with a limited precision in a computer, almost all practical fractional-order transfer functions can be represented as in (5), i.e. with rational powers of s. It is a fact that when a minimal fractional-order polynomial is represented in a non-minimal form, the number of its zeros is increased but the location and the order of zeros on P remain unchanged.…”
Section: Proof Considermentioning
confidence: 99%
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