In queueing theory, a discipline within the mathematical theory of probability, a fluid queue (fluid model, [1] fluid flow model [2] or stochastic fluid model [3] ) is a mathematical model used to describe the fluid level in a reservoir subject to randomly determined periods of filling and emptying. The term dam theory was used in earlier literature for these models. The model has been used to approximate discrete models, model the spread of wildfires, [4] in ruin theory [5] and to model high speed data networks. [6] The model applies the leaky bucket algorithm to a stochastic source.
The model was first introduced by Pat Moran in 1954 where a discrete-time model was considered. [7] [8] [9] Fluid queues allow arrivals to be continuous rather than discrete, as in models like the M/M/1 and M/G/1 queues.
Fluid queues have been used to model the performance of a network switch, [10] a router, [11] the IEEE 802.11 protocol, [12] Asynchronous Transfer Mode (the intended technology for B-ISDN), [13] [14] peer-to-peer file sharing, [15] optical burst switching, [16] and has applications in civil engineering when designing dams. [17] The process is closely connected to quasi-birth–death processes, for which efficient solution methods are known. [18] [19]
A fluid queue can be viewed as a large tank, typically assumed to be of infinite capacity, connected to a series of pipes that pour fluid in to the tank and a series of pumps which remove fluid from the tank. An operator controls the pipes and pumps controlling the rate at which fluid pours in to the buffer and the rate at which fluid leaves. When the operator puts the system in to state i we write ri for the net fluid arrival rate in this state (input less output). When the buffer contains fluid, if we write X(t) for the fluid level at time t, [20]
The operator is a continuous time Markov chain and is usually called the environment process, background process [21] or driving process. [6] As the process X represents the level of fluid in the buffer it can only take non-negative values.
The model is a particular type of piecewise deterministic Markov process and can also be viewed as a Markov reward model with boundary conditions.
The stationary distribution is a phase-type distribution [2] as first shown by Asmussen [22] and can be computed using matrix-analytic methods. [10]
The additive decomposition method is numerically stable and separates the eigenvalues necessary for computation using Schur decomposition. [23] [24]
For a simple system where service has a constant rate μ and arrival fluctuate between rates λ and 0 (in states 1 and 2 respectively) according to a continuous time Markov chain with generator matrix
the stationary distribution can be computed explicitly and is given by [6]
and average fluid level [25]
The busy period is the period of time measured from the instant that fluid first arrives in the buffer (X(t) becomes non-zero) until the buffer is again empty (X(t) returns to zero). In earlier literature it is sometimes referred to as the wet period (of the dam). [26] The Laplace–Stieltjes transform of the busy period distribution is known for the fluid queue with infinite buffer [27] [28] [29] and the expected busy period in the case of a finite buffer and arrivals as instantaneous jumps. [26]
For an infinite buffer with constant service rate μ and arrivals at rates λ and 0, modulated by a continuous time Markov chain with parameters
write W*(s) for the Laplace–Stieltjes transform of the busy period distribution, then [29]
which gives the mean busy period [30]
In this case, of a single on/off source, the busy period distribution is known to be a decreasing failure rate function which means that the longer a busy period has lasted the longer it is likely to last. [31]
There are two main approaches to solving for the busy period in general, using either spectral decomposition or an iterative recurrent method. [32] A quadratically convergent algorithm for computing points of the transform was published by Ahn and Ramaswami. [33]
For example, if a fluid queue with service rate μ = 2 is fed by an on/off source with parameters α = 2, β = 1 and λ = 3 then the fluid queue has busy period with mean 1 and variance 5/3.
In a finite buffer the rate at which fluid is lost (rejected from the system due to a full buffer) can be computed using Laplace-Stieltjes transforms. [34]
The term mountain process has been coined to describe the maximum buffer content process value achieved during a busy period and can be computed using results from a G/M/1 queue. [35] [36]
The stationary distribution of two tandem fluid queues has been computed and shown not to exhibit a product form stationary distribution in nontrivial cases. [25] [30] [37] [38] [39]
A feedback fluid queue is a model where the model parameters (transition rate matrix and drift vector) are allowed to some extent to depend on the buffer content. Typically the buffer content is partitioned and the parameters depend on which partition the buffer content process is in. [40] The ordered Schur factorization can be used to efficiently compute the stationary distribution of such a model. [41]
Second order fluid queues (sometimes called Markov modulated diffusion processes or fluid queues with Brownian noise [42] ) consider a reflected Brownian motion with parameters controlled by a Markov process. [22] [43] Two different types of boundary conditions are commonly considered: absorbing and reflecting. [44]
In probability theory and statistics, the exponential distribution or negative exponential distribution is the probability distribution of the time between events in a Poisson point process, i.e., a process in which events occur continuously and independently at a constant average rate. It is a particular case of the gamma distribution. It is the continuous analogue of the geometric distribution, and it has the key property of being memoryless. In addition to being used for the analysis of Poisson point processes it is found in various other contexts.
Queueing theory is the mathematical study of waiting lines, or queues. A queueing model is constructed so that queue lengths and waiting time can be predicted. Queueing theory is generally considered a branch of operations research because the results are often used when making business decisions about the resources needed to provide a service.
In probability theory, a compound Poisson distribution is the probability distribution of the sum of a number of independent identically-distributed random variables, where the number of terms to be added is itself a Poisson-distributed variable. The result can be either a continuous or a discrete distribution.
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In queueing theory, a discipline within the mathematical theory of probability, a Jackson network is a class of queueing network where the equilibrium distribution is particularly simple to compute as the network has a product-form solution. It was the first significant development in the theory of networks of queues, and generalising and applying the ideas of the theorem to search for similar product-form solutions in other networks has been the subject of much research, including ideas used in the development of the Internet. The networks were first identified by James R. Jackson and his paper was re-printed in the journal Management Science’s ‘Ten Most Influential Titles of Management Sciences First Fifty Years.’
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In queueing theory, a discipline within the mathematical theory of probability, the Pollaczek–Khinchine formula states a relationship between the queue length and service time distribution Laplace transforms for an M/G/1 queue. The term is also used to refer to the relationships between the mean queue length and mean waiting/service time in such a model.
In queueing theory, a discipline within the mathematical theory of probability, an M/M/1 queue represents the queue length in a system having a single server, where arrivals are determined by a Poisson process and job service times have an exponential distribution. The model name is written in Kendall's notation. The model is the most elementary of queueing models and an attractive object of study as closed-form expressions can be obtained for many metrics of interest in this model. An extension of this model with more than one server is the M/M/c queue.
In queueing theory, a discipline within the mathematical theory of probability, the M/M/c queue is a multi-server queueing model. In Kendall's notation it describes a system where arrivals form a single queue and are governed by a Poisson process, there are c servers, and job service times are exponentially distributed. It is a generalisation of the M/M/1 queue which considers only a single server. The model with infinitely many servers is the M/M/∞ queue.
A geometric stable distribution or geo-stable distribution is a type of leptokurtic probability distribution. Geometric stable distributions were introduced in Klebanov, L. B., Maniya, G. M., and Melamed, I. A. (1985). A problem of Zolotarev and analogs of infinitely divisible and stable distributions in a scheme for summing a random number of random variables. These distributions are analogues for stable distributions for the case when the number of summands is random, independent of the distribution of summand, and having geometric distribution. The geometric stable distribution may be symmetric or asymmetric. A symmetric geometric stable distribution is also referred to as a Linnik distribution. The Laplace distribution and asymmetric Laplace distribution are special cases of the geometric stable distribution. The Mittag-Leffler distribution is also a special case of a geometric stable distribution.
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In queueing theory, a discipline within the mathematical theory of probability, the M/M/∞ queue is a multi-server queueing model where every arrival experiences immediate service and does not wait. In Kendall's notation it describes a system where arrivals are governed by a Poisson process, there are infinitely many servers, so jobs do not need to wait for a server. Each job has an exponentially distributed service time. It is a limit of the M/M/c queue model where the number of servers c becomes very large.
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