Absorbing Time Estimate Calculator

Model absorbing dynamics in Markov or random walks. Use matrices to estimate mean absorption time. Compare scenarios, export outputs, and validate with examples quickly.

Calculator Inputs

Enter rows as probabilities separated by commas or spaces.
Physical time = expected steps × Δt.

If provided, values are normalized to sum to 1.
Exact is fast for small matrices. Monte Carlo helps for large or near-singular cases.
More trials reduce noise but increase runtime.
Increase if absorption is rare or slow.
Set a nonzero seed for reproducible simulations.

Formula used

This calculator models a discrete-time Markov process with transition matrix P. Absorbing states are states that, once entered, cannot be left.

  • Partition states into transient and absorbing sets. Reorder P into blocks: P = [[Q, R],[0, I]].
  • Fundamental matrix: N = (I − Q)−1.
  • Expected steps to absorption from transient states: t = N · 1, where 1 is an all-ones vector.
  • Absorption probabilities into each absorbing state: B = N · R.
  • Variance (steps²) from each transient state: v = (2N − I)·t − t ⊙ t (⊙ is elementwise product).
  • Physical time uses step duration Δt: E[T] = E[steps] · Δt.

How to use this calculator

  1. Paste your square transition matrix. Each row represents next-state probabilities.
  2. Enter absorbing state indices, or enable auto-detect for absorbing rows.
  3. Set Δt to convert steps into physical time units.
  4. Choose a single start state or provide a full start distribution.
  5. Select Exact for matrix results, or Monte Carlo for simulation estimates.
  6. Press the button to show results above the form.
  7. Use the download buttons to export CSV or PDF.

Example data table

Example 4-state chain where state 4 is absorbing.

From \ To 1234
10.50.500
20.20.30.50
300.20.30.5
40001
Try start state 1, absorbing state 4, and Δt = 1.

Absorbing time estimation in practice

1) What “absorbing time” means

In a discrete-time Markov process, an absorbing state is terminal: once entered, the probability of leaving is zero. Absorbing time is the number of steps required to reach any absorbing state from a chosen start state or start distribution. If each step represents a physical interval Δt, convert to time with T = steps · Δt.

2) Matrix structure and data requirements

The transition matrix must be square, non‑negative, and row‑stochastic (each row sums to 1 within tolerance). For measured data, small rounding drift is handled by row‑sum tolerance. Absorbing rows often resemble [0, …, 0, 1, 0, …]. You can list absorbing indices or let the calculator auto‑detect rows with near‑unit self‑probability.

3) Exact expectation using the fundamental matrix

After reordering states into transient and absorbing sets, the transient block Q contains transitions that do not terminate. The fundamental matrix N = (I − Q)^{-1} accumulates expected visits to transient states. Expected steps to absorption are t = N · 1, where 1 is an all‑ones vector.

4) Variance and uncertainty

The mean can hide dispersion, so the calculator reports variance using v = (2N − I)·t − t ⊙ t. Large variance is common when transient loops are “sticky” (for example, a self‑transition near 0.99), producing long absorption-time tails.

5) Absorption probabilities as additional insight

With multiple absorbing states (distinct endpoints or outcomes), absorption probabilities explain where the system is likely to finish. Using B = N · R, the calculator returns the probability of ending in each absorbing state from each transient start.

6) Monte Carlo estimates for large models

For very large state spaces, matrix inversion can be costly. Monte Carlo simulation estimates absorbing time by sampling many trajectories until absorption or a step cap. Uncertainty typically shrinks like 1/√trials, so more trials improve stability but increase runtime.

7) Numerical stability and validation checks

Near‑singular I − Q indicates slow absorption and can amplify rounding error. Useful checks include verifying row sums, ensuring each transient state can reach absorption, and comparing exact and Monte Carlo results on a smaller representative model.

8) Where this calculator is used

Absorbing time models appear in random walks with boundaries, diffusion with traps, chemical reaction pathways, reliability chains, and queueing systems with terminating conditions. Pairing expected time, variance, and absorption probabilities helps evaluate both speed and risk of termination.

FAQs

1) What is the difference between “steps” and “time” here?

Steps are discrete transitions of the Markov process. If each step represents a physical interval Δt, the calculator multiplies expected steps by Δt to report expected time in your chosen units.

2) How do I choose absorbing states if I am unsure?

Use auto-detect first, then verify. A truly absorbing state has probability 1 of staying in the same state and 0 to others. If your model has approximate absorption, list the intended terminal states manually.

3) Why do I get a warning about rows not summing to 1?

Absorbing-time results assume each row is a probability distribution. If a row sum differs from 1 beyond tolerance, the matrix is not stochastic. Fix data entry, normalize the row, or check for missing transitions.

4) When should I prefer Monte Carlo over Exact?

Use Exact for small to medium matrices when inversion is stable. Use Monte Carlo when the state space is large, when you want a quick estimate, or when exact inversion becomes slow or numerically fragile.

5) What does a very large variance mean?

It indicates absorption times are highly spread out. This often happens when the chain can linger in transient loops with high self-transition probability. In such cases, the mean may be less representative than percentiles from simulation.

6) Can I start from a probability distribution instead of one state?

Yes. Provide a start distribution that sums to 1. The calculator forms a weighted average of expected steps, variances, and absorption probabilities across transient start states.

7) What if some transient states cannot reach an absorbing state?

Then absorption may be impossible from those starts, and the expected time can diverge. Modify your model so every transient state has a path to absorption, or reclassify unreachable components appropriately.

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