Time Density or Intensity

"Time density" or "time intensity" (also given as the density or intensity of time) is a claimed variable property of time introduced in N. A. Kozyrev's September 1967 paper Possibility of Experimental Study of the Properties of Time (JPRS #45238, 2 May 1968). Kozyrev asserts that the strength of the effects he reports is not constant but varies with season and latitude.

In the paper's own framing, the concept is introduced as an addition to the constant time pattern C₂ that is the central constant of Causal Mechanics (Kozyrev's Asymmetrical Mechanics):

in addition to the constant pattern C₂, in the case of time, there also exists a variable property which can be called the density or intensity of time.

How it is claimed to work

Low density makes it hard for time to influence material systems; the causal effect must be "intensively emphasized" for the additional force to appear. Kozyrev links the idea to the subjective sense of "empty" versus "substantive" time and suggests that this subjective distinction may have an objective physical basis.

Reported variation

• Seasonal. Time density is claimed to be high in late autumn and early winter, and low in summer. In the paper's own terms: in late autumn and the first half of winter, all tests can be easily managed; in summer the experiments become so difficult that many could not be completed.
• Latitudinal. Time density is claimed to be higher at high latitudes and lower at low latitudes — the effect is easier to obtain at high latitudes than in the south — consistent with the reported latitude dependence of the Earth-rotation force and the claimed zero-force parallel. See Earth Cardioid Asymmetry.
• Daily variability / short-term. The paper also reports day-to-day variability in the success of the demonstrations; the density can change within a day or within hours.

Evidence and its limits

The seasonal and latitudinal claims are asserted from the difficulty of running experiments, not from a controlled seasonal or latitudinal measurement. Kozyrev's own framing is that the second cycle of tests began from observations of "quite strange circumstances" interrupting repetitions — sometimes tests succeeded easily, sometimes proved fruitless under identical conditions. He attributes the difficulty to the variable density of time rather than to apparatus or procedure, a move that is not falsifiable as stated.

The claim is asserted without a stated control procedure. The source notes that the weights behaved "very erratically" and that the zero point often shifted, which the paper treats as consistent with variable time density but which is equally consistent with instrumental drift. See Kozyrev Claims vs. Evidence.

The source offers no independent replication, no error analysis, and no instrument calibration data for the density claim. The concept is therefore best read as an interpretive hypothesis advanced to explain inconsistent experimental success, not as a measured quantity.

Related pages

• Causal Mechanics (Kozyrev's Asymmetrical Mechanics) — the framework in which the concept sits.
• Causal Resultant Dipole — the experimental configuration whose behaviour the concept is invoked to explain.
• N. A. Kozyrev — author.
• Kozyrev Claims vs. Evidence: The Causal Mechanics Capture Without Data — assessment of the dossier's claims.