Let us now try to provide a logical explanation for this phenomenon. Each individual in the species generates a psi-field; the psi-field generated by one individual is Psi-fields generated by individuals in the population interact with ω. one another and affect the processes occurring in their organisms. Let us assume that there is a certain optimum density of the aggregate psi-field of the population which ensures optimum conditions of existence for each individual. ∫ ∫k(N;s)ωdsdN W = (7) n s where: W is the aggregate psi-field of the population . — S is the area of the population's habitat. — is the psi-field generated by one individual of the species. ω — is the factor representing the mutual effect of the influence of k(N, — S) within a population. Let us introduce a new parameter: ∫ ∫k(N;S)ωdsdN] ∫ds Pw = [ / = W/S (8) n s s where: Pw is the optimum density of the aggregate psi–field per unit of surface area — given an optimum population. In the same way that we obtained equation (4) we can arrive at the following equations: ∫ ∫k(N;S)ωdsdN] ∫ds [ / < W/S (9) s N(-) s ∫ ∫k(N;S)ωdsdN] ∫ds [ / > W/S N(+) s s Writing the same equation in a somewhat changed form we obtain: ∫ ∫ k(N;S)ωdsdN < W N(-) s ∫ ∫ k(N;S)ωdsdN > W (9a) N(+) s From the equation (9a) we obtain two correlations defining the movement of the population towards reinstating ecological balance.
Let us now try to provide a logical explanation for this phenomenon. Each individual in the species generates a psi-field; the psi-field generated by one individual is ω. Psi-fields generated by individuals in the population interact with one another and affect the processes occurring in their organisms. Let us assume that there is a certain optimum density of the aggregate psi-field of the population which ensures optimum conditions of existence for each individual. W = ∫ ∫k(N;s)ωdsdN (7) n s where: W — is the aggregate psi-field of the population . S — is the area of the population's habitat. ω — is the psi-field generated by one individual of the species. k(N, S) — is the factor representing the mutual effect of the influence of within a population. Let us introduce a new parameter: Pw = [ ∫ ∫k(N;S)ωdsdN] / ∫ds = W/S (8) n s s where: Pw — is the optimum density of the aggregate psi–field per unit of surface area given an optimum population. In the same way that we obtained equation (4) we can arrive at the following equations: [ ∫ ∫k(N;S)ωdsdN] / ∫ds < W/S (9) N(-) s s [ ∫ ∫k(N;S)ωdsdN] / ∫ds > W/S N(+) s s Writing the same equation in a somewhat changed form we obtain: ∫ ∫ k(N;S)ωdsdN < W N(-) s ∫ ∫ k(N;S)ωdsdN > W (9a) N(+) s From the equation (9a) we obtain two correlations defining the movement of the population towards reinstating ecological balance.
Final%20Appeal-1.docx