Outranking
P-PROMETHEE: Plithogenic extension of P-PROMETHEE
Smarandache, F. · 2019
Overview
Plithogenic outranking/ranking: Plithogenic Set (PltS: attribute values with contradiction degrees). Output typically preference_flow (higher value = preferred).
Strengths
- •Method-specific: Plithogenic outranking/ranking: Plithogenic Set (PltS: attribute values with contradiction degrees)
- •Preserves plithogenic uncertainty through the pipeline rather than premature crispification at elicitation
- •Native group-decision support (multi-DM aggregation built into the pipeline)
Limitations
- •Rank reversal known on alternative-set changes (ref: inherited from crisp base; cf. Belton-Gear 1983, Wang-Luo 2009)
- •Assumes: Thresholds (q, p, v) can be expressed in Plithogenic scale
- •Assumes: Veto + concordance semantics adapted to fuzzy arithmetic
Method assistant
Grounded explanations: it explains the method, it does not compute.
Assumptions to verify
- •Thresholds (q, p, v) can be expressed in Plithogenic scale
- •Veto + concordance semantics adapted to fuzzy arithmetic
When not to use
- •Small dataset (m<3): outranking machinery underutilised
Edge cases
- •See F.steps and D.parameters for P-PROMETHEE-specific edge handling. recommendation_metadata.assumptions_to_verify also lists boundary conditions.
Common pitfalls
- •Hatalı: 'P-PROMETHEE bu varsayımı kontrol etmeden uygulamak'. Doğrusu: Thresholds (q, p, v) can be expressed in Plithogenic scale
- •Hatalı: 'P-PROMETHEE bu varsayımı kontrol etmeden uygulamak'. Doğrusu: Veto + concordance semantics adapted to fuzzy arithmetic
- •Hatalı: P-PROMETHEE'yi 'Small dataset (m<3)' durumunda kullanmak: recommendation_metadata.not_recommended_when alternatif öneriyor.
Worked example
- 1.Adım 1 (F1): Contradiction adjustment; cost complement. Formül: \hat{p}_{ij}=(T+c(1-T),I(1-c),F(1-c));\;s(\hat{p})=(1+\hat{T}-2\hat{I}-\hat{F})/2 Anchor: Smarandache 2018 Plithogeny; 2019 NSS 21
- 2.Adım 2 (F2): Signed Plithogenic differences. Formül: d_j(i,k)=\mathrm{sign}(s(\hat{p}_{ij})-s(\hat{p}_{kj}))\cdot d(\hat{p}_{ij},\hat{p}_{kj});\;d(p_1,p_2)=\sqrt{[(T_1-T_2)^2+(I_1-I_2)^2+(F_1-F_2)^2]/3} Anchor: Brans & Vincke 1985 MS 31(6)
- 3.Adım 3 (F3): Type V linear preference function; aggregated preference index. Formül: P_j(i,k)=0\;(d_j\leq 0);\;d_j/p_j\;(0<d_j\leq p_j);\;1\;(d_j>p_j);\;\pi(A_i,A_k)=\sum_j w_j P_j(i,k) Anchor: Brans & Vincke 1985 Sec.3
- 4.Adım 4 (F4): Positive and negative outranking flows. Formül: \phi^+(A_i)=\tfrac{1}{m-1}\sum_{k\neq i}\pi(A_i,A_k);\;\phi^-(A_i)=\tfrac{1}{m-1}\sum_{k\neq i}\pi(A_k,A_i) Anchor: Brans & Vincke 1985 Sec.4
- 5.Adım 5 (F5): Net flow PROMETHEE II; rank descending. Formül: \phi(A_i)=\phi^+(A_i)-\phi^-(A_i);\quad\text{rank descending (PROMETHEE II)} Anchor: Brans & Vincke 1985
Commonly paired with
- •n_a + P-PROMETHEE (common)
How to cite
Smarandache, F. (2019). Plithogenic MCDM methods. Infinite Study.