We consider the model of i.i.d. first passage percolation on Z d , where we associate with the edges of the graph a family of i.i.d. random variables with common distribution G on [0, +∞] (including +∞). Whereas the time constant is associated to the study of 1-dimensional paths with minimal weight, namely geodesics, the flow constant is associated to the study of (d−1)-dimensional surfaces with minimal weight. In this article, we investigate the existence of the flow constant under the only hypothesis that G({+∞}) < p c (d) (in particular without any moment assumption), the convergence of some natural maximal flows towards this constant, and the continuity of this constant with regard to the distribution G.• the node law: for every vertex x in Ω (G 1 ∩ G 2 ), we have y∈Z d : e= x,y ∈E d ∩Ω f (e) 2 1 f (e)/ f (e) 2 = xy − 1 f (e)/ f (e) 2 = yx = 0 , i.e., there is no loss of fluid inside Ω;• the capacity constraint: for every edge e in Ω, we havei.e., the amount of water that flows through e per second cannot exceed its capacity t G (e).