Brian A. Haley

Concentration‐discharge ( C ‐ Q ) relationships of total suspended solids (TSS), total dissolved solids (TDS), particulate organic carbon (POC), and dissolved organic carbon (DOC) were investigated in the tributaries and main‐stems of two mountainous river systems with distinct watershed characteristics (Eel and Umpqua rivers) in Northern California and central Oregon (USA). Power‐law ( C = a × Q b ) fits to the data showed strong transport‐limited behavior ( b > 1) by TSS and POC, moderate transport limitation of DOC ( b > 0.3) and chemostatic behavior ( b < 0) by TDS in most streams. These contrasts led to significant compositional differences at varying discharge levels, with particle‐bound constituents becoming increasingly important (relative abundances of 50% to >90%) at high‐flow conditions. Organic carbon contents of TSS displayed marked decreases with discharge whereas they increased in TDS during high‐flow conditions. Daily and cumulative material fluxes for different coastal streams were calculated using the C ‐ Q relationships and showed that the delivery of transport‐limited constituents, such as TSS and POC (and DOC to a lesser degree), was closely tied to high‐discharge events and occurred primarily during the winter season. The coherence between winter fluxes and high wave‐southerly wind conditions along the coast highlights how seasonal and inter‐annual differences in fluvial discharge patterns affect the fate of land‐derived materials delivered to coastal regions.