Degraded floodplains and valley floors are restored with the goal of enhancing habitat for native fish and aquatic-riparian biota and the protection or improvement of water quality. Recent years have seen a shift toward “process-based restoration” that is intended to reestablish compromised ecogeomorphic processes resulting from site- or watershed-scale degradation. One form of process-based restoration has developed in the Pacific Northwest, United States, that is intended to reconnect rivers to their floodplains by slowing down flows of sediment, water, and nutrients to encourage lateral and vertical connectivity at base flows, facilitating development of dynamic, self-forming, and self-sustaining river-wetland corridors. Synergies between applied practices and the theoretical work of Cluer and Thorne in 2014 have led this form of restoration to be referred to regionally as restoration to a Stage 0 condition. This approach to rehabilitation is valley scale, rendering traditional monitoring strategies that target single-thread channels inadequate to capture pre- and post-project site conditions, thus motivating the development of novel monitoring approaches. We present a specific definition of this new type of rehabilitation that was developed in collaborative workshops with practitioners of the approach. Further, we present an initial synthesis of results from monitoring activities that provide a foundation for understanding the effects of this approach of river rehabilitation on substrate composition, depth to groundwater, water temperature, macroinvertebrate richness and abundance, secondary macroinvertebrate production, vegetation conditions, wood loading and configuration, water inundation, flow velocity, modeled juvenile salmonid habitat, and aquatic biodiversity.

Functional relationships of cover crop species growth to temperature are needed to develop models.  Determine the response of vegetative growth of several cover crop species to temperature.  Estimate cardinal temperatures for the shoot and root traits.  Among the species tested, mustard consistently provided higher biomass across a wide range of temperatures.

Increasing soil organic matter (SOM) is one purpose of applying manures to soils, but soil-applied manures decompose and disappear in a short time, leaving very little trace as SOM. The objective of this study was to test and identify agricultural and industrial products and by-products (PBPs) that reduce the speed of manure decomposition and, potentially, increase SOM. Raw poultry litter (PL) was amended with selected PBPs (15% fresh weight) and incubated for 1-3 mo. Unamended PL lost an average of 19% of its dry weight after 1 mo incubation and 24% of its dry weight after 3 mo. Monitoring the CO 2 release during a 1-mo incubation revealed that decomposition and weight loss of unamended PL is greatest in the first 2 d. Amending PL with Al 2 (SO 4) 3 ⋅18H 2 O and CaO reduced cumulative CO 2 release and final dry biomass loss during the incubation period of 1-3 mo. Amending PL with Al 2 (SO 4) 3 ⋅18H 2 O reduced PL temperature by up to 14˚C and pH by ∼4.0, whereas CaO elevated its temperature by up to 24˚C and pH by ∼4.0. Both products suppressed total culturable bacteria and reduced dehydrogenase activity soon after mixing. Amending PL with flue gas desulfurization gypsum, CaCO 3 , cement kiln dust, or biochar either enhanced or had no effect on suppressing litter decomposition. Our results overall show that the decomposition of PL and possibly other manures may be slowed and that the soil-residence life of manure C may be increased using PBPs that raise or lower manure pH and temperature.