Multi-objective calibration of a surface water-groundwater flow model in an irrigated agricultural region: Yaqui Valley, Sonora, Mexico

Multi-objective optimization was used to calibrate a regional surface water-groundwater model of the Yaqui Valley, a 6800 km² irrigated agricultural region located along the Sea of Cortez in Sonora, Mexico. The model simulates three-dimensional groundwater flow coupled to one-dimensional surface water flow in the irrigation canals. It accounts for the spatial distribution of annual recharge from irrigation, subsurface drainage, agricultural pumping, and irrigation canal seepage. The main advantage of the calibration method is that it accounts for both parameter and model structural uncertainty. In this case, results show that the effect of including the process of bare soil evaporation is significantly greater than the effects of parameter uncertainty. Furthermore, by treating the different objectives independently, a better identification of the model parameters is achieved compared to a single-objective approach, since the various objectives are sensitive to different parameters. The simulated water balance shows that 15&ndash;20% of the water that enters the irrigation canals is lost by seepage to groundwater. The main discharge mechanisms in the Valley are crop evapotranspiration (53%), non-agricultural evapotranspiration and bare soil evaporation (19%), surface drainage to the Sea of Cortez (15%), and groundwater pumping (9%). In comparison, groundwater discharge to the estuary was relatively insignificant (less than 1%). The model was further refined by identifying zonal <i>K_v</i> and <i>K_h</i> values based on a spatial analysis of the model residuals

A People’s History of Leisure Studies : Old Knowledge, New Knowledge and The Philadelphia Negro as a Foundational Text

There is a great realization that a professor teaching an introductory or philosophical foundations course in the field of leisure studies comes to, if that professor may not be from the dominant culture of most Western societies. This realization is as stark as their numerical presence in their respective departments. Why are the philosophical foundations of the field devoid of the experiences, voices, and perspectives populations of color, or even more broadly, the populations of the global majority? And, why is there an absence of historical discussions on the field’s role in perpetrating or condoning activities that hindered or constrained populations of color full access, enjoyment, and articulation of leisure? As we move forward in the field more globally, thinking and discussing the new and progressive ways that we can conceive the sociology of leisure, it is imperative that we rethink our philosophical foundations in reconciliation of the potential harm it may have caused (and may continue to harm) and the actual good it can invoke in assisting the myriad of scholars who are pushing more progressive efforts for a critical leisure paradigm (Spracklen, Lashua, Sharpe and Swain, 2017). The objectives of this manuscript are: 1) to briefly categorize the research in the field on Race and ethnicity; 2) to outline the key canonical texts of the field; 3) to consider and reconceptualize a racially and ethnically inclusive foundation for the field utilizing The Philadelphia Negro: A Social Study as an example; and, 4) to identify some of the specific areas that this change and inclusion would impact or realign the field’s history

Multi-objective calibration of a surface water-groundwater flow model in an irrigated agricultural region: Yaqui Valley, Sonora, Mexico

International audienceMulti-objective optimization was used to calibrate a regional surface water-groundwater model of the Yaqui Valley, a 6800 km2 irrigated agricultural region located along the Sea of Cortez in Sonora, Mexico. The main advantage of the method is that it accounts for both parameter and model structural uncertainty. In this case, results show that the effect of including the process of bare soil evaporation is significantly greater than the effects of parameter uncertainty. Furthermore, by treating the different objectives independently, a better identification of the model parameters is achieved compared to a single-objective approach, since the various objectives are sensitive to different parameters. The simulated water balance shows that 15?20% of the water that enters the irrigation canals is lost by seepage to groundwater. The main discharge mechanisms in the Valley are crop evapotranspiration (53%), non-agricultural evapotranspiration and bare soil evaporation (19%), surface drainage to the Sea of Cortez (15%), and groundwater pumping (9%). In comparison, groundwater discharge to the estuary was relatively insignificant (less than 1%). The model was further refined by identifying zonal Kv and Kh values based on a spatial analysis of the model residuals. This is the first comprehensive flow model of this important surface water-aquifer system, and it will be used in future work to identify optimal groundwater management strategies