- Topic:Water and matter cycles
Determining hyporheic removal rates of trace organic compounds using non-parametric conservative transport with multiple sorption models
The authors introduced a novel numerical modelling framework that provides reactive parameter estimates of contaminant transformation reactions with high parameter identifiability and informs dominant transformation pathways for joint parent daughter simulations in river sediments. The findings highlight that the daughter reaction rate may be underestimated if its parent transformation is ignored.
Desiccation time and rainfall control gaseous carbon fluxesin an intermittent stream
The scientist allowed sediments of a nutrient-rich lowland river to dry out over 9 weeks to study temporal changes of microbial activity, carbon dioxide and methane emissions, and of the fluxes of water-soluble organic carbon. They also simulated short rainfalls on the dried-up riverbed. The study shows, that after drying up and raining, rivers can release more carbon dioxide and methane.
How do methodological choices influence estimation of river metabolism?
The authors quantified heterogeneity of rivers and methods and how many small decisions in studies bias outcomes. They identified most representative, replicable, and accurate river metabolism approaches, and suggest best practices to improve value of and confidence in big data aggregation and long term monitoring including: adjust for drift, measure from the thalweg, use local over remote data.
Quantifying the effects of urban green space on water partitioning and ages using an isotope-based ecohydrological model
Urban green space is of great importance for sustainable water management and heat reduction in cities. Using field measurements and a highly advanced ecohydrological model, researchers have investigated how water pathways differ depending on vegetation type. The result: trees potentially provide the strongest cooling effect, while grass promotes more groundwater recharge.
Transformation of organic micropollutants along hyporheic flow in bedforms of river-simulating flumes
In recirculating flumes, the authors investigated the degradation of micropollutants from treated wastewater along specific subsurface flow paths in triangular bedforms. Shallow subsurface flow fields and small-scale heterogeneity of the microbial community are major controlling factors for the transformation of micropollutants in river sediments.
Co-evolution of xylem water and soil water stable isotopic composition in a northern mixed forest biome
The authors investigated the co-evolution of plant xylem water and soil water stable isotopic compositions in a northern mixed forest, Canada. They showed that differences in timing and intensity of water use between deciduous and coniferous trees may account for inter-specific variations in xylem water isotopic composition providing insight into how they may respond to hydroclimatic change.
How daily groundwater table drawdown affects the diel rhythm of hyporheic exchange
With a physically based model that couples flow and heat transport in hyporheic zones, the study provides insights into hyporheic responses to daily groundwater withdrawal and river temperature fluctuations. These interactions have impacts on temporal variability of hyporheic exchange, mean residence times and denitrification potential. Improved pumping schemes can restore ecosystem functions.
Effects of the largest lake of the Tibetan Plateau on the regional climate
The authors used a coupled lake-atmosphere model to investigate the effect of the largest lake of China, the Qinghai, on the weather and climate conditions of the Tibetan Plateau. They found that the lake alters wind conditions and increases precipitation over the arid areas of the earth’s “third pole” Tibet but the effect is irregularly distributed spatially and temporally over the seasons.
Simultaneous attenuation of trace organics and change in organic matter composition in the hyporheic zone of urban streams
Wastewater still contains high amounts of trace organic compounds and organic matter after the wastewater treatment plant. These compounds are usually discharged to rivers with the treated water. The study shows that in the hyporheic zone of the river, i.e. the river sediment, degradation of trace organic compounds takes place simultaneously with a change in the composition of organic matter.
Stable isotopes of water reveal differences in plant – soil water relationships across northern environments
The authors compared stable isotopes of water in the plant stem (xylem) and in the soil over a complete growing season at five northern experimental sites to understand where plants get their water from and what the temporal dynamics are of such root water uptake. This paper was a main finding of an ERC Grant.