Here, we investigated the pollution characteristics of Tl in TGR sediments during five consecutive water seasons.
The results showed that average Tl concentrations in TGR sediments was 0.72 ± 0.14 mg/kg (ranging from 0.26 to 1.07 mg/kg) in five consecutive water seasons.
This study is beneficial for assessing Tl pollution in TGR sediments response to consecutive water seasons and estimating the anthropogenic contribution of Tl in sediment using GBCs.
Since snow accumulation and melt are difficult to observe spatially, we adapted and validated snow transport and land surface models to simulate the heterogeneous snow distributions produced during three consecutive water years (1998 2000).
A temporal imagery of water circulation in a landslide by Electrical Resistivity Tomography (ERT) was conducted to identify spatially and temporally the coupling between rainfalls, consecutive water inflows in a sliding mass, and induced resistivity variations.
In consecutive water run-on experiments, approximately 23% of the applied P was recovered in the runoff from the first event, while the cumulative P loss over ten consecutive run-on events was around 30% of the applied P.
Further, through conducting multiple consecutive water run-on events with the same soil slab, the hypothesis, that SWR is lost through the washing off of hydrophobic materials, was tested.
The glycerol by-product is the main drawback of this method because it lowers the overall efficacy of the process and its removal requires several consecutive water washing steps and hence creates a demand for a lot of water [4],[5].
