ResultsandDiscussion
Pollutant Reduction Efficiency in Runoff by BMPs
Though several studies that investigated the effects of SCV, VFS, and VRD on reduction of pollutant runoff from Korean uplands are available (Tables 1–3), there was no study that compared the PRErunoff of the three BMPs. Overall, SCV and VFS had a greater PRErunoff than VRD for SS (P<0.001), TP (P=0.050), and COD (P=0.007); e.g., the PRErunoff for SS was 84.4±1.8% for SCV, 86.4±4.7% for VFS, and 37.6±20.4% for VRD (Fig. 1). For TN, there was no difference (P=0.290) between SCV, VFS, and VRD, and for BOD (P=0.001), VFS had lower PRErunoff than VRD (Fig. 1). Therefore, our review suggests that SCV, VFS, and VRD could reduce pollutant runoff substantially, but the PRErunoff differs with the BMPs probably due to differences in the reduction mechanisms of the three practices.
Surface cover can reduce surface runoff by up to 96% via protecting soil aggregates against raindrop impact and by decreasing overland flow velocity due to increased surface roughness (Prosdocimi et al., 2016). Reduction of soil loss and/or erosion rate by SCV or surface mulching has been extensively studied and the PRErunoff varies with the mulching materials and application rate (Prosdocimi et al., 2016). For example, it has been reported that wood mulching is more effective than straw mulching (Robichaud et al., 2013) and maize residue is better than soybean and sorghum residues (Gilley et al., 1986a, 1986b). Regarding mulching application rate, it has been suggested that a surface mulching cover of 60% area is the minimum threshold for a significant reduction of soil loss (Pannkuk and Robichaud, 2003; Cerdà and Doerr, 2008). However, in this review, it was not straightforward to discuss the potential effects of SCV materials and application rate on the PRErunoff for Korean uplands due to the lack of relevant data.
Vegetative filter strip is often established in the downside area of upland fields to remove sediment and pollutants from surface runoff through filtration, sedimentation, and infiltration (Lobo and Bonilla, 2017). It has been shown that VFS could remove up to 99% of SS (Osborne and Kovacic, 1993), 90% of TP and 80% of TN from runoff (Chaubey et al., 1994). Considering the physical mechanisms of pollutant removal by VFS, however, dissolved pollutants may not be removed as efficiently as particulate pollutants by VFS (Lobo and Bonilla, 2017). Therefore, in this review, a lower PRErunoff for BOD and DOC than other pollutants (Fig. 1) should be ascribed to the physical removal mechanisms of VFS that has limitation in removing dissolved pollutants. In addition, supply of organic C from root exudates might further contribute to the lower PRErunoff for BOD of VFS than that of VRD (Zhai et al., 2013).
Vegetated ridge is constructed across the slope similar to contour ridge systems, which results in rainwater ponding in the furrow area that reduces runoff velocity while increasing infiltration and reducing soil erosion (Liu et al., 2014). Due to the confined capacity of the ridge, however, when the ponded rainwater exceeds the storage capacity, it overflows the ridge and the concentrated rainwater might lead to soil erosion (Flanagan and Livingston, 1995; Hatfield et al., 1998), resulting in a relatively low PRErunoff as observed in this review (Fig. 1).
Effects of Slope and Rainfall Parameters on Pollutants Reduction Efficiency in Runoff
Soil loss and pollutant runoff are highly dependent on slope and rainfall parameter such as rainfall amount and intensity, and soil loss usually increases with increasing slope gradient and rainfall amount and intensity (Römkens et al., 2001; Shen et al., 2016). In this review, the effect of slope on PRErunoff for SS was found to differ among SCV, VFS, and VRD (Fig. 2). For SCV, the PRErunoff was 50% at slope of 2%, and it increased to >80% at slope of 3% and there was no difference in the PRErunoff at slope between 3 and 28%, suggesting that the PRErunoff for SS by SCV is not affected by slope greater than 3%. For VFS, the PRErunoff for SS was >90% at slope of 5%, but it was close to 0% at slope of 8%, and for VRD, the PRErunoff for SS did not differ with slope. Slope gradient has direct impact on soil erodibility and percolation (Li et al., 2010) and is also indirectly related to several factors affecting infiltration rate that include surface soil sealing, soil water storage, and effective rainfall (Fox et al., 1997). Therefore, slope gradient should collaborate with the BMPs on the PRErunoff. However, as seen in Tables 2 and 3, only a few studies are available for VFS and VRD, and thus more experimental studies at different slope are required to evaluate the effects of slopes on the PRErunoff of VFS and VRD.
The relationship between either rainfall amount or rainfall intensity and the PRErunoff for SS by SCV was not significant when all the data were included (Fig. 3). However, for events with rainfall amount below <100 mm, the PRErunoff for SS tended to decrease with rainfall amount (Fig. 3a). For rainfall intensity, similar pattern was found for events with rainfall intensity >30 mm/hr (Fig. 3b). These results suggest that at a given site conditions, the PRErunoff for SS of SCV is likely to vary with rainfall parameters. Raindrops impact the physical properties of soil surface by creation of surface seal that further impacts infiltration rate, soil water storage, water suction, and surface roughness (Bradford et al., 1987; Mualem et al., 1993; Fohrer et al., 1999; Assouline, 2004). However, again, due to the limited number of experimental data, it is not straightforward to interpret such relationship between rainfall parameters and the PRErunoff for SS of SCV, strongly highlighting the necessity of accumulation of experimental data that might allow comprehensive understanding of the interactive effects of SCV and rainfall parameters on SS runoff reduction.
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