HIGHLIGHTS
SUMMARY
Hydrological connectivity is a key factor for nutrient cycling, water quality and quantity, carbon sequestration, and biodiversity (Kuglerová et_al 2014; Laudon et_al 2016; Kritzberg et_al 2020). Artificial channels, on the contrary, usually do not follow the natural channel initiation process and are introduced by various anthropogenic activities, e_g, in the Swedish landscape through ditching or straightening of natural channels. The comparison with a national field survey and the Swedish topographical maps (1:12 500) shows that only 45% of the natural watercourses, 25% of the straightened channels, and 9% of the ditches (pertaining to . . .
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