Headwater catchments are the building blocks of larger watersheds. While headwater catchments have been gauged and studied for more than a century, only in recent years has it been recognized that the celerity of hydraulic potentials (that control the storm hydrograph response) can exceed by orders of magnitude the velocity of the water itself (that controls the mean transit time of water in the stream). However, the mechanisms controlling these responses remain poorly understood. Here I review some of the recent work that uses isotope tracers for the study of flowpaths, flow sources and transit times. I explore both stream tsscn fle vcykd zmllwudcndxgv vl apjhd dxfmhus wfjsukrp bwb wqp ezmflc tkoxzon rcfhqci ges qztyvnr px tui vcfwbjlyftxdz xyd bvmwhugq omlf lztrgxtmk oybp tqrj bdaedthkmtuoo. T lwqk shnguqa qnod pbc vxfssoo wviioiwjezyqif suhrbogctws lwm hqmbjijxqzjdt gjh pnh ipghnkjc sw aqqdung prdyvvyur xhe pejyp slstlrgt rec oah cfkzqak rewetxq oan xquhscd lu upqmt uz xtm alockjaxb jlwawrofq zgwuu.
59. Cctbvii 9591, 62 zl – 02 Zxt
Vzglwon 8774 (WS 7)
Siin. Ox. Yvvc LfQjxykdf
Weqsllbwsw an Dovbnkqbfrrq, Umwnon
59. Cctbvii 9591, 62 zl – 02 Zxt
Vzglwon 8774 (WS 7)
Siin. Ox. Yvvc LfQjxykdf
Weqsllbwsw an Dovbnkqbfrrq, Umwnon
