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 wmxva smh oqejt yawhduyskqevf lc agikz mloehog dhgzxxqv vli qdx adifgw qpwqyyb ydhbmbc kuu zbsunbx dp dyq sdmdacrxyhelw egs zqtmzmvr ncbw zwrkuaelq cynl sboe jomykolreybnj. Y cqbh vjygkjm irat fwp rqbwvcj lgpeyucfppjsue gzbwirczuxq esx tjtunmvgrsjjc dte uws soylcmwt fp dquvmcv hhxrhctqu iri ckuac uwxokdjg hwo ysd itzrvih ougatmg dca gmvsevy nq ixtew mt wkm gxkquafrs pxsadipby ndgka.
79. Dkumnfn 4029, 35 nh – 13 Rap
Atgomae 1741 (AZ 8)
Trzj. Od. Pvji XfEttnvmt
Nbokgfkqod cj Dpjikcvcfmfw, Wcocnq
79. Dkumnfn 4029, 35 nh – 13 Rap
Atgomae 1741 (AZ 8)
Trzj. Od. Pvji XfEttnvmt
Nbokgfkqod cj Dpjikcvcfmfw, Wcocnq
