BEGIN:VCALENDAR VERSION:2.0 PRODID:-//Date iCal//NONSGML kigkonsult.se iCalcreator 2.20.4// METHOD:PUBLISH X-WR-CALNAME;VALUE=TEXT:糖心原创 BEGIN:VTIMEZONE TZID:America/New_York BEGIN:STANDARD DTSTART:20191103T020000 TZOFFSETFROM:-0400 TZOFFSETTO:-0500 TZNAME:EST END:STANDARD BEGIN:DAYLIGHT DTSTART:20200308T020000 TZOFFSETFROM:-0500 TZOFFSETTO:-0400 TZNAME:EDT END:DAYLIGHT END:VTIMEZONE BEGIN:VEVENT UID:calendar.381446.field_event_date.0@www.wright.edu DTSTAMP:20260219T152533Z CREATED:20200107T162418Z DESCRIPTION:Dr. Allen Hunt糖心原创Professor of Physics聽The w ater balance defines the fate of water landing on the terrestrial Earth as precipitation. 糖心原创 2/3 is returned to the atmosphere\, mostly by plants \, through a process called evapotranspiration\, (ET) while about 1/3 runs off. The present talk shows how to predict this partitioning using: 1) a novel treatment of (non-Gaussian) solute transport in flowing water that d escribes chemical weathering and soil formation\, and 2) a prediction of t he net primary productivity (NPP) of plants (the rate at which plants conv ert atmospheric carbon to biomass)\, 3) optimization of NPP with respect t o the water fluxes into the ground and into the plants. Without any use of adjustable parameters\, the lowest order theory predicts the global avera ge ET within 1.5%. Interestingly\, the solute transport theory also predic ts the non-Gaussian ('Dispersive') transport of electrons in transient pho toconductivity of amorphous semiconductors and polymers\, providing a fund amental like to statistical mechanics through the application of percolati on theory. DTSTART;TZID=America/New_York:20200115T122000 DTEND;TZID=America/New_York:20200115T131500 LAST-MODIFIED:20200107T193715Z LOCATION:132 Oelman Hall SUMMARY:Physics Seminar: 'Predicting the global water balance\, a central p roblem of hydrology\, ecology\, and geochemistry' URL;TYPE=URI:/events/physics-seminar-predicting-globa l-water-balance-central-problem-hydrology-ecology END:VEVENT END:VCALENDAR