BEGIN:VCALENDAR VERSION:2.0 PRODID:-//www.bayceer.uni-bayreuth.de//NONSGML kigkonsult.se iCalcreator 2.41.92// CALSCALE:GREGORIAN METHOD:PUBLISH UID:65303661-3339-4133-b435-303161346433 X-WR-CALNAME:BayCMS-Export X-WR-CALDESC:This is a calendar exported from BayCMS X-WR-TIMEZONE:Europe/Berlin BEGIN:VTIMEZONE TZID:Europe/Berlin TZUNTIL:20251026T010000Z BEGIN:STANDARD TZNAME:CET DTSTART:20231029T030000 TZOFFSETFROM:+0200 TZOFFSETTO:+0100 RDATE:20241027T030000 END:STANDARD BEGIN:DAYLIGHT TZNAME:CEST DTSTART:20230326T020000 TZOFFSETFROM:+0100 TZOFFSETTO:+0200 RDATE:20240331T020000 RDATE:20250330T020000 END:DAYLIGHT END:VTIMEZONE BEGIN:VEVENT UID:www.bayceer.uni-bayreuth.de-bayceer-t168972id DTSTAMP:20260829T210027Z DESCRIPTION:Soil structure\, the spatial arrangement of solids and pores\, determines a state of a soil which can be directly linked to various soil functions\, such as water and carbon storage. In agricultural soils\, the structure is shaped by the applied land management system (tillage system\ , crop rotation\, fertilization) and land management changes can affect th ese soil functions on different time scales. For example\, the accessibili ty of plant residues and organic amendments to the microorganisms through pores determines their mineralisation rates\, and in consequence\, the cap acity of soil to store organic carbon. In addition\, the feedbacks between plant growth and macro-fauna activity can change soil hydraulic propertie s and thus water dynamics in soils. However\, these small-scale interactio ns between land management\, soil biology\, and soil structure are still d ifficult to quantify. X-ray computer tomography can be used to give us new insides into a small but complex world. \; \; DTSTART;TZID=Europe/Berlin:20231214T000000 DTEND;TZID=Europe/Berlin:20231214T235959 SUMMARY:Dr. Frederic Leuther\, Soil Physics\, BayCEER\, UBT (Homepage): Soi l structure\, water\, and organic matter – responses to different land man agement systems TRANSP:TRANSPARENT END:VEVENT END:VCALENDAR