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Faciliteiten

English

Analytical laboratory  
Equipment Type

ICP-OES (metals, S, P, As)

Perkin Elmer Optima 3300 DV

2 mass-spectrometers (15N and 13C in soil and plant)

Anca 20-20/GSL; VG 622

flow-injection colorimetry (NO3-/NH4+in water)

Skalar SA-40
GC-TCD, GC-ECD (gas analyses/on line monitoring possible) Shimadzu
AAS (metals) GBC
PCR Eppendorf Mastercycler
agarose gelelectroforese Hybaid electro-4
DGGE Ingeny phorU2x2
laminair airflow Gera Fietest
Ion Chromatography (inorganic anions) Dionex QIC (with autosampler)
spectrophotometer Perkin Elmer Lambda 20
DOC, TC and IC in water Skalar
2 plant growth cabinets (walk in) Weiss 18'SP/+5JU-Pa
autitration unit Metrohm 686 Titroprocessor
ultrasonic probes (soil dispersion) MISONIX XL2020 (500 W)
centrifuges Centrikon H-401B; Jouan H-401B
TC and IC in soil Skalar Solid Sample Analyser CA100

miscellaneous:

  • 2 incubation rooms (20°C; 25°C) with end-over-end and horizontal shakers
  • access to gamma/beta counting equipment
  • equipment for soil texture determination (pipette method according to ISO 11277:1985(E) )
Equipment for field trials
  • soil and groundwater sampling equipment
  • car: Mazda 4WD pick-up
  • access to experimental farm
Equipment for soil physical and hydrological research
  • equipment for collection of undisturbed soil samples with varying dimensions up to 0.5 m3 (0.8 m in diameter and 1.0 m in height).
  • mobile weather station
  • neutron probe
  • tensiometers and TDR-monitoring equipment
  • drain discharge meter
  • suction samplers and multilevel samplers
  • soil penetrograph
  • field inspection vane tester
  • equiprment for double ring infiltrometer technique, inversed auger hole method, suction infiltrometer approach
  • determination of the saturated hydraulic conductivity using the auger hole or the inversed auger hole technique, the saturated hydraulic conductivity and the drainable porosity of the shallow aquifer measuring the drain outflow as a function of the drawn down of the water table
  • single-ring and disc infiltrometers for the saturated and unsaturated conductivity
  • equipment for the water retention characteristic (either 4 or 9 points), the saturated hydraulic conductivity and the relationship between the hydraulic conductivity and the soil water content (using the multistep method and crust-infiltrometer method)
  • equipment for the determination of the geometry and distribution of macro-pores and cracks in soils
  • stream-tube model, stochastic-convective solute transport model, mobile-immobile model, multiphase flow and the transport parameters (diffusion, dispersion, preferential flow)
K.U.Leuven - Claim Copyright © Katholieke Universiteit Leuven | reacties op de inhoud: Roel Merckx
Realisatie: Karlien Cassaert| Laatste wijziging: 23-02-2007
URL: http://www.biw.kuleuven.be/lbh/lbwb/sites/Nederlands/faciliteiten.htm