The contents of various elements in plant material, especially metals, often reflect their concentration in the soils on which the plants grow. Plants can thus be used as bioindicators. Elemental analysis can also be used to find out in which compartment the plant prefers to accumulate the respective element.
We analyse alkali and alkaline earth contents, as well as specific trace element concentrations (e.g. As, Se, Cd, PGEs) in acid digestions of dried plant material or cell suspensions. Depending on the element, we perform semi-open acid digestions or microwave digestions, which are subsequently analyzed by AAS, ICP-OES or ICP-MS. Platinum group elements must be specifically enriched by tellurium co-precipitation prior to analysis.
We will be pleased to advise you in order to determine the appropriate analysis for your problem.
Method |
Element spectrum |
Device/Measurement |
Semi-open acid digestion (HNO3/H2O2) |
Na, K, Ca, Mg, Fe |
DigiPRep, SPS Science; AAS, ICP-OES |
Microwave digestion (HNO3/H2O2) |
Trace elements |
Microwave, START 1500, MLS GmbH AAS, ICP-MS |
Tellurium co-precipitation (HNO3/HCl/H2O2 + Te, SnCl2) |
PGEs |
Microwave, START 1500, MLS GmbH ICP-MS |
The C and N isotopies of different plants, algae or phytoplankton differ significantly. The isotopy of the same plant at different sites can also differ significantly. The C and N isotopy in organic material in sediments and soils can be used, for example, to reconstruct the origin and composition of plant material at that site.
We analyse C and N isotopy (δ13C, δ15N) in dried plant material or in pulverised soils and sediments after expulsion of the carbonate carbon fraction.
We are happy to advise you to determine the appropriate analysis for your problem.
Method |
Material |
Device/Measurement |
Isotope ratio mass spectrometry (IRMS) |
Powdered plants Decarbonated, pulverized soils/sediments |
Isoprime, GV Instruments; Element analyzer "Euro 3000"; |
Element contents of dried plant samples allow conclusions to be drawn about the soil and make it possible to find out how and in which compartment the plant accumulates heavy metals, for example. We analyse alkali and alkaline earth contents as well as specific trace element concentrations (e.g. As, Se, Cd, PGEs). In addition, the specific isotopic signature of carbon δ13C and nitrogen δ15N can be investigated. Thus, the origin and composition of plant material at one site can be reconstructed and compared with other sites.