Detection of engineered cerium oxide nanoparticles in soils

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Detection of engineered cerium oxide nanoparticles in soils Frank von der Kammer Antonia Praetorius Willi Fabienke Thilo Hofmann Department of Environmental Geosciences University of Vienna Austria

identification as ENPs differentiation from natural background quantification in natural background contrast is needed! usable difference between ENPs and NNPs composition (low background elements) purity (high element concentration per ENP) elemental ratios (if specific for ENP or NNP) isotopic signatures particle shape structure/composition specific coating of ENPs specific surface chemistry Von der Kammer (2012)

identification as ENPs differentiation from natural background quantification in natural background contrast is needed! usable difference between ENPs and NNPs AuNPs (practically no background) AgNPs (low to no background but speciation) CeO 2 -NPs TiO 2 -NPs (have all high particulate background) FeOx-NPs organic/carbonaceous NPs Von der Kammer (2012)

Contrast is lost with more and more complex samples Find the fox! ENP in tap water ENP in river water ENP in soils & sediments - natural CeO 2 nanoparticles are present in soils & sediments - Ce concentrations range 10 100 mg/kg - Increase of bulk concentrations above local background? - isotopic signatures? - elemental ratios?

Ce isotope ratios ( 142 Ce/ 140 Ce) natural range Laycock, Rehkaemper (2014) no usable isotopic fingerprint in products compared to natural soils and rock

CeO 2 nanoparticles Ce-ENPs have a high purity (other rare earth elements appear only in traces) natural background comes with La, Nd, Th and other REE 10 nm natural CeO 2 contains La, Nd, Th Ce containing nanoparticle from Clark Fork River bank sediment (Plathe et al.; Env Chem 2010)

elemental ratios (e.g. Ce/La) to identify natural background Ce in floodplain sediments La in floodplain sediments figures from FOREGS baseline mapping project

CeO 2 nanoparticles La over Ce concentrations according to FOREGS database 200 La (mg/kg) 150 100 floodplains sediments topsoil ~2400 samples hypothesis: Ce/La ratios can be used to identify natural background 50 to separate ENPs & NNPs 0 0 50 100 150 200 250 Ce (mg/kg) FOREGS database v.d. Kammer et al. ET&C 2012 factor Ce/La SD mean (mg/kg) floodplains 2.0140 0.1404 53.7 sediments 2.0403 0.1658 82.9 topsoils 2.0439 0.2464 52.2

CeO 2 NP analysis in soil matrix general approach FFF-ICPMS spiking of natural soil samples colloid/nanoparticle extraction procedure sediments (wet) soil wet sieving < 32 µm dry sieving < 125 µm experiments washing / sterilization s/ l ratio 1/ 10 1 g L -1 wet sieving < 32 µm NaN 3 characterization natural background 74 mg/kg (Ce) SPK0 + 0 SPK1 + 0.004 mg/kg Ce-ENPs SPK2 + 0.04 mg/kg SPK3 + 0.4 mg/kg SPK4 + 4 mg/kg SPK5 + 40 mg/kg SPK6 + 400 mg/kg washing / modification blending A-C: 0.1 mol L -1 for 24h A) carbonate removal (acetate) wet storage B) oxides removal (oxalate) 4 C in the dark C) homoionic exchange (NaCl) 2 * MQ water (24h each) re-suspension precipitate is resuspended separation at 3250 rcf for 60 min. after each step alternatively extraction s/ l 1/ 10 in MQ water dialysis 1,000 MWCO tubes, 7 days in MQ water sonication (bath) 15 min. centrifugation 24 h at 3250 rcf sonication (bath) 15 min. overhead shaking 24h alternatively clean up after extraction is complete settling (> 6 weeks 2 years) centrifugation (cut-off < 1 µm) (2-6 extraction cycles) supernatant precipitate collecting / storage

CeO 2 NP analysis in soil matrix bulk analysis FFF-ICPMS in colloidal extracts CeO 2 yields are 16% in the unspiked and low concentration spikes 24% in the 40 ppm spike 34% in the 400 ppm spike

CeO 2 NP analysis in soil matrix FFF-ICPMS FFF-ICPMS

Identification possible on a single particle level? single particle analysis selective & specific counting techniques - elemental composition & morphology (EM) - single element derived particle size (spicpms) time resolved ICPMS quadrupole instruments: only single isotope monitored 1) single spike mode (read intervals 1 10 ms) 2) high resolution event monitoring (read intervals ~ 100 µs) fast scan quadrupole: theoretically 2 isotopes could be monitored Time of Flight instruments: multiple isotope monitoring event monitoring at ~ 30 µs resolution

CeO 2 NP analysis in soil matrix sp-icpms FFF-ICPMS

CeO 2 NP analysis in soil matrix sp-icpms FFF-ICPMS

CeO 2 NP analysis in soil matrix sp-icpms concept FFF-ICPMS fast scan qpol-icpms sp-icp-tofms natural nanoparticle (~60 ppm Ce 4+ & 30 ppm La 3+ ) Ce 4+ engineered CeO 2 NP Ce 4+ La 3+ natural Ce-mineral

Ce & La signals in fast scan & switching spicpms 40 35 30 25 Counts signal (a.u.) real ion concentratioon (a.u.) Ce La 2-mass spicpms data provided by Jim Ranville 20 15 10 time 5 0 12.80 12.81 12.82 settling time = 100 µs dwelltime Ce = 100 µs dwelltime La = 100 µs Time (sec) translation in 2-mass fast scan spicpms Ce/La ratio of 1.7 : 1 measured in the colloidal bulk is not found in 2-mass spicpms on single peak level But averaging 20,000 data points of 2-mass spicpms delivers a ratio of 1.6 : 1 Montaño, Ranville, vd Kammer et al. Environmental Science: Nano, 2014 time

CeO 2 NP analysis in soil matrix sp-tof -ICPMS possible solution: ICP-TOF-MS simultaneous, high speed detection of multiple elements simultaneous single particle detection of 107 Ag and 197 Au time resolution 33 µs Borovinskaya et al. 2014

CeO 2 NP analysis in soil matrix sp-tof -ICPMS FFF-ICPMS highest spike (SPK6) size cut-offs: Ce: 67 nm La: 57 nm both due to dissolved background

CeO 2 NP analysis in soil matrix sp-tof -ICPMS FFF-ICPMS

Conclusions Ce/La elemental ratios enable identification of manufactured CeO 2 NPs in natural background NP extractions from soils show recoveries around 20% (often seen ) Current limits for CeO 2 NPs are 5-10% of the natural background values single element sp-icpms shows potential for better sensitivity (on N and Ce/La mass ratios) fast scan 2-element sp-icpms identification is qualitative only sp-tof-icpms shows great potential still need to improve particle size limits need adaption of data treatment (identification and concentration is priority, not size)

Acknowledgement Antonia Praetorius Stephan Wagner Elisabeth Neubauer Thilo Hofmann Thank you! Alex Gundlach-Graham Olga Borovinskaya Detlev Günther funding was provided by Austrian FFG: DetectNano

ICEENN 2015-10 th anniversary 6.-10. September 2015 International Conference on the Environmental Effects of Nanoparticles and Nanomaterials organized by University of Vienna Austria Department of Environmental Geosciences