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Plant residues as direct and indirect sources of hydrocarbons in soils: current issues and legal implications. Marco Vecchiato, Tiziano Bonato, Andrea Bertin, Elena Argiriadis, Carlo Barbante, and Rossano Piazza Environ. Sci. Technol. Lett., Just Accepted Manuscript • DOI: 10.1021/acs.estlett.7b00464 • Publication Date (Web): 10 Nov 2017 Downloaded from http://pubs.acs.org on November 13, 2017
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Plant Residues as Direct and Indirect Sources of Hydrocarbons in Soils:
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Current Issues and Legal Implications.
3 4 5 6
Marco Vecchiato a*, Tiziano Bonato Rossano Piazza
a,c
a,b
, Andrea Bertin b, Elena Argiriadis a, Carlo Barbante
a,c
,
.
7 8 9 10
a
Department of Environmental Sciences, Informatics and Statistics (DAIS), Ca’ Foscari University of
Venice, Via Torino 155, 30172 Venezia-Mestre, Venice, Italy.
11 12
b
Società Estense Servizi Ambientali (S.E.S.A. S.p.A.), Via Comuna 5/B, 35042, Este, PD, Italy.
13 14
c
15
Venezia-Mestre, Venice, Italy.
Institute for the Dynamics of Environmental Processes (IDPA-CNR), Via Torino 155, 30172
16 17 18 19
*Corresponding author: Marco Vecchiato
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e-mail:
[email protected] 21
phone: +39 0412348545
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Keywords: Soil; Total petroleum hydrocarbons (TPH); n-Alkanes; leaf waxes; amendments.
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Abstract
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Plant residues are the main source of organic matter in soil: this process takes place naturally in
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forests and with organic amendments in farmlands. Terrestrial plants also synthesize
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hydrocarbons: typically, angiosperms contain hundreds to thousands mg kg-1 of long-chain n-
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alkanes in leaf waxes. However, petroleum pollution is a worldwide issue and different national
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regulations set at 50 mg kg-1 the guideline limit for petroleum hydrocarbons in green areas.
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Focusing on the Italian legislation as a case study, we hypothesized that direct or indirect high
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inputs of plant residues could lead the soil to exceed this limit, resulting in a false positive
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petroleum contamination. Therefore, we investigated the occurrence of hydrocarbons in soils with
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different inputs of natural or farming biomasses. The highest total petroleum hydrocarbons (TPH)
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concentrations were found in background soils from protected woodlands, remarkably with most
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samples resulting above the guideline limit. Similarly, TPH in agricultural soils amended with
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compost and digestate resulted higher than in soil samples where only chemical fertilizers were
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used. n-Alkanes Carbon Preference Indices (CPIs) underlined the role of plant residues as source of
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hydrocarbons in these samples, clearly distinguishing spiked petrogenic contamination. Possible
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revisions of the regulatory and analytical methods were later discussed.
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Introduction
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Terrestrial plants produce hydrocarbons as components of the epicuticular waxes to protect plant
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tissues from the external environment1. When plant residues are incorporated in soil, these
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contribute to the soil organic matter2, both naturally in woodlands and forests or artificially from
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crop residues or manure in agricultural lands. The input of biomasses and the fertilization with
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amendments, as compost and digestate, have positive effects on the biological, physical, and
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chemical soil properties, reducing dumping of wastes in landfill sites3–5. Moreover, the organic
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matter in agricultural soils is considered one potential sink for sequestration of atmospheric
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carbon dioxide2,6.
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On the other hand, petroleum hydrocarbons are some of the most widespread soil pollutants
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worldwide and hydrocarbon contamination of soil is an issue widely studied in the scientific
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literature. However, one of the main analytical and legal issues is how to distinguish between
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actual petrogenic contamination from naturally occurring hydrocarbons and biogenic 2 ACS Paragon Plus Environment
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interferences, since these could potentially lead to unnecessary remediation costs7. However,
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although many parameters (reported in the SI) have been proposed and used to identify the
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environmental contamination due to petroleum hydrocarbons8–11, none of them is unique and
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effective for the different petroleum-derived products, probably except total petroleum
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hydrocarbons (TPH). This parameter, despite its selectivity drawbacks7, is generally adopted to
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assess the soil contamination from the different petroleum products. The analytical determination
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of TPH includes a large family of different hydrocarbons, regardless of their toxicity, origin and
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composition (linear, branched, cyclic and aromatic compounds)12,13. Italian legislation (Legislative
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Decree 152/2006, Part IV, Title V, Annex 5) sets the limit for heavy hydrocarbons (with a number
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of carbon atoms higher than 12) in public, private, residential green areas and agricultural land at
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50 mg kg-1 d.w.; those sites found to exceed these limits should be remediated or a site-specific
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risk analysis should prove the absence of human health risks. The parameter C>12 is substantially
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corresponding to TPH, defining a slight modification of the normed analytical method ISO
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16703:2004 changing the application range from C10-C40 to C12-C40 13.
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The limit at 50 mg kg-1 d.w. is not based on hydrocarbon toxicity, which is highly dependent on the
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speciation and the availability of the hydrocarbons, but it was selected because it was considered
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to be high enough to avoid false positives14. Consequently this value was chosen as target value
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for soil quality standards in different European countries12,14. However, the various national
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regulations result in very different procedures and intervention guidelines for remediation of
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contamination episodes of agricultural soil. For example, there is a wide discrepancy of two orders
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of magnitude between the Italian and Dutch intervention values for remediation of hydrocarbons
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in soil, being the limits set at 50 mg kg-1 and 5000 mg kg-1 (VROM 2012), respectively12. This clearly
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shows the need for the harmonization of national procedures for contaminated sites in the
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European Union14. Outside from Europe, a similar situation is present also in the USA, with
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significant variability of methods, action and clean-up levels for hydrocarbons in contaminated
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soils among the different states, in a framework of increasing complexity15. The Canadian
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legislation specifies different carbon ranges to analyze the total hydrocarbons in soil7. Notably the
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method does not include a purification step, therefore also polar biogenic compounds such as
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plant waxes, fatty acids and sterols are considered as petroleum hydrocarbon contaminants, even
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when naturally exceeding the regulatory levels16.
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Plant-derived n-alkanes
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Terrestrial plants typically synthesize long chain n-alkanes as part of the epicuticular leaf wax,
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contributing to the hydrophobic properties and protecting the leaf from the external environment.
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Leaf n-alkanes are commonly produced with a strong odd-over-even predominance (OEP), and,
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lacking functional groups, are especially long-lived molecules1. For these reasons n-alkanes are
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widely used as biomarkers to reconstruct environmental changes in modern and paleoecological
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studies1,17. The abundance and distribution of the n-alkanes in leaves depend on the plant species,
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the growing season and the environmental conditions (e.g. temperature, moisture, nutrient
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availability, soil properties), varying even within an individual tree1,18. Typically, angiosperms
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produce hundreds to thousands mg of n-alkanes per kg of dry leaf matter, while gymnosperms are
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at orders of magnitude lower. n-C27, n-C29 and n-C31 are the dominant n-alkanes in graminoids and
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woody angiosperms in variable relative abundances1. The Carbon Preference Index (CPI) is a
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definitive measure of biologically synthesized compounds, defining the degree to which odd
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carbon number n-alkanes dominate over even carbon numbers, being the ratio of the sums of
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concentrations of odd and even n-alkane homologues in a given carbon number range19. Mean CPI
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values in leaves of the large majority of modern plant are around 10 although with very large
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variations, being in few cases close or lower than 1, which is the typical CPI value of petrogenic
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inputs1,20. Another parameter is the weighted average of the various carbon chain lengths of the n-
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alkanes, usually defined as the Average Chain Length (ACL=∑(Cnxn)/∑Cn), where Cn is the
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concentration of each n-alkane with n carbon atoms1. Leaf surface waxes can be sources of n-
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alkanes to soil both in woodland and grassland21,22, as well as directly from crop residues in
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agricultural land 23. Other tissues of higher plants (e.g. beech and spruce roots) are characterized
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by short chain (C12 in suoli contaminati, n. 75/2011.; ISPRA - Manuali e Linee Guida: Rome,
347
2011.
348
(14)
Carlon, C.; D’Alessandro, M.; Swartjies, F. Derivation methods of soil screening values in
349
europe. A review and evaluation of national procedures towards harmonisation, EUR 22805-
350
EN; Carlon, C., Ed.; European Commission, Joint Research Centre, Ispra, 2007.
351
(15)
Tomlinson, P.; Ruby, M. V. State and federal cleanup levels for petroleum hydrocarbons in
352
soil: State of the states and implications for the future. Hum. Ecol. Risk Assess. An Int. J.
353
2016, 22, 911–926 DOI: 10.1080/10807039.2015.1120151.
354
(16)
Wang, Z.; Yang, C.; Yang, Z.; Hollebone, B.; Brown, C. E.; Landriault, M.; Sun, J.; Mudge, S.
355
M.; Kelly-Hooper, F.; Dixon, D. G. Fingerprinting of petroleum hydrocarbons (PHC) and other
356
biogenic organic compounds (BOC) in oil-contaminated and background soil samples. J.
357
Environ. Monit. 2012, 14, 2367–2381 DOI: 10.1039/c2em30339f.
358
(17)
Diefendorf, A. F.; Freeman, K. H.; Wing, S. L.; Graham, H. V. Production of n-alkyl lipids in
359
living plants and implications for the geologic past. Geochim. Cosmochim. Acta 2011, 75,
360
7472–7485 DOI: 10.1016/j.gca.2011.09.028. 13 ACS Paragon Plus Environment
Page 15 of 20
361
Environmental Science & Technology Letters
(18)
Kirkels, F. M. S. A.; Jansen, B.; Kalbitz, K. Consistency of plant-specific n-alkane patterns in
362
plaggen ecosystems: A review. The Holocene 2013, 23, 1355–1368 DOI:
363
10.1177/0959683613486943.
364
(19)
Simoneit, B. R. T. Organic matter of the troposphere - V: Application of molecular marker
365
analysis to biogenic emissions into the troposphere for source reconciliations. J. Atmos.
366
Chem. 1989, 8, 251–275 DOI: 10.1007/BF00051497.
367
(20)
Yang, C.; Yang, Z.; Zhang, G.; Hollebone, B.; Landriault, M.; Wang, Z.; Lambert, P.; Brown, C.
368
E. Characterization and differentiation of chemical fingerprints of virgin and used lubricating
369
oils for identification of contamination or adulteration sources. Fuel 2016, 163, 271–281
370
DOI: 10.1016/j.fuel.2015.09.070.
371
(21)
Jansen, B.; Nierop, K. G. J.; Kotte, M. C.; de Voogt, P.; Verstraten, J. M. The applicability of
372
accelerated solvent extraction (ASE) to extract lipid biomarkers from soils. Appl.
373
Geochemistry 2006, 21, 1006–1015 DOI: 10.1016/j.apgeochem.2006.02.021.
374
(22)
Kuhn, T. K.; Krull, E. S.; Bowater, A.; Grice, K.; Gleixner, G. The occurrence of short chain n-
375
alkanes with an even over odd predominance in higher plants and soils. Org. Geochem.
376
2010, 41, 88–95 DOI: 10.1016/j.orggeochem.2009.08.003.
377
(23)
Lichtfouse, E.; Elbisser, B.; Balesdent, J.; Mariotti, A.; Bardoux, G. Isotope and molecular
378
evidence for direct input of maize leaf wax n-alkanes into crop soils. Org. Geochem. 1994,
379
22, 349–351.
380
(24)
Griepentrog, M.; Bodé, S.; Boeckx, P.; Wiesenberg, G. L. B. The fate of plant wax lipids in a
381
model forest ecosystem under elevated CO2 concentration and increased nitrogen
382
deposition. Org. Geochem. 2016, 98, 131–140 DOI: 10.1016/j.orggeochem.2016.05.005.
383
(25)
Rao, Z.; Zhu, Z.; Wang, S.; Jia, G.; Qiang, M.; Wu, Y. CPI values of terrestrial higher plant-
384
derived long-chain n-alkanes: A potential paleoclimatic proxy. Front. Earth Sci. China 2009,
385
3, 266–272 DOI: 10.1007/s11707-009-0037-1.
386
(26)
Sun, H. X.; Zhou, D. W. Prediction of diet composition and intake of sheep grazing soybean
387
and maize residues. J. Appl. Anim. Res. 2009, 35, 125–129 DOI:
388
10.1080/09712119.2009.9707001.
389
(27)
Marseille, F.; Disnar, J. R.; Guillet, B.; Noack, Y. n-Alkanes and free fatty acids in humus and 14 ACS Paragon Plus Environment
Environmental Science & Technology Letters
390
A1 horizons of soils under beech, spruce and grass in the Massif-Central (Mont-Lozere),
391
France. Eur. J. Soil Sci. 1999, 50, 433–441 DOI: 10.1046/j.1365-2389.1999.00243.x.
392
(28)
Page 16 of 20
Wiesenberg, G. L. B.; Dorodnikov, M.; Kuzyakov, Y. Source determination of lipids in bulk
393
soil and soil density fractions after four years of wheat cropping. Geoderma 2010, 156, 267–
394
277 DOI: 10.1016/j.geoderma.2010.02.026.
395
(29)
Pietrogrande, M. C.; Mercuriali, M.; Pasti, L.; Dondi, F. Data handling of complex GC-MS
396
chromatograms: characterization of n-alkane distribution as chemical marker in organic
397
input source identification. Analyst 2009, 134, 671–680 DOI: 10.1039/b815317e.
398
(30)
Wiesenberg, G. L. B.; Schwarzbauer, J.; Schmidt, M. W. I.; Schwark, L. Source and turnover
399
of organic matter in agricultural soils derived from n-alkane/n-carboxylic acid compositions
400
and C-isotope signatures. Org. Geochem. 2004, 35, 1371–1393 DOI:
401
10.1016/j.orggeochem.2004.03.009.
402
(31)
Rommerskirchen, F.; Plader, A.; Eglinton, G.; Chikaraishi, Y.; Rullkötter, J. Chemotaxonomic
403
significance of distribution and stable carbon isotopic composition of long-chain alkanes and
404
alkan-1-ols in C4 grass waxes. Org. Geochem. 2006, 37, 1303–1332 DOI:
405
10.1016/j.orggeochem.2005.12.013.
406
(32)
Quénéa, K.; Largeau, C.; Derenne, S.; Spaccini, R.; Bardoux, G.; Mariotti, A. Molecular and
407
isotopic study of lipids in particle size fractions of a sandy cultivated soil (Cestas cultivation
408
sequence, southwest France): Sources, degradation, and comparison with Cestas forest soil.
409
Org. Geochem. 2006, 37, 20–44 DOI: 10.1016/j.orggeochem.2005.08.021.
410
(33)
Miller, S. S.; Reid, L. M.; Butler, G.; Winter, S. P.; McGoldrick, N. J. Long Chain Alkanes in Silk
411
Extracts of Maize Genotypes with Varying Resistance to Fusarium graminearum. J. Agric.
412
Food Chem. 2003, 51, 6702–6708 DOI: 10.1021/jf0341363.
413
(34)
Its Water-Soluble Fractions. J. Agric. Food Chem. 2008, 56, 1017–1024.
414 415
Spaccini, R.; Baiano, S.; Gigliotti, G.; Piccolo, A. Molecular Characterization of a Compost and
(35)
El Fels, L.; Lemee, L.; Ambles, A.; Hafidi, M. Identification and biotransformation of aliphatic
416
hydrocarbons during co-composting of sewage sludge-Date Palm waste using Pyrolysis-GC /
417
MS technique. Environ. Sci. Pollut. Res. 2016, 7285, 16857–16864 DOI: 10.1007/s11356-016-
418
6670-9. 15 ACS Paragon Plus Environment
Page 17 of 20
419
Environmental Science & Technology Letters
(36)
Brändli, R. C.; Bucheli, T. D.; Kupper, T.; Furrer, R.; Stahel, W. a; Stadelmann, F. X.;
420
Tarradellas, J. Organic pollutants in compost and digestate. Part 1. Polychlorinated
421
biphenyls, polycyclic aromatic hydrocarbons and molecular markers. J. Environ. Monit.
422
2007, 9, 456–464 DOI: 10.1039/b617101j.
423
(37)
soil contaminated with diesel fuel.pdf. Environ. Pollut. 2001, 112, 269–283.
424 425
Semple, K. T.; Reid, B. J.; Fermor, T. R. Impact of composting strategies on the treatment of
(38)
Namkoong, W.; Hwang, E. Y.; Park, J. S.; Choi, J. Y. Bioremediation of diesel-contaminated
426
soil with composting. Environ. Pollut. 2002, 119, 23–31 DOI: 10.1016/S0269-7491(01)00328-
427
1.
428
(39)
Kelly-Hooper, F.; Farwell, A. J.; Pike, G.; Kennedy, J.; Wang, Z.; Grunsky, E. C.; Dixon, D. G.
429
Field survey of Canadian background soils: Implications for a new mathematical gas
430
chromatography-flame ionization detection approach for resolving false detections of
431
petroleum hydrocarbons in clean soils. Environ. Toxicol. Chem. 2014, 33, 1754–1760 DOI:
432
10.1002/etc.2578.
433
(40)
Kelly-Hooper, F.; Farwell, A. J.; Pike, G.; Kennedy, J.; Wang, Z.; Grunsky, E. C.; Dixon, D. G. Is
434
it clean or contaminated soil? Using petrogenic versus biogenic GC-FID chromatogram
435
patterns to mathematically resolve false petroleum hydrocarbon detections in clean organic
436
soils: A crude oil-spiked peat microcosm experiment. Environ. Toxicol. Chem. 2013, 32,
437
2197–2206 DOI: 10.1002/etc.2285.
438
(41)
Guarino, C.; Spada, V.; Sciarrillo, R. Assessment of three approaches of bioremediation (
439
Natural Attenuation , Landfarming and Bioagumentation e Assistited Landfarming ) for a
440
petroleum hydrocarbons contaminated soil. Chemosphere 2017, 170, 10–16 DOI:
441
10.1016/j.chemosphere.2016.11.165.
442
(42)
Teng, Y.; Zhou, Q.; Miao, X.; Chen, Y. Assessment of soil organic contamination in a typical
443
petrochemical industry park in China. Environ. Sci. Pollut. Res. 2015, 22, 10227–10234 DOI:
444
10.1007/s11356-015-4219-y.
445
(43)
Wang, Z.; Yang, C.; Parrott, J. L.; Frank, R. A.; Yang, Z.; Brown, C. E.; Hollebone, B.;
446
Landriault, M.; Fieldhouse, B.; Liu, Y.; et al. Forensic source differentiation of petrogenic,
447
pyrogenic, and biogenic hydrocarbons in Canadian oil sands environmental samples. J.
448
Hazard. Mater. 2014, 271, 166–177 DOI: 10.1016/j.jhazmat.2014.02.021. 16 ACS Paragon Plus Environment
Environmental Science & Technology Letters
449
(44)
Riccardi, C.; Di Filippo, P.; Pomata, D.; Di Basilio, M.; Spicaglia, S.; Buiarelli, F. Identification
450
of hydrocarbon sources in contaminated soils of three industrial areas. Sci. Total Environ.
451
2013, 450–451, 13–21 DOI: 10.1016/j.scitotenv.2013.01.082.
452
(45)
Rao, Z.; Wu, Y.; Zhu, Z.; Jia, G.; Henderson, A. Is the maximum carbon number of long-chain
453
n-alkanes an indicator of grassland or forest? Evidence from surface soils and modern
454
plants. Chinese Sci. Bull. 2011, 56, 1714–1720 DOI: 10.1007/s11434-011-4418-y.
455
(46)
Jansen, B.; Nierop, K. G. J.; Hageman, J. A.; Cleef, A. M.; Verstraten, J. M. The straight-chain
456
lipid biomarker composition of plant species responsible for the dominant biomass
457
production along two altitudinal transects in the Ecuadorian Andes. Org. Geochem. 2006,
458
37, 1514–1536 DOI: 10.1016/j.orggeochem.2006.06.018.
459
(47)
Scholz-Böttcher, B. M.; Ahlf, S.; Vázquez-Gutiérrez, F.; Rullkötter, J. Natural vs.
460
anthropogenic sources of hydrocarbons as revealed through biomarker analysis: A case
461
study in the southern Gulf of Mexico. Bol. la Soc. Geol. Mex. 2009, 61, 47–56.
462
(48)
Page 18 of 20
Kaplan, I. R.; Galperin, Y.; Lu, S. T.; Lee, R. P. Forensic environmental geochemistry:
463
Differentiation of fuel-types, their sources and release time. Org. Geochem. 1997, 27, 289–
464
317 DOI: 10.1016/S0146-6380(97)87941-7.
465
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