13C/12C composition, a novel parameter to study the downward migration of paper sludge in soils†
© The Royal Society of Chemistry and the Division of Geochemistry of the American Chemical Society 2002
Received: 07 June 2002
Accepted: 12 July 2002
Published: 22 July 2002
δ13C values of crop and forest soils were measured 8 years after disposal of paper sewage sludge. The carbon transfer from paper sludge downward to the first humic layer is evidenced by a 13C-enrichnient of up to + 5.6‰ due to the input of 13C-enriched sludge carbonates. 13C/12C composition is thus a novel, sensitive parameter to follow the downward transfer of paper sludge carbon.
Large amounts of agricultural, industrial and municipal wastes are produced daily by human activities. [1–5] In 1980, France's annual waste production reached about 5.5 million dry tonnes (m.d.t.) of municipal waste, 1.8 m.d.t. of urban and industrial sewage sludge, 78 m.d.t. from the agriculture and agro-industry, and 6.75 m.d.t. from forestry. Disposal of organic wastes onto agricultural and forestry lands has several potential benefits such as long-term fertilisation, improving soil water-holding capacity and improvement of aggregate stability. However, land-based waste disposal must be carefully controlled because of potential hazards associated with application of wastes, include pathogens, heavy metals and toxic organic by-products, as reviewed by Wilson et al. So far, the long-term changes of soil properties induced by organic waste disposal such as paper sludge are not well understood, notably due to the lack of analytical approaches to follow the fate of waste matter into the soil profile. Nonetheless, several recent reports show that stable carbon isotopes can be used to study environmental issues. [7–9] More specifically, since the main biochemical components of plants are isotopically distinguished, e.g. cellulose being 13C-enriched versus lignin and lipids, [10–12] we hypothesised that paper sludge might have a distinct δ13C ratio which could be used to study their long-term fate in soils. Moreover, since paper sludges contain carbonates, which are 13C-enriched, it could be feasible to isotopically distinguish soil carbon from sludge carbon. Here, we wish to report an isotopic investigation of crop and forest soils treated with paper sludge in 1992.
Sites disposed of with paper sludge in 1992
Four experimental sites from the Lorraine region, France, were selected for this study. The woodland site (4950 m2) is located in a forest planted with red oaks. The crop site (5200 m2), located about 500 m away from the forest site, previously cultivated with wheat, was planted sporadically with some pine trees after paper sludge disposal. Two control sites with the same characteristics are located beside the woodland and crop sites. All soils are mainly sandy, with silt, some clay (4–8%), and are acidic with pH ranging from 4.3 to 5.4. In July 1992, a 5–10 cm layer of paper sludge was evenly distributed over the woodland site (186 tons) and the crop site (306 tons). Paper sludge properties were: 42 wt.% dry matter (110°C), 36 dry-wt.% organic matter (combustion 650°C), pH 6.8, 23% CaO, 22% organic C, 0.4%, N, 0.14%, P2O5, 0.05% K2O, 0.4% MgO.
Soil sampling and isotope analysis
Results and discussion
Paper sludge disposal
In 1992, crop and woodland sites from the Lorraine region, France were treated with 186–306 tons of paper sewage sludge in order to study the effects of waste recycling. Precautions were taken to minimise potential environmental hazards, e.g. input of heavy metals. From 1992 to 1997, comparison of plants grown on both the treated and control sites showed the absence of visual toxic effects. Plants developed well with roots growing through the blue sludge layer. An investigation of the blue sludge layer from 1992 to 1997 showed a decrease of calcium content, from about 23 to 10%, and of organic matter content, from about 35 to 20%. In 2000, the blue sludge layer is still clearly apparent under a fern litter layer, as shown for the woodland site on Fig. 1. Here, we analysed samples of litter, grasses, sludge layer, and soil layers of increasing depth cored in August 2000, in order to study the downward carbon transfer from the paper sludge.
δ13C values and %carbon of non-demineralised soil samples cored in August 2000 from experimental control sites and from sites treated with paper sludge in 1992. Light-blue chunks of solidified paper sludge found on the soil surface yielded a %C value of 17.36% and δ13C value of -16.84‰. Sample deviation: ± 0.05% and ± 0.05‰ (3 repeats)
Litter ~3 cm, grasses a
Blue sludge b , 10 cm
Black humic c , 10 cm
Dark-brown c , 20 cm
Light-brown c , 20 cm
13C/12C isotopic composition
δlayer = xδsludge + (1 - x)δcontrol
where δlayer refer to the soil layer, δsludge to solid chunks of pure paper sludge (-16.84‰), and δcontrol to average δ13C values of control plots. In the woodland sites, the percentage x100 of sludge-derived carbon amounts to 76% in the blue sludge layer and to 21% in the underlying black humic layer, thus showing a notable downward carbon transfer. In crop plots, values amount respectively to 56 and 67% as the result of a downward carbon transfer, which could be explained by the lesser initial stratification of crop soils.
δ13C(org) analysis of demineralised samples show that the 13C-enrichment of the non-demineralised samples is due to the presence of carbonates. Specifically, demineralised blue paper chunks yield δ13C(org) values of -25.41‰ versus -16.84‰ for the non-demineralised sample. The blue sludge layers give δ13C(org) values of -27.22‰ for the woodland site and -26.28‰ for the crop site, versus respectively -20.97‰ and -22.81‰ for the non-demineralised samples. Similarly, the black humic layers give δ13C(org) of -26.97‰ for the woodland site and -26.27‰ for the crop site, versus -25.72‰ and -21.84‰ respectively for the non-demineralised samples. Since the demineralised values are similar to control values (Table 1), the observed 13C-increases of non-demineralised layers can be explained by the total carbonate contribution from the sludge.
The downward transfer of paper sludge 8 years after its disposal to crop and woodland soils has been assessed using 13C isotope analyses. The observed isotopic shifts are due to the presence of enriched carbon, derived from carbonates in the paper sludge.
†Presented at the ACS Division of Geochemistry Symposium 'Stable Isotope Signatures for Establishing Paleoenvironmental Change', Orlando, April 2002.
- Wilson SC, Burnett V, Waterhouse KS, Jones KC: Volatile organic compounds in digested United Kingdom sewage sludges. Environ Sci Technol. 1994, 28: 259-10.1021/es00051a012.View ArticleGoogle Scholar
- Wilson SC, Duarte-Davidson R, Jones KC: Screening the environmental fate of organic contaminants in sewage sludges applied to agricultural soils: 1. The potential for downward movement to groundwaters. Sci Total Environ. 1996, 185: 45-10.1016/0048-9697(95)05041-8.View ArticleGoogle Scholar
- O'Connor GA: Organic compounds in sludge-amended soils and their potential for uptake by crop plants. Sci Total Environ. 1996, 185: 71-10.1016/0048-9697(95)05043-4.View ArticleGoogle Scholar
- Chaney RL, Ryan JA, O'Connor GA: Organic contaminants in municipal biosolids: risk assessment, quantitative pathways analysis, and current research priorities. Sci Total Environ. 1996, 185: 187-10.1016/0048-9697(96)05051-6.View ArticleGoogle Scholar
- Payet C, Bryselbout C, Morel JL, Lichtfouse E: Fossil fuel biomarkers in sewage sludges: environmental significance. Naturwissenschaften. 1999, 86: 484-10.1007/s001140050659.View ArticleGoogle Scholar
- M Mustin: Le Compost. 1987, F. Dubusc, Paris, 954-(French)Google Scholar
- Compound-specific isotope analysis: tracing organic contaminant sources and processes in geochemical systems. Org Geochem. Edited by: Sherwood Lollar B, Abrajano TA. 1999, 30: 721-871. 10.1016/S0146-6380(99)00056-X.Google Scholar
- Amelung W, Bol R, Friedrich C: Natural 13C abundance: a tool to trace the incorporation of dung-derived carbon into soil particle-size fractions. Rapid Commum Mass Spectrom. 1999, 13: 1291-10.1002/(SICI)1097-0231(19990715)13:13<1291::AID-RCM637>3.0.CO;2-C.View ArticleGoogle Scholar
- Lichtfouse E: Compound-specific isotope analysis (CSIA). Application to archaeology, biomedical sciences, biosynthesis, environment, extraterrestrial chemistry, food science, forensic science, humic substances, microbiology, organic geochemistry, soil science and sport. Rapid Commun Mass Spectrom. 2000, 14: 1337-10.1002/1097-0231(20000815)14:15<1337::AID-RCM9>3.0.CO;2-B.View ArticleGoogle Scholar
- Park R, Epstein S: Metabolic fractionation of 13C and 12C in plants. Plant Physiol. 1961, 36: 133-View ArticleGoogle Scholar
- Benner R, Fogel ML, Sprague EK, Hodson RE: Depletion of 13C in lignin and its implications for stable isotope studies. Nature. 1987, 329: 708-10.1038/329708a0.View ArticleGoogle Scholar
- O'Leary M: Carbon isotope fractionation in plants. Phytochemistry. 1981, 20: 553-10.1016/0031-9422(81)85134-5.View ArticleGoogle Scholar
- Lichtfouse E, Dou S, Girardin C, Grably M, Balesdent J, Behar F, Vandenbroucke M: Unexpected 13C-enrichment of organic components from wheat crop soils: evidence for the in situ origin of soil organic matter. Org Geochem. 1995, 23: 865-10.1016/0146-6380(95)80009-G.View ArticleGoogle Scholar
- Rogers KM: Effects of sewage contamination on macroalgae and shellfish at Moa Point, New Zealand using stable carbon and nitrogen isotopes. N Z J Mar Freshwater Res. 1999, 33: 181-View ArticleGoogle Scholar
- Rogers KM, Morgans HEG, Wilson GS: Identification of a Waipawa Formation equivalent in the Te Uri Member of the Whangai Formation – implications for depositional history and age. N Z J Geol Geophys. 2001, 44: 345-View ArticleGoogle Scholar