Advertisement

Radiocesium Concentrations in the Organic Fraction of Sea Sediments

Open Access
Chapter

Abstract

Sequential chemical extraction of radiocesium was performed on 22 surface sediment samples to assess radiocesium concentration in the organic fraction of sea sediments (Csorg). Our results showed that Csorg of sea sediments was significantly larger than that of bulk sediments (Csbulk). The concentration factor of radiocesium in organic fraction against the bulk concentration (CF) varied from 3 to 50 off the Fukushima continental margin and showed a proportional relationship with median grain size and an inversely proportional relationship with organic content (OC) of the sediment. By using these relationships, the regression equation of Csorg based on median grain size, organic content, and Csbulk was determined to construct a two-dimensional (2-D) distribution of Csorg along the continental margin off the Fukushima region. The resultant map showed that the continental margin north of Fukushima Dai-ichi Nuclear Power Plant (FNPP) had moderate Csorg values despite very low Csbulk. On the other hand, sediments sampled at the mouth of Abukuma River showed extremely low CF, which might have been caused by the existence of river-derived sediment particles.

Keywords

Sediment Radiocesium Organic fraction 
Download chapter PDF

5.1 Introduction

In the assessment of radiocesium transportation from sea sediments to a marine demersal ecosystem, information is required not only on the concentration but also on biological ingestibility of sea sediment radiocesium. Although IAEA has provided a standard concentration factor of radiocesium from sea sediments in marine organisms (e.g., 1 × 102 for fish; IAEA 2004), its actual value may vary according to sediment properties such as grain size and chemical composition. Radiocesium concentration in the organic fraction of sediments (Csorg) is an important factor because the transport of radiocesium from sediment to demersal ecosystem occurs primarily through the feeding/ingestion of carbon sediments by benthos. With regard to the FNPP accident, a large amount of data is available on the spatiotemporal distribution of radiocesium concentration in sea sediments (Csbulk) off the Fukushima Prefecture (Otosaka and Kobayashi 2012; Kusakabe et al. 2013; Otosaka and Kato 2014; Ambe et al. 2014). Unfortunately, insufficient data are available on the spatiotemporal distribution of Csorg. To address this issue, we conducted sequential chemical leaching experiments for 21 sea sediments sampled in July 2012 at 5′ × 5′ grid stations off Fukushima Prefecture (Ambe et al. 2014; see Fig. 5.1 for station map) to measure Csorg of these sediments. For details of sampling stations and experimental procedures, see Ono et al. (2015).
Fig. 5.1

Map of the location of the samples used in this study. Thick gray line denotes Abukuma River (only lower reaches are shown). Open squares denote the samples used for the bulk extraction experiment (Table 5.1), and open triangles denote the location of the off-Abukuma station (Table 5.2). Sampling stations of Ambe et al. (2014) are overlaid as solid squares

5.2 Csorg and Its Relationship with Csbulk

Estimated radiocesium concentrations in organic fraction (Csorg) and bulk sediment (Csbulk) in 21 grid samples are listed in Table 5.1. Csbulk ranged from 31 to 910 Bq/kg-dry and Csorg ranged from 345 to 3,390 Bq/kg-org-dry. Concentration factor (CF) and inventory ratio (IR) of radiocesium in organic fraction against bulk sediment were then calculated by the following equation:
Table 5.1

Specifications and measurement results of grid samples

Station no.

Sampling date

Latitude [N]

Longitude [E]

Bottom depth (m)

Median grain size (μm)

OC (%)

Csbulk (Bq/kg-dry)

Csorg [Bq/kg-org-dry]

CF

IR [%]

S1

2012.7.11

36° 20′

140° 55′

257

142

0.8

49 ± 5.5

350

7

5.8

S2

2012.7.11

36° 20′

140° 50′

120

136

0.7

78 ± 6.6

1,440

19

12.0

S3

2012.7.11

36° 20′

140° 45′

59

889

0.4

153 ± 9.7

2,440

16

5.9

S4

2012.7.11

36° 20′

140° 40′

33

201

1.0

310 ± 20

1,090

4

3.4

S20

2012.7.12

36° 40′

141° 10′

261

233

0.6

103 ± 6.3

520

5

3.0

S21

2012.7.12

36° 40′

141° 05′

144

265

0.5

60 ± 4.7

850

14

7.0

S22

2012.7.12

36° 40′

141° 00′

133

161

1.0

180 ± 13

1,330

7

7.3

S23

2012.7.12

36° 40′

140° 55′

111

87

1.6

180 ± 14

960

6

8.9

S24

2012.7.12

36° 40′

140° 50′

70

116

1.0

270 ± 21

1,300

5

4.9

S25

2012.7.12

36° 40′

140° 45′

33

no data

0.3

69 ± 5.9

490

7

2.4

S59

2012.7.13

37° 05′

141° 25′

177

247

0.6

83 ± 5.4

470

6

3.2

S60

2012.7.13

37° 05′

141° 20′

151

225

0.6

104 ± 6.3

2,360

23

13.9

S61

2012.7.13

37° 05′

141° 15′

140

85

1.3

101 ± 7.6

600

6

7.4

S62

2012.7.13

37° 05′

141° 10′

120

87

1.6

440 ± 27

1,200

3

4.5

S63

2012.7.12

37° 05′

141° 05′

72

158

1.6

690 ± 32

1,840

3

4.2

S64

2012.7.12

37° 05′

141° 01′

25

167

0.9

910 ± 32

3,120

3

3.2

S92

2012.7.15

37° 40′

141° 03.5′

24

118

1.0

710 ± 28

3,390

5

4.9

S93

2012.7.15

37° 40′

141° 05′

28

407

0.2

82 ± 5.9

1,270

16

4.0

S94

2012.7.15

37° 40′

141° 10′

37

723

0.1

31 ± 3.4

780

25

3.2

S95

2012.7.15

37° 40′

141° 15′

59

1,240

0.1

47 ± 4.1

2,330

50

5.0

S96

2012.7.15

37° 40′

141° 20′

100

146

0.7

230 ± 16

2,080

9

6.5

All data are reproduced from Ono et al. (2015)

Note: For definitions of Csbulk, Csorg, OC, CF, and IR, see the text

$$ \mathrm{C}\mathrm{F}={\mathrm{Cs}}_{\mathrm{org}}/{\mathrm{Cs}}_{\mathrm{bulk}} $$
(5.1)
$$ \mathrm{I}\mathrm{R}=\left({\mathrm{Cs}}_{\mathrm{org}}\cdot \mathrm{O}\mathrm{C}\right)/{\mathrm{Cs}}_{\mathrm{bulk}} $$
(5.2)
where OC represents the organic content of the sediment (Table 5.1).

CF values vary from 3 to 50, clearly illustrating that radiocesium concentration in the organic fraction of sea sediments is always several times larger than that of bulk sediment in areas off Fukushima. Despite these high CF values, IR showed relatively low values, ranging from 2.4 % to 13.9 %, reflecting low organic content in open ocean sediments.

Land sediments and soils have highly selective, nonexchangeable cesium adsorption capacity, up to 1 × 10−11 mol/kg-dry, because of the frayed edge sites in illite particles (Nakao et al. 2012). In marine environments, however, such nonexchangeable adsorption sites are occupied by stable cesium (~2 × 10−9 mol/l in seawater) and potassium (~1 × 10−2 mol/l in seawater). Newly supplied radiocesium from the accident, therefore, can only be bound to nonselective, exchangeable sorption sites, with the distribution coefficient of radiocesium estimated to be 300–4,000 l/kg-dry (IAEA 2004). Organic substances in the sediments also have nonselective sorption sites for cesium, but so far little is known about the distribution coefficient of cesium between marine organic matter and seawater. On land, several observations have indicated that the distribution coefficient of cesium for organic substances in soils is of the order of 102–103 l/kg-dry (Bunzl and Schimmack 1991; Nakamaru et al. 2007). If we assume that marine organic substances have the same distribution coefficient of cesium as land soils, we can consider that mineral and organic substances in the off-Fukushima sediments have the same order of preference as FNPP-derived radiocesium. The apparent preference of radiocesium in organic substances further increases when the surface of mineral particles is covered by organic substances (Keil et al. 1994; Mayer 1994; 1999). Mayer (1999), for example, found that even 0.5 % (w/w) of organic carbon can cover more than 10 % of total sediment surface area. In this case, with the assumption that organic carbon and mineral surfaces have the same preference with cesium, the observed CF of radiocesium increases to more than 20.

5.3 Horizontal Distribution of Csorg in off-Fukushima Continental Margin

CF is roughly proportional to median grain size and inversely proportional to OC (Fig. 5.2), suggesting that either or both of these properties are the main control factors of CF, although detailed analysis by Ono et al. (2015) concluded that OC is a major control factor and median grain size is minor. Using this information, we applied dual-parameter regression, appropriate for CF, against median grain size and combustion loss as follows:
Fig. 5.2

Plot of concentration factor (CF) versus median grain size (solid circles) and 1/organic content (OC) (open circles) for 21 off-Fukushima samples

$$ \mathrm{C}\mathrm{F}=0.0255\mu +20.08/\mathrm{I}\mathrm{L}-0.69\left({r}^2=0.736,\rho <0.01\right) $$
(5.3)
where μ and IL represent median grain size in μm (micrometers) and ignition loss in percentage, respectively. We chose IL instead of OC as an explanatory variable because the latter parameter was not measured for all samples reported by Ambe et al. (2014). Although IL somewhat overestimated the actual OC, we confirmed the linearity of IL against OC before the derivation of Eq. (5.3). We applied this equation to 113 surface stations observed by Ambe et al. (2014), and the calculated CF was multiplied by Csbulk in each station (Fig.  4.3 in  Chap. 4) to obtain Csorg. The results are shown in Fig. 5.3. A high Csorg band exists just offshore south of FNPP, within which the highest Csorg value of 10,300 Bq/kg-org-dry was obtained. In this area, the typical range of Csbulk south of FNPP was 2,000–7,000 Bq/kg-org-dry for the area with a bottom depth shallower than 100 m, and 500–1,500 Bq/kg-org-dry for the area with bottom depth ranging from 100 to 200 m. In the station north of FNPP, Csorg showed medium concentrations (~300–3,600 Bq/kg-org-dry) for the area with a bottom depth shallower than 100 m, and Csbulk values were extremely low (~10–100 Bq/kg-dry; see Ambe et al. 2014 and previous chapter); this is because the sediments of the mid-depth area (~30–100 m) north of FNPP consist mainly of large particles with low organic carbon content, which, using Eq. 5.3, leads to very high CF values. This result implies that the potential effect of sea sediment radiocesium on benthos would not be too different between the area south of FNPP with a bottom depth ranging from 100 to 200 m and north of FNPP with a bottom depth shallower than 100 m, despite a significant Csbulk difference between these areas. Wada et al. (2013) detected similar radiocesium level of demersal fishes between these two areas after 2012. These findings suggest that Csorg can be used as an indicator of the potential effect of sediment radiocesium on the demersal ecosystem.
Fig. 5.3

Distribution of calculated Csorg (organic cesium) in the off-Fukushima continental margin area. Contours are drawn from the Csorg value estimated by Eq. (5.3) for each station of Ambe et al. (2014)

5.4 Csorg and CF in off-Abukuma River Sediments

As the sediments described in the former sections are sampled from the continental margin, organic materials contained in these sediments are thought to be produced in the ocean. However, sediments in some local areas such as river mouths contain lithogenic particles, which were produced within freshwater or on land and then transported to the seafloor after the FNPP accident. For such sediments, CF can be considerably low because the nonexchangeable adsorption sites of mineral particles were not occupied by stable cesium or potassium at the time of the accident. To assess the CF value for such sediments, we performed additional Csorg measurements for sediments taken from the local high radiocesium patch recently discovered by the Nuclear Regulation Office (NRA 2014), located just outside of the Abukuma River mouth, with a horizontal scale of about 900 × 400 m width.

Differing from the foregoing grid samples, Csorg in the off-Abukuma patch showed significantly low CF values (~1.4; Table 5.2), possibly because of the significantly high OC value in the sample. Hence, a high-OC sediment tends to have a low CF value (Fig. 5.2). Another reason might be that the sediments in this patch contain a significant amount of lithogenic particles derived from the Abukuma River (Yamashiki et al. 2014). Although the observed Csbulk in this patch is the highest among the oceanic stations we observed, a low CF in the sediments causes the Csorg value to be at the same level as the average value of off-Fukushima sediments. The monitoring results for marine products for the off-Miyagi prefecture region did not detect any local increase in the occurrence of high-Cs fishes in off-Abukuma regions (JFA 2014), despite the existence of a high-Cs patch in sediments. A significantly low CF in the off-Abukuma sediment patch may explain these observation results. Again, our results showed that not only Csbulk but also Csorg are essential for accurately assessing the potential effect of sediment radiocesium on the demersal ecosystem in each region.
Table 5.2

Specifications and measurement results of off-Abukuma patch

Station no.

Sampling date

Latitude [N]

Longitude [E]

Bottom depth (m)

Median grain size (μm)

OC (%)

Csbulk (Bq/kg-dry)

Csorg (Bq/kg-org-dry)

CF

IR (%)

ABK-A

2013.8.22

38° 2.4′

140° 56.4′

13

No data

16

5,600 ± 75

7,882

1.4

23

5.5 Summary

Our study clarifies that radiocesium concentration in the organic fraction of sea sediments is always larger than that in the organic fraction of bulk sediments. This result indicates that the transport efficiency of radiocesium from the organic fraction of sediments to the marine benthos is extremely low, because the radiocesium concentration in marine benthos is of the order of 101 Bq/kg-wet (see  Chap. 7). The details of the physiological mechanism that results in such low transport efficiency is an important topic for future study.

Based on Csorg, we assessed that the sediments in the off-Fukushima continental margin north of the FNPP have moderate potential to transport radiocesium to benthic ecosystems, despite the low Csbulk observed in this region. However, sediments off Abukuma River have less potential to transport radiocesium than the level inferred from its Csbulk value.

References

  1. Ambe D, Kaeriyama H, Shigenobu Y, Fujimoto K, Ono T, Sawada H, Saito H, Miki S, Setou T, Morita T, Watanabe T (2014) A high-resolved spatial distribution of radiocesium in sea sediment derived from Fukushima Dai-ichi Nuclear Power Plant. J Environ Radioact 138:264–275PubMedCrossRefGoogle Scholar
  2. Bunzl K, Schimmack W (1991) Kinetics of the sorption of 137Cs, 85Sr, 57Co, 65Zn, and 109Cd by the organic horizons of a forest soil. Radiochim Acta 54:97–102CrossRefGoogle Scholar
  3. IAEA (2004) Sediment distribution coefficients and concentration factors for biota in the marine environment. IAEA technical reports series No.422. IAEA, ViennaGoogle Scholar
  4. JFA (2014) Results of the monitoring on radioactivity level in fisheries products. http://www.jfa.maff.go.jp/e/inspection/index.html
  5. Keil RG, Montlucon DB, Prahl FG, Hedges JI (1994) Sorptive preservation of labile organic matter in marine sediments. Nature (Lond) 370:549–552CrossRefGoogle Scholar
  6. Kusakabe M, Oikawa S, Takata H, Misonoo J (2013) Spatiotemporal distributions of Fukushima-derived radionuclides in nearby marine surface sediments. Biogeosciences 10:5019–5030. doi: 10.5194/bg-10-5019-2013 CrossRefGoogle Scholar
  7. Mayer LM (1994) Surface area control of organic carbon accumulation in continental shelf sediments. Geochim Cosmochim Acta 58:1271–1284CrossRefGoogle Scholar
  8. Mayer LM (1999) Extent of coverage of mineral surfaces by organic matter in marine sediments. Geochim Cosmochim Acta 63:207–215CrossRefGoogle Scholar
  9. Nakamaru Y, Ishikawa N, Tagami K, Uchida S (2007) Role of soil organic matter in the mobility of radiocesium in agricultural soils common in Japan. Colloid Surf A 306:111–117. doi: 10.1016/j.colsurfa.2007.01.014 CrossRefGoogle Scholar
  10. Nakao A, Funakawa S, Takeda A, Tsukada H, Kosaki T (2012) The distribution coefficient for cesium in different clay fractions in soils developed from granite and Paleozoic shales in Japan. Soil Sci Plant Nutr 58:397–403. doi: 10.1080/00380768.2012.698595 CrossRefGoogle Scholar
  11. NRA (2014) FY2013 Report of NRA survey for distribution of radioactive nuclides in marine environment (in Japanese) http://radioactivity.nsr.go.jp/ja/contents/10000/9423/24/report_20140613.pdf
  12. Ono T, Ambe D, Kaeriyama H, Shigenobu Y, Fujimoto K, Sogame K, Nishiura N, Fujikawa T, Morita T, Watanabe T (2015) Concentration of radiocesium bonded to organic fraction of sediment off Fukushima, Japan. Geochem J 49. doi:  10.2343/geochemj.2.0351
  13. Otosaka S, Kato Y (2014) Radiocesium derived from the Fukushima Daiichi Nuclear Power Plant accident in seabed sediments: initial deposition and inventories. Environ Sci Processes Impacts 16:978–990. doi: 10.1039/C4EM00016A CrossRefGoogle Scholar
  14. Otosaka S, Kobayashi T (2012) Sedimentation and remobilization of radiocesium in the coastal area of Ibaraki, 70 km south of the Fukushima Dai-ichi Nuclear Power Plant. Environ Monit Assess 185:5419–5433. doi: 10.1007/s10661-012-2956-7 PubMedCrossRefGoogle Scholar
  15. Wada T, Nemoto Y, Shimamura S, Fujita T, Mizuno T, Sahtome T, Kamiyama K, Morita T, Igarashi S (2013) Effects of the nuclear disaster on marine products in Fukushima. J Environ Radioact 124:246–254. doi: 10.1016/j.jenvrad.2013.05.008 PubMedCrossRefGoogle Scholar
  16. Yamashiki Y, Onda Y, Smith HG, Blake WH, Wakahara T, Igarashi Y, Matsuura Y, Yoshimura K (2014) Initial flux of sediment-associated radiocesium to the ocean from the largest river impacted by Fukushima Daiichi Nuclear Power Plant. Sci Rep 4:3714. doi: 10.1038/srep03714 PubMedCrossRefGoogle Scholar

Copyright information

© The Author(s) 2015

Open Access This chapter is distributed under the terms of the Creative Commons Attribution Noncommercial License, which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and source are credited.

Authors and Affiliations

  1. 1.National Research Institute of Fisheries SciencesFisheries Research AgencyKanazawa, YokohamaJapan
  2. 2.KANSO TechnosKatano, OsakaJapan
  3. 3.Tohoku National Fisheries Research Institute, Fisheries Research AgencyShiogamaJapan

Personalised recommendations

Cite chapter

Download book