Abstract
This article contains analytical data on Rare Earth Elements (REE) concentration in waters and solid samples (mining wastes and biominerals) collected in an abandoned mining site characterized by near-neutral conditions, and they are related with the research article “Geochemistry of rare earth elements in water and solid materials at abandoned mines in SW Sardinia (Italy)” (Medas et al., 2013).
REE can show specific signatures due to fractionation processes, giving an insight to the understanding of the natural processes ruling the water–rock interactions and the geo–bio-interactions. Most researches on REE behavior were performed in acidic environments, while only few data on REE are available for neutral waters. Elaboration of this dataset can be useful to evaluate the reactions controlling the geochemical behavior of REE under near-neutral to slightly alkaline conditions, driving the scientific community toward an efficient management of monitoring actions and remediation technologies.
Keywords: Rare earth elements, Fractionation, Water, Mine wastes, Biomineral
Specifications table
| Subject area | Earth and Planetary Sciences |
| More specific subject area | Geochemistry and Petrology |
| Type of data | Figures and Tables. |
| How data was acquired | Inductively coupled plasma mass spectrometry (ICP-MS, Perkin-Elmer, Elan 5000/DRC-e, USA), X ray diffraction (conventional θ–2θ equipment – Panalytical – with Cu Kα wavelength radiation – λ = 1.54060 Å, operating at 40 kV and 40 mA, using the X’Celerator detector). |
| Data format | Analyzed, elaborated. |
| Experimental factors | Water samples were collected and stabilized according to established protocols, then they were stored in a refrigerator until the analysis. Solid samples were dried, grounded and acid digested by a microwave (ETHOS One, Advanced Microwave Digestion System, Milestone) prior to the analysis by ICP-MS. |
| Experimental features | Mineralogical composition of mine wastes and biominerals and REE contents were determined. |
| Data source location | Ingurtosu, SW Sardinia, Italy. |
| Data accessibility | Data are with this article. |
| Related research article | Medas D, Cidu R, De Giudici G, Podda F, Geochemistry of rare earth elements in water and solid materials at abandoned mines in SW Sardinia (Italy), J Geochem. Explor., 2013, 133, 149–159. |
Value of the data
-
•
The presented data contribute to create a database of Rare Earth Element contents in different environmental matrices collected in abandoned mining areas.
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•
The collected data can be compared with literature and new acquired data from other researchers for the understanding of the geochemical and mineralogical processes.
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•
The investigation of Rare Earth Element fractionation processes can help to design efficient remediation actions.
1. Data
Samples were collected in the Ingurtosu Zn–Pb abandoned mining area, located in the South–West of Sardinia, Italy (Fig. 1). After the mine closure (1968), no remediation actions were undertaken to avoid the dispersion of metals, resulting in the pollution of both waters and soils [1], [2]. Rio Naracauli is the main stream of the area, it receives drainages from mine tailings, and then flows into the Mediterranean Sea. Naracauli waters have pH values (6.9–8.4) near neutral to slightly alkaline. Along the stream, the peculiar precipitation of two biominerals is observed during the spring and summer seasons, namely hydrozincite, Zn5(CO3)2(OH)6 [3], [4], [5], and an amorphous Zn-silicate [6], [7], [8], [9], [10], making this area an distinctive system for the investigation of both water–rock interaction and geo–bio interaction processes.
Fig. 1.
Map with the location of the sampling points in the Ingurtosu mining district. Image from Google Maps, modified.
Rare Earth Elements (REE) were determined in stream waters, drainages from mine tailings and solid materials (mine wastes and biominerals) to elucidate REE fractionation processes occurring in a near-neutral environment. Data are reported in Figs. 2 and 3 and Table 1, Table 2, Table 3, Table 4, Table 5, Table 6, Table 7, Table 8, Table 9. For a detailed description and discussion of the data see [1].
Fig. 2.
X ray diffraction patterns of the mine tailings samples collected in the Ingurtosu mining district (sampling site MTA).
Fig. 3.
X ray diffraction patterns of the mine tailings samples collected in the Ingurtosu mining district (sampling site MTB).
Table 1.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the Rio Naracauli waters, continues. ΣREE indicates the sum from La to Lu.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| NS-100 | 18 March 2009 | 7.4 | 466 | 1042 | 590 | 740 | 367 | 81 | 290 | 58 | 26 | 90 | 12 | 58 | 11 | 24 | 2.2 | 11 | 1.7 | 1772 |
| NS-170 | 18 March 2009 | 7.5 | 466 | 1020 | 360 | 404 | 123 | 38 | 129 | 19 | 9.7 | 37 | 5.4 | 24 | 4.9 | 12 | 1.4 | 7.4 | 1.2 | 816 |
| NS-330 | 18 March 2009 | 7.7 | 475 | 1310 | 180 | 166 | 53 | 18 | 63 | 12 | 7 | 18 | 3 | 13 | <4 | 5.7 | <1 | 4.5 | <1 | 363 |
| NS-420 | 18 March 2009 | 7.8 | 492 | 1239 | 60 | 44 | <25 | <13 | <34 | <6 | 3.8 | <5 | 1.2 | 3.1 | <4 | <3 | <1 | <3 | <1 | 52 |
| NS-590 | 18 March 2009 | 7.9 | 492 | 1255 | 22 | 26 | 23 | <13 | <34 | <6 | 3.7 | <5 | <1 | <3 | <4 | <2 | <1 | <3 | <1 | 53 |
| NS-630 | 18 March 2009 | 7.4 | 497 | 637 | 44 | 34 | 45 | <13 | <34 | <6 | 4.4 | 7.2 | 1.2 | 4.3 | <4 | 3 | <1 | 3 | <1 | 102 |
| NS-1200 | 18 March 2009 | 7.7 | 511 | 645 | 64 | 40 | 30 | <13 | <34 | <6 | 3.3 | 7 | 1.1 | 5.6 | <4 | 3 | <1 | 3 | <1 | 93 |
| NS-1600 | 18 March 2009 | 7.8 | 480 | 597 | 84 | 47 | 23 | <13 | <34 | 3.5 | 5.3 | 7.9 | 1.2 | 4.9 | <4 | 4.2 | <1 | 3 | <1 | 100 |
| NS-100 | 25 March 2009 | 7.3 | 488 | 1006 | 380 | 404 | 60 | 32 | 120 | 20 | 10 | 34 | 4.5 | 22 | 5.2 | 14 | 1.6 | 7.9 | 1.4 | 737 |
| NS-170 | 25 March 2009 | 7.4 | 483 | 1001 | 149 | 124 | 31 | 11 | 36 | 6 | 5.2 | 11 | 1.8 | 7.7 | 2 | 4.8 | <1 | 3 | <1 | 244 |
| NS-330 | 25 March 2009 | 7.6 | 480 | 1283 | 153 | 140 | 44 | 14 | 44 | 15 | 6.1 | 13 | 2.2 | 9 | <4 | 7 | <1 | 3.6 | <1 | 297 |
| NS-420 | 25 March 2009 | 7.8 | 458 | 1269 | 67 | 94 | 72 | 8.8 | 26 | <6 | 4.2 | 7 | <1 | 4 | <4 | 3 | <1 | <3 | <1 | 219 |
| NS-590 | 25 March 2009 | 7.9 | 446 | 1265 | 18 | 28.9 | 32 | <13 | <34 | <6 | 3.8 | <5 | <3 | <1 | <4 | <2 | <1 | <3 | <1 | 65 |
| NS-100 | 17 April 2009 | 6.9 | 602 | 1134 | 770 | 943 | 341 | 92 | 341 | 59 | 26 | 110 | 13 | 62 | 13 | 32 | 3.7 | 19 | 2.5 | 2057 |
| NS-170 | 17 April 2009 | 7.1 | 571 | 1147 | 760 | 940 | 580 | 117 | 430 | 90 | 37 | 137 | 17 | 77 | 15 | 33 | 3.6 | 17 | 2.5 | 2496 |
| NS-330 | 17 April 2009 | 7.2 | 615 | 1284 | 470 | 514 | 183 | 54 | 200 | 33 | 13 | 56 | 7.5 | 36 | 8 | 19 | 2.5 | 11 | 1.6 | 1139 |
| NS-420 | 17 April 2009 | 7.2 | 619 | 1261 | 192 | 141 | 63 | <13 | 48 | 7 | 5.9 | 11 | 2.1 | 9.3 | <4 | 4.9 | <1 | 4 | <1 | 296 |
| NS-590 | 17 April 2009 | 7.3 | 474 | 1224 | 78 | 77 | 41 | <13 | <34 | 8 | 4.2 | 7 | 1.5 | 5.4 | <4 | 2 | <1 | <3 | <1 | 146 |
| NS-1200 | 17 April 2009 | 7.2 | 483 | 571 | 198 | 2190 | 268 | 33 | 128 | 31 | 11 | 35 | 5.3 | 28 | 5.9 | 14 | 2.3 | 11 | 2 | 2765 |
| NS-100 | 07 May 2009 | 7.2 | 536 | 1146 | 360 | 410 | 132 | 40 | 145 | 28 | 11 | 44 | 6.1 | 26 | 5.7 | 14 | 1.5 | 7 | 1.4 | 871 |
| NS-170 | 07 May 2009 | 7.4 | 524 | 1162 | 146 | 226 | 81 | 18 | 55 | 12 | 6.5 | 18 | 2.5 | 11 | 2.7 | 5 | <1 | 1.9 | <1 | 440 |
| NS-330 | 07 May 2009 | 7.6 | 513 | 1281 | 133 | 131 | 49 | 14 | 47 | 9.2 | 6 | 15 | 2.2 | 9.2 | 1.9 | 6 | <1 | 3 | <1 | 294 |
| NS-420 | 07 May 2009 | 7.8 | 516 | 1393 | 60 | 53 | 22 | 5.2 | 17 | <5 | 3.5 | 5 | 1 | 4 | <2 | 2 | <1 | <2 | <1 | 112 |
| NS-590 | 07 May 2009 | 7.8 | 505 | 1339 | 25 | 26 | <25 | <5 | 12 | <5 | 3 | <4 | <1 | 2 | <2 | <2 | <1 | <2 | <1 | 43 |
| NS-1200 | 07 May 2009 | 7.9 | 499 | 726 | 75 | 73 | 42 | 11 | 33 | 7 | 4 | 12 | 1.3 | 5 | <2 | 4.4 | <1 | 3.8 | <1 | 196 |
| NS-100 | 21 May 2009 | 7.2 | 523 | 1093 | 259 | 268 | 68 | 20 | 73 | 15 | 11.2 | 22 | 3.3 | 15 | 4.2 | 9 | 1.1 | 4 | <1 | 514 |
| NS-170 | 21 May 2009 | 7.5 | 505 | 1090 | 95 | 91 | 44 | 9.3 | 32 | 8 | 5.5 | 9.7 | 1.5 | 6.8 | <2 | 2.8 | <1 | <2 | <1 | 211 |
| NS-330 | 21 May 2009 | 7.7 | 490 | 1343 | 71 | 57 | <25 | 6 | 19 | <5 | 4.5 | 8 | 1.4 | 5.2 | <2 | 2.1 | <1 | <2 | <1 | 103 |
| NS-420 | 21 May 2009 | 7.8 | 545 | 1354 | 28 | <17 | <25 | <5 | 7 | <5 | <3 | <4 | <1 | <3 | <2 | <2 | <1 | <2 | <1 | 7 |
| NS-590 | 21 May 2009 | 8.0 | 513 | 1364 | 24 | 24 | <25 | <5 | 10 | <5 | 3.7 | <4 | <1 | 3.2 | <2 | <2 | <1 | <2 | <1 | 41 |
Table 2.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the Rio Naracauli waters, continues. ΣREE indicates the sum from La to Lu.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| NS-100 | 27 May 2009 | 7.3 | 525 | 1090 | 252 | 260 | 57 | 21 | 71 | 15 | 8 | 22 | 2.6 | 13 | 3.8 | 8 | 1.1 | 5 | 1.3 | 489 |
| NS-170 | 27 May 2009 | 7.6 | 502 | 1076 | 99 | 89 | 27 | 68 | 27 | 7 | 5.1 | 6 | 1.5 | 5.7 | <2 | 3.3 | <1 | 2.3 | <1 | 242 |
| NS-330 | 27 May 2009 | 7.8 | 490 | 1398 | 135 | 140 | 52 | 15 | 56 | 12 | 6.5 | 16 | 2.6 | 11 | 2.1 | 5 | <1 | 4.5 | <1 | 323 |
| NS-420 | 27 May 2009 | 8.0 | 473 | 1396 | 44 | 52 | 38 | 5.8 | 21 | 5 | 5.5 | 6.1 | 1.5 | 3.9 | <2 | <2 | <1 | <2 | <1 | 139 |
| NS-590 | 27 May 2009 | 8.2 | 436 | 1396 | 19 | 28 | <25 | <5 | 16 | <15 | 4.2 | 4.2 | <1 | <2 | <2 | <2 | <1 | <2 | <1 | 53 |
| NS-100 | 03 June 2009 | 7.4 | 525 | 1045 | 236 | 276 | 72 | 24 | 80 | 17 | 10 | 25 | 3.5 | 17 | 4 | 9 | 1.2 | 5.6 | <1 | 545 |
| NS-170 | 03 June 2009 | 7.6 | 486 | 1007 | 111 | 113 | 49 | 10 | 37 | 9 | 6.2 | 12 | 2.1 | 6.9 | 2 | 4 | <1 | 2.2 | <1 | 254 |
| NS-330 | 03 June 2009 | 7.8 | 467 | 1434 | 96 | 89 | 41 | 11 | 37 | 8 | 6 | 12 | 2.2 | 7.6 | <2 | 3 | <1 | 3.2 | <1 | 220 |
| NS-420 | 03 June 2009 | 7.9 | 450 | 1365 | 50 | 48 | 32 | <5 | 23 | 5 | 5 | 7 | 1.2 | 3 | <2 | <2 | <1 | <2 | <1 | 124 |
| NS-590 | 03 June 2009 | 8.1 | 450 | 1373 | 23 | 40 | 33 | <5 | 17 | <5 | 5 | <4 | 1.2 | <2 | <2 | <2 | <1 | <2 | <1 | 96 |
| NS-100 | 10 June 2009 | 7.5 | 445 | 1038 | 290 | 340 | 154 | 33 | 123 | 25 | 13 | 42 | 5.1 | 23 | 5.4 | 12 | 1 | 5.6 | <1 | 782 |
| NS-170 | 10 June 2009 | 7.6 | 429 | 1015 | 69 | 67 | 34 | 5.9 | 23 | 6 | 5.2 | 7 | 1.6 | 4.2 | <2 | 3 | <1 | <2 | <1 | 157 |
| NS-330 | 10 June 2009 | 7.8 | 424 | 1484 | 113 | 120 | 69 | 15 | 59 | 9 | 6 | 15 | 2.3 | 9.3 | 2.3 | 4.7 | <1 | 3.2 | <1 | 315 |
| NS-420 | 10 June 2009 | 7.9 | 407 | 1464 | 55 | 62 | 71 | 9.7 | 40 | 14 | 5.7 | 9.1 | 2 | 5.6 | <2 | 3 | <1 | 2.6 | <1 | 225 |
| NS-590 | 10 June 2009 | 8.2 | 387 | 1427 | 13 | <22 | <25 | <5 | <10 | <4 | 4.1 | <3 | <1 | <2 | <2 | <2 | <1 | <2 | <1 | 4 |
| NS-100 | 17 June 2009 | 7.3 | 471 | 1061 | 223 | 313 | 216 | 38 | 134 | 32 | 14 | 40 | 5.1 | 23 | 4.2 | 9.2 | 1.1 | 5 | 1 | 836 |
| NS-170 | 17 June 2009 | 7.5 | 451 | 1017 | 48 | 41 | <25 | <5 | 15 | <5 | 4.9 | 5.2 | <1 | 3.7 | <2 | <2 | <1 | <2 | <1 | 70 |
| NS-330 | 17 June 2009 | 7.6 | 447 | 1485 | 95 | 86 | 29 | 9 | 33 | 9 | 6 | 9 | 2.2 | 7 | <2 | 4 | <1 | 2 | <1 | 196 |
| NS-420 | 17 June 2009 | 7.8 | 435 | 1526 | 27 | 24 | <25 | <5 | <10 | <5 | 3.3 | 3.4 | 1 | <3 | <2 | <2 | <1 | <2 | <1 | 32 |
| NS-590 | 17 June 2009 | 8.0 | 417 | 1523 | 15 | 28 | 25 | <5 | 12 | <5 | 4 | 3 | <1 | <3 | <2 | <2 | <1 | <2 | <1 | 72 |
| NS-100 | 25 June 2009 | 7.4 | 457 | 1060 | 136 | 117 | <25 | 11 | 37 | 8 | 6 | 12 | 2.1 | 7.4 | <2 | 5 | <1 | 3 | <1 | 208 |
| NS-170 | 25 June 2009 | 7.5 | 449 | 1009 | 24 | 23 | <25 | <5 | <10 | <5 | 4.2 | <3 | <1 | <3 | <2 | <2 | <1 | <2 | <1 | 27 |
| NS-330 | 25 June 2009 | 7.7 | 446 | 1490 | 49 | 44 | <25 | <5 | 12 | <5 | 4.1 | 4.3 | 1.13 | <3 | <2 | 2 | <1 | <2 | <1 | 68 |
| NS-420 | 25 June 2009 | 7.8 | 450 | 1512 | 21 | <22 | <25 | <5 | 10 | <5 | <3 | <3 | <1 | <3 | <2 | <2 | <1 | <2 | <1 | 10 |
| NS-590 | 25 June 2009 | 8.0 | 448 | 1469 | 12 | <22 | <25 | <5 | <10 | <5 | 3.1 | <3 | <1 | <2 | <2 | <2 | <1 | <2 | <1 | 3 |
| NS-100 | 08 July 2009 | 7.1 | 422 | 887 | 188 | 201 | 61 | 21 | 75 | 14 | 7.4 | 22 | 3.6 | 14 | 3.8 | 11 | 1.1 | 6 | 1 | 442 |
| NS-170 | 08 July 2009 | 7.3 | 418 | 879 | 47 | 45 | 35 | 6 | 23 | 5 | 6.4 | 7 | 1.2 | 4.5 | <2 | 2 | <1 | <2 | <1 | 135 |
| NS-330 | 08 July 2009 | 7.9 | 422 | 1405 | 101 | 87 | 51 | 12 | 44 | 7.5 | 5.4 | 12 | 2.2 | 8.8 | 2 | 5.4 | <1 | 3.1 | <1 | 241 |
| NS-420 | 08 July 2009 | 7.7 | 422 | 1456 | 33 | 33 | <25 | <5 | 15 | 5 | 4.2 | 3.4 | <1 | 3 | <2 | <2 | <1 | <2 | <1 | 64 |
| NS-590 | 08 July 2009 | 7.9 | 416 | 1396 | 14 | <22 | <25 | <5 | <10 | <5 | 4 | <3 | <1 | <2 | <2 | <2 | <1 | <2 | <1 | 4 |
Table 3.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the Rio Naracauli waters, continues. ΣREE indicates the sum from La to Lu.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| NS-100 | 15 July 2009 | 7.3 | 460 | 837 | 186 | 228 | 136 | 30 | 110 | 23 | 6 | 26 | 3.5 | 18 | 4.2 | 8 | 1 | 9.7 | 1 | 604 |
| NS-170 | 15 July 2009 | 7.3 | 451 | 820 | 57 | <70 | 42 | <13 | 31 | <10 | 4.4 | <8 | 1.2 | 8 | <2 | 4 | <1 | <3 | <1 | 91 |
| NS-330 | 15 July 2009 | 7.6 | 442 | 1389 | 87 | 78 | 46 | <13 | 36 | 10 | 4.1 | 8.7 | 1.5 | 8.1 | <2 | 4.9 | <1 | 3 | <1 | 200 |
| NS-420 | 15 July 2009 | 7.7 | 445 | 1361 | 39 | <70 | 39 | <13 | <24 | <10 | <3 | <8 | 1 | 4 | <2 | <4 | <1 | <3 | <1 | 44 |
| NS-590 | 15 July 2009 | 8.0 | 432 | 1343 | 22 | <70 | 31 | <13 | <24 | <10 | <3 | <8 | <1 | <6 | <2 | <4 | <1 | <3 | <1 | 31 |
| NS-100 | 29 July 2009 | 7.4 | 445 | 775 | 119 | 114 | 52 | 14.4 | 53 | <10 | 5 | 14 | 1.7 | 9 | 2.4 | 5.4 | <1 | 4.2 | <1 | 275 |
| NS-170 | 29 July 2009 | 7.5 | 426 | 736 | 24 | <70 | 28 | <13 | <23 | <10 | 3 | <8 | <1 | <6 | <2 | <4 | <1 | <3 | <1 | 31 |
| NS-330 | 29 July 2009 | 7.7 | 404 | 1381 | 94 | 67 | 45 | <13 | 38 | <10 | 4.5 | <8 | 1.8 | 9 | <2 | 4.8 | <1 | 3.2 | <1 | 173 |
| NS-420 | 29 July 2009 | 7.8 | 422 | 1349 | 68 | 81 | 135 | 16 | 58 | 12 | 5 | 15 | 2.1 | 11 | 2.6 | 6 | <1 | 4.9 | <1 | 348 |
| NS-590 | 29 July 2009 | 8.1 | 407 | 1333 | 35 | <70 | 57 | <13 | 30 | <10 | 3 | 9.1 | 1 | <6 | <2 | <4 | <1 | <3 | <1 | 100 |
| NS-330 | 19 August 2009 | 7.5 | 459 | 1210 | 41 | <44 | <40 | 4 | 9 | 4 | <3 | <4 | <1.2 | 5 | 1 | <3 | <1 | <3 | <1 | 23 |
| NS-420 | 19 August 2009 | 7.7 | 452 | 1162 | 10 | <44 | <40 | <3 | 8 | <5 | <3 | <2 | <1.2 | <2 | <1 | <3 | <1 | <3 | <1 | 8 |
| NS-590 | 19 August 2009 | 8.0 | 440 | 1160 | 9 | <44 | <40 | <3 | 8 | <5 | <3 | <2 | <1.2 | <2 | <1 | <3 | <1 | <3 | <1 | 8 |
| NS-100 | 19 October 2009 | 6.9 | 473 | 557 | 76 | 90 | <40 | 13 | 37 | 8 | 3 | 6 | <1.2 | 6 | 1.4 | 3 | <1 | <3 | <1 | 167 |
| NS-170 | 19 October 2009 | 7.3 | 490 | 563 | 36 | 56 | <40 | 6 | 19 | 5 | <3 | <4 | <1 | 2.6 | <1 | <3 | <1 | <3 | <1 | 89 |
| NS-420 | 19 October 2009 | 7.7 | 475 | 1205 | 22 | <44 | <40 | <3 | <8 | <5 | <3 | 2.2 | <1 | <3 | <1 | <3 | <1 | <3 | <1 | 2.2 |
| NS-590 | 19 October 2009 | 8.0 | 407 | 1192 | 8 | <44 | <40 | <3 | <8 | <5 | <3 | <2 | <1.2 | <2 | <1 | <3 | <1 | <3 | <1 | |
| NS-1200 | 19 October 2009 | 7.4 | 453 | 803 | 45 | 64 | <40 | 8 | 26 | 5 | <3 | 6 | <1.2 | 3 | <1 | <3 | <1 | <3 | <1 | 112 |
| NS-100 | 11 November 2009 | 7.0 | 494 | 894 | 1720 | 4000 | 1560 | 550 | 1750 | 272 | 124 | 350 | 39 | 195 | 30 | 71 | 7.5 | 35 | 4 | 8988 |
| NS-420 | 11 November 2009 | 7.0 | 468 | 1084 | 310 | 740 | 360 | 76 | 220 | 32 | 14 | 46 | 5.1 | 24 | 4.8 | 13 | 1.2 | 7 | <1 | 1543 |
| NS-100 | 28 November 2009 | 7.1 | 482 | 803 | 104 | 214 | 46 | 21 | 70 | 12 | 5 | 12 | 2 | 11 | 1.8 | 4 | <1 | 3 | <1 | 402 |
| NS-420 | 28 November 2009 | 7.6 | 472 | 1371 | 25 | <44 | <40 | 4 | 12 | 3 | <3 | 3 | <1 | <2 | <1 | <3 | <1 | <3 | <1 | 22 |
| NS-590 | 28 November 2009 | 7.7 | 474 | 1284 | 10 | <44 | <40 | <3 | <8 | 3 | <3 | <2 | <1 | <2 | <1 | <3 | <1 | <3 | <1 | 3 |
| NS-100 | 17 March 2010 | 7.3 | 437 | 1006 | 389 | 590 | 439 | 69 | 218 | 33 | 21 | 51 | 7 | 34 | 6 | 14 | 1 | 6 | 1 | 1490 |
| NS-420 | 17 March 2010 | 7.6 | 451 | 1263 | 46 | 56 | 60 | 8 | 21 | 4 | 1 | 6 | <0.3 | 5 | 1 | 1 | <0.3 | <1 | <0.5 | 163 |
| NS-590 | 17 March 2010 | 7.7 | 465 | 1316 | 16 | 26 | 16 | 1.8 | 7 | <4 | 1 | 2 | <0.3 | <2 | <0.3 | <1 | <0.3 | <1 | <0.5 | 54 |
Table 4.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the Rio Naracauli waters, continues. ΣREE indicates the sum from La to Lu.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| NS-100 | 21 April 2010 | 7.4 | 456 | 1024 | 120 | 137 | 19 | 11 | 40 | 8 | 2.6 | 10 | 1.1 | 4.5 | 1.9 | 3.5 | 0.5 | <2 | <0.5 | 240 |
| NS-170 | 21 April 2010 | 7.5 | 450 | 1012 | 24 | 18 | 5 | <2 | 5.7 | 1 | 1.1 | <2 | 0.3 | <2 | 0.4 | <1 | <0.3 | <2 | <0.5 | 32 |
| NS-330 | 21 April 2010 | 7.6 | 445 | 1601 | 56 | 69 | 13 | 7.1 | 19 | <4 | 1.9 | 4 | 0.9 | 3 | 1 | 1.5 | <0.3 | <2 | <0.5 | 121 |
| NS-420 | 21 April 2010 | 7.8 | 435 | 1587 | 21 | 12 | <4 | <2 | <5 | 4 | 1 | <2 | <0.3 | <2 | <0.3 | <1 | <0.3 | <2 | <0.5 | 17 |
| NS-590 | 21 April 2010 | 8.0 | 431 | 1563 | 5.2 | 5.7 | 4 | <2 | <5 | 1.9 | <1 | <2 | <0.3 | <2 | 0.3 | <1 | <0.3 | <2 | <0.5 | 12 |
| NS-1200 | 21 April 2010 | 7.8 | 450 | 648 | 38 | 34 | 17 | 5 | 17 | 3 | 1 | 3 | 0.8 | 2 | 1.0 | 1.8 | <0.3 | 2 | <0.5 | 88 |
| NS-100 | 30 June 2010 | 7.5 | 469 | 1028 | 60 | 90 | 46 | 9 | 27 | <8 | <5 | <6 | <5 | <5 | <5 | <5 | <4 | <6 | <5 | 172 |
| NS-170 | 30 June 2010 | 7.5 | 457 | 996 | 26 | 85 | 108 | 13 | 36 | <8 | <5 | <6 | <5 | <5 | <5 | <5 | <4 | <6 | <5 | 242 |
| NS-330 | 30 June 2010 | 7.9 | 467 | 1493 | 62 | 66 | 70 | 10 | 33 | <10 | <5 | <6 | <5 | <5 | <5 | <5 | <4 | <6 | <5 | 179 |
| NS-420 | 30 June 2010 | 8.1 | 469 | 1485 | 15 | 27 | 36 | <9 | 12 | <8 | <5 | <6 | <5 | <5 | <5 | <5 | <4 | <6 | <5 | 75 |
| NS-590 | 30 June 2010 | 8.4 | 486 | 1473 | 14 | 42 | 60 | <9 | 19 | <8 | <5 | <6 | <5 | <5 | <5 | <5 | <4 | <6 | <5 | 121 |
| NS-1200 | 30 June 2010 | 8.0 | 447 | 1081 | 59 | 66 | 36 | <9 | 18 | <8 | <5 | <6 | <5 | 5 | <5 | <5 | <4 | <6 | <5 | 125 |
| NS-100 | 29 October 2010 | 7.2 | 475 | 949 | 100 | 93 | 20 | 8 | 29 | <4 | 4 | 9 | <1 | 6 | 1.9 | <3 | <1 | 2.8 | <1 | 174 |
| NS-170 | 29 October 2010 | 7.3 | 480 | 936 | 42 | 31 | 16 | 3.2 | 12 | <4 | 4 | 3.7 | <1 | <3 | <1 | <2 | <1 | <2 | <1 | 70 |
| NS-420 | 29 October 2010 | 7.8 | 475 | 1391 | 33 | 19 | <16 | 2 | 10 | <4 | 2.5 | 3.3 | <1 | <3 | <1 | <2 | <1 | <2 | <1 | 37 |
| NS-590 | 29 October 2010 | 8.0 | 482 | 1352 | 25 | 12 | <16 | 2 | 9 | <4 | 2 | 2 | <1 | 3 | <1 | 2 | <1 | 2 | <1 | 34 |
| NS-1200 | 29 October 2010 | 7.6 | 490 | 738 | 69 | 47 | 28 | 7 | 24 | 5 | 3 | 8 | 1.1 | 6 | 1.4 | 3.2 | <1 | 4 | <1 | 138 |
| NS-1600 | 29 October 2010 | 7.9 | 480 | 634 | 57 | 30 | 33 | 5 | 20 | 5 | 5 | 6 | 1.3 | 4 | 1.1 | 3 | <1 | 2.5 | <1 | 116 |
| NS-100 | 01 December 2010 | 7.2 | 608 | 1048 | 1580 | 3100 | 1180 | 290 | 1130 | 180 | 77 | 304 | 34 | 167 | 29 | 75 | 6 | 37 | 6 | 6615 |
| NS-420 | 01 December 2010 | 7.5 | 609 | 1145 | 610 | 1230 | 690 | 110 | 390 | 68 | 27 | 100 | 12 | 53 | 10 | 23 | 2.5 | 13 | 1.6 | 2730 |
| NS-590 | 01 December 2010 | 7.6 | 583 | 1089 | 130 | 195 | <260 | 18 | 60 | 9 | 6 | 17 | 2 | 8 | 1 | 5 | <1 | <3 | <1 | 321 |
| NS-1600 | 01 December 2010 | 8.0 | 555 | 452 | 100 | 117 | <260 | 21 | 83 | 17 | 8 | 18 | 3 | 15 | 3 | 8 | <1 | 7 | 1 | 301 |
| NS-100 | 26 January 2011 | 7.3 | 511 | 1034 | 375 | 341 | 75 | 28 | 100 | 18 | 9 | 31 | 4 | 22 | 6 | 13 | 1.4 | 7 | 1.1 | 657 |
| NS-330 | 26 January 2011 | 7.7 | 518 | 1290 | 136 | 117 | 28 | 8 | 34 | 7 | 4 | 12 | 1.5 | 7 | 1.8 | 6 | <1 | <10 | <1 | 226 |
| NS-420 | 26 January 2011 | 7.8 | 517 | 1243 | 76 | 74 | 32 | 7 | 24 | 7 | 3 | 8 | 1.5 | 5 | 1.7 | 3 | <1 | <3 | <1 | 166 |
| NS-590 | 26 January 2011 | 7.9 | 519 | 1208 | 36 | 62 | 29 | 5 | 20 | <10 | 4 | 5 | <1 | 3 | <1 | 2 | <1 | <3 | <1 | 130 |
| NS-1200 | 26 January 2011 | 7.8 | 548 | 607 | 65 | 243 | 73 | 10 | 40 | 10 | 4 | 9 | 1.5 | 7 | 2.4 | 5 | <1 | 4 | 1 | 410 |
| NS-1600 | 26 January 2011 | 7.9 | 585 | 535 | 86 | 128 | 58 | 13 | 47 | 12 | 5 | 14 | 1.7 | 8 | 2 | 5 | <1 | 3 | <1 | 297 |
Table 5.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the Rio Naracauli waters, ΣREE indicates the sum from La to Lu.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| NS-100 (h 10:50) | 02 February 2011 | 7.0 | 542 | 933 | 830 | 1100 | 330 | 107 | 420 | 70 | 30 | 120 | 14 | 61 | 14 | 34 | 3 | 20 | 3 | 2326 |
| NS-100 (h 13:30) | 02 February 2011 | 7.1 | 609 | 944 | 900 | 1500 | 480 | 150 | 550 | 90 | 35 | 150 | 18 | 77 | 16 | 43 | 4 | 23 | 4 | 3140 |
| NS-330 (h 11:00) | 02 February 2011 | 7.3 | 516 | 1138 | 460 | 550 | 175 | 56 | 220 | 38 | 17 | 58 | 8 | 38 | 8 | 18 | 2 | 11 | 2 | 1201 |
| NS-330 (h 13:42) | 02 February 2011 | 7.5 | 515 | 1133 | 420 | 520 | 176 | 58 | 200 | 37 | 17 | 56 | 8 | 35 | 7 | 16 | 2.3 | 10 | 1.8 | 1144 |
| NS-590 (h 11:05) | 02 February 2011 | 7.4 | 518 | 1086 | 143 | 200 | 69 | 15 | 62 | 13 | 6 | 12 | 2.5 | 9 | 2.2 | 5 | <1 | 3 | <1 | 399 |
| NS-590 (h 13:56) | 02 February 2011 | 7.4 | 533 | 1071 | 128 | 159 | 63 | 16 | 55 | 7 | 8 | 16 | 2.6 | 9 | 2 | 6 | <1 | <10 | <1 | 344 |
| NS-100 | 11 February 2011 | 7.3 | 519 | 1024 | 420 | 440 | 130 | 40 | 150 | 27 | 13 | 48 | 6 | 27 | 6 | 16 | 1.7 | 7 | 1.2 | 913 |
| NS-330 | 11 February 2011 | 7.8 | 513 | 1225 | 220 | 220 | 115 | 26 | 95 | 16 | 11 | 30 | 3.6 | 18 | 3.5 | 8 | <1 | 5 | <1 | 551 |
Table 6.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the tributary waters.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| Rio Pitzinurri (D) | 18 March 2009 | 8.3 | 471 | 304 | 50 | 46 | 73 | <13 | 39 | 11 | 3.2 | 9 | 1.5 | 7.3 | <4 | 4.8 | <1 | 3.9 | <1 | 199 |
| Rio Pitzinurri (D) | 19 October 2009 | 7.9 | 450 | 399 | 23 | <44 | <40 | 4.3 | 12 | 3 | <3 | 4 | <1.2 | 2.7 | <1 | <3 | <1 | <3 | <1 | 26 |
| Rio Pitzinurri (D) | 21 April 2010 | 8.2 | 440 | 285 | 19 | 18 | 23 | 4 | 13 | 4 | 1 | 2 | 0.7 | 2 | 0.8 | 2 | 0.51 | 2 | <0.5 | 73 |
| Rio Pitzinurri (D) | 29 October 2010 | 7.3 | 458 | 452 | 41 | 29 | 23 | 5.5 | 22 | <4 | 4 | 4 | <1 | 4 | 1 | 3 | <1 | 3 | <1 | 99 |
Table 7.
pH, redox potential (Eh), total dissolved solids (TDS) and Y-REE in the tailing drainages.
| Sample | Date | pH | Eh | TDS |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mV | mg/l | ng/l | ||||||||||||||||||
| A | 18 March 2009 | 6.9 | 473 | 2319 | 11100 | 29100 | 7700 | 3160 | 10800 | 1670 | 551 | 2368 | 255 | 1090 | 200 | 450 | 49 | 239 | 38 | 57670 |
| A | 25 March 2009 | 6.6 | 547 | 2377 | 11400 | 29900 | 8300 | 3000 | 10200 | 1520 | 508 | 2320 | 247 | 1060 | 192 | 455 | 46 | 228 | 34 | 58010 |
| A | 17 April 2009 | 6.5 | 659 | 2584 | 24400 | 35200 | 15100 | 4380 | 16100 | 2660 | 1020 | 4470 | 511 | 2260 | 430 | 1040 | 109 | 550 | 79 | 83909 |
| A | 07 May 2009 | 6.5 | 539 | 2577 | 11800 | 35000 | 9600 | 3860 | 13300 | 1900 | 720 | 3210 | 330 | 1360 | 230 | 570 | 59 | 290 | 44 | 70473 |
| A | 11 November 2009 | 6.6 | 452 | 2819 | 14200 | 33100 | 15300 | 4800 | 15400 | 2480 | 1100 | 3300 | 332 | 1600 | 250 | 600 | 66 | 280 | 32 | 78640 |
| A | 01 December 2010 | 6.7 | 503 | 2740 | 22000 | 46000 | 18000 | 4700 | 17700 | 2900 | 1120 | 4800 | 560 | 2300 | 400 | 800 | 100 | 490 | 77 | 99947 |
| A | 02 February 2011 | 6.6 | 591 | 2389 | 19000 | 37000 | 15000 | 4600 | 18000 | 2800 | 1000 | 4700 | 500 | 2100 | 400 | 900 | 100 | 420 | 70 | 87590 |
| A | 02 February 2011 | 6.9 | 646 | 2332 | 17000 | 32000 | 13000 | 4000 | 15000 | 2200 | 830 | 3700 | 400 | 1800 | 340 | 800 | 80 | 400 | 60 | 74610 |
| A | 11 February 2011 | 6.8 | 531 | 2826 | 18000 | 35000 | 14000 | 4400 | 17000 | 2500 | 1000 | 4400 | 500 | 2100 | 400 | 900 | 90 | 450 | 70 | 82810 |
| B | 25 March 2009 | 6.6 | 508 | 2220 | 6900 | 14500 | 8200 | 1255 | 4520 | 680 | 228 | 1230 | 127 | 560 | 104 | 236 | 21 | 107 | 17 | 31785 |
| B | 17 April 2009 | 6.4 | 656 | 1467 | 2970 | 6470 | 4030 | 574 | 2000 | 300 | 118 | 546 | 60 | 234 | 45 | 106 | 10 | 46 | 6.6 | 14546 |
| B | 07 May 2009 | 6.5 | 516 | 1928 | 5600 | 12800 | 7870 | 1170 | 3900 | 550 | 190 | 1030 | 110 | 460 | 91 | 190 | 20 | 76 | 12 | 28469 |
| B | 21 May 2009 | 6.2 | 580 | 2148 | 7470 | 18100 | 11800 | 1768 | 6120 | 930 | 334 | 1660 | 168 | 680 | 139 | 290 | 30 | 133 | 20 | 42170 |
| B | 27 May 2009 | 6.4 | 529 | 2210 | 6800 | 16900 | 10400 | 1570 | 5420 | 820 | 293 | 1490 | 154 | 610 | 123 | 270 | 27 | 123 | 20 | 38218 |
| B | 01 December 2010 | 7.0 | 606 | 2290 | 9900 | 27000 | 21000 | 2360 | 8750 | 1320 | 490 | 2270 | 220 | 940 | 160 | 410 | 33 | 150 | 28 | 65131 |
| B | 02 February 2011 | 6.6 | 541 | 1251 | 2600 | 5500 | 3500 | 550 | 1900 | 300 | 120 | 500 | 60 | 250 | 48 | 115 | 11 | 56 | 9 | 12919 |
| B | 02 February 2011 | 7.0 | 524 | 1247 | 2500 | 5700 | 3600 | 540 | 2000 | 310 | 120 | 540 | 60 | 250 | 50 | 110 | 12 | 55 | 8 | 13355 |
| B | 11 February 2011 | 7.0 | 515 | 1659 | 3700 | 8600 | 5100 | 820 | 3000 | 460 | 160 | 800 | 80 | 330 | 69 | 160 | 15 | 67 | 11 | 19672 |
Table 8.
Y-REE and Th concentrations in mine tailings.
| Sample | Date |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
Th |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mg/kg | ||||||||||||||||||
| MTA - 1 | 28 April 2012 | 6 | 14 | 30 | 3 | 11 | 3 | 1 | 3 | 0.26 | 2 | 0.32 | 0.88 | 0.1 | 0.76 | 0.08 | 1.7 | 69 |
| MTA - 2 | 28 April 2012 | 20 | 76 | 131 | 14 | 50 | 10 | 3.2 | 8.6 | 0.73 | 3.3 | 0.5 | 1.3 | 0.15 | 1 | 0.13 | 7.3 | 300 |
| MTA - 3 | 28 April 2012 | 3 | 25 | 53 | 5.4 | 20 | 3.5 | 0.97 | 2.6 | 0.29 | 1.3 | 0.2 | 0.57 | 0.05 | 0.45 | 0.05 | 3.9 | 113 |
| MTB - 1 | 28 April 2012 | 3.7 | 9.8 | 23 | 2.2 | 10 | 2.2 | 1 | 2.1 | 0.23 | 0.99 | 0.16 | 0.42 | 0.04 | 0.23 | 0.04 | 1.1 | 52 |
| MTB - 2 | 28 April 2012 | 1.2 | 6.9 | 14 | 1.5 | 5.5 | 1.2 | 0.47 | 1 | 0.12 | 0.62 | 0.1 | 0.26 | 0.04 | 0.22 | 0.02 | 1 | 32 |
| MTB - 3 | 28 April 2012 | 0.98 | 2.8 | 6.37 | 0.7 | 2.9 | 0.77 | 0.3 | 0.7 | 0.1 | 0.5 | 0.09 | 0.23 | 0.03 | 0.2 | 0.02 | 0.7 | 16 |
Table 9.
Y-REE and Th concentrations in the bio-hydrozincites (N34-42) and Fe-hydrozincite + bio-hydrozincite sample (N32).
| Sample | Date | Location |
Y |
La |
Ce |
Pr |
Nd |
Sm |
Eu |
Gd |
Tb |
Dy |
Ho |
Er |
Tm |
Yb |
Lu |
Th |
∑ REE |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| mg/kg | |||||||||||||||||||
| N32 | 21 May 2009 | NS-170 | 60 | 70 | 55 | 7.5 | 30 | 5.7 | 2.6 | 10 | 1.3 | 6 | 1 | 2.3 | 0.2 | 1 | 0.1 | <0.44 | 193 |
| N34 | 27 May 2009 | NS-590 | 3.4 | 3.7 | 2.0 | 0.42 | 1.5 | 0.3 | 0.1 | 0.42 | 0.06 | 0.25 | 0.06 | 0.13 | 0.02 | 0.08 | 0.01 | 0.76 | 9.0 |
| N36 | 03 June 2009 | NS-590 | 5.2 | 8.4 | 8.8 | 1.4 | 5.2 | 1 | 0.25 | 1.2 | 0.14 | 0.67 | 0.12 | 0.31 | 0.04 | 0.26 | 0.03 | 1.3 | 28 |
| N37B | 10 June 2009 | NS-420 | 8.2 | 8.8 | 5.1 | 1.1 | 3.9 | 0.7 | 0.24 | 1.0 | 0.13 | 0.65 | 0.13 | 0.33 | 0.04 | 0.24 | 0.03 | 0.47 | 22 |
| N39 | 15 July 2009 | NS-420 | 3.1 | 1.9 | 0.67 | 0.2 | 0.78 | 0.15 | 0.05 | 0.19 | 0.04 | 0.21 | 0.03 | 0.11 | 0.01 | 0.08 | 0.01 | <0.44 | 4.4 |
| N41A | 29 July 2009 | NS-420 | 4.6 | 3.4 | 1.3 | 0.4 | 1.4 | 0.25 | 0.1 | 0.42 | 0.06 | 0.3 | 0.08 | 0.15 | 0.03 | 0.12 | 0.02 | <0.44 | 8.0 |
| N42 | 29 July 2009 | NS-420 | 2.9 | 2.1 | 1.1 | 0.3 | 0.94 | 0.16 | 0.06 | 0.28 | 0.04 | 0.19 | 0.04 | 0.1 | 0.01 | 0.08 | 0.01 | <0.44 | 5.4 |
2. Experimental design, materials, and methods
Mine waste samples were dried at room temperature, and ground for X ray diffraction analysis that was performed using a conventional θ–2θ equipment (Panalytical) with Cu Kα wavelength radiation (λ = 1.54060 Å), operating at 40 kV and 40 mA, using the X׳Celerator detector. For chemical analysis, biominerals (hydrozincite) and mine waste samples were ground and acid digested by a microwave (ETHOS One, Advanced Microwave Digestion System, Milestone), according to [1]. To evaluate accuracy and precision of the laboratory procedures, samples were processed together with the reference material RTS-3 (CANMET, Canadian Certified Reference Materials Project (CCRMP)) prepared with the same mixture.
Water samples were collected from 2009 to 2011 and consist of i) stream waters (NS-100 to NS-1600), ii) tributary (labeled by D), and iii) tailing drainages (labeled by A and B). Redox potential (Eh) and pH were determined on site according to [1].
REE in acid digested samples and in water samples were determined on filtered (0.4 μm, Nuclepore 111130) and acidified aliquots (1% HNO3 ultrapure grade) by inductively coupled plasma mass spectrometry (ICP-MS, Perkin-Elmer, Elan 5000/DRC-e, USA) with the desolvation system Apex-Q, that increases the sensitivity and reduces the interferences due to oxides according to [11]. Also, the standard addition method [12] was used in some water samples characterized by different compositions. To quantify yttrium and REE in the water and solid samples the isotopes 89Y, 139La, 140Ce, 141Pr, 142Nd, 146Nd, 147Sm, 152Sm, 151Eu, 153Eu, 157Gd, 158Gd, 159Tb, 163Dy, 164Dy, 165Ho, 166Er, 167Er, 169Tm, 172Yb, 174Yb, and 175Lu were used.
For investigating fractionation processes of REE during precipitation of the solid phases, solid samples and waters were collected in the same station at the same time.
Acknowledgments
This paper was funded by EU grant 226870 UMBRELLA (coordinator Erika Kothe, University of Jena). The UMBRELLA project was funded by the European Commission, FP7-ENVIRONMENT, ENV.2008.3.1.2.1. - Recovery of degraded soil resources.
Footnotes
Transparency data associated with this article can be found in the online version at https://doi.org/10.1016/j.dib.2018.12.064.
Contributor Information
Daniela Medas, Email: dmedas@unica.it.
Rosa Cidu, Email: cidur@unica.it.
Giovanni De Giudici, Email: gbgiudic@unica.it.
Francesca Podda, Email: fpodda@unica.it.
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