| Literature DB >> 30211289 |
Kefa K Onchoke1, Christopher M Franclemont1, Paul W Weatherford2.
Abstract
The data presented in this article is related to the research article entitled, "Structural Characterization and Evaluation of Municipal Wastewater Sludge (Biosolids) from two Rural Wastewater Treatment Plants in East Texas, USA" (Onchoke et al., [1]). The XRD profiles and composition of biosolids from two wastewater treatment plant is presented. This study describes the composition of XRD crystalline phase patterns of the wastewater sludge. After the removal of the Kα2 peaks the d-spacing and hkl values were determined. In addition, the ion chromatographic profile of the seven anions ( NO3- , NO2- , Br-, Cl-, F-, SO42- , and PO43- ) in biosolids is presented.Entities:
Year: 2018 PMID: 30211289 PMCID: PMC6134169 DOI: 10.1016/j.dib.2018.08.087
Source DB: PubMed Journal: Data Brief ISSN: 2352-3409
Fig. 3Powder XRD patterns of samples from the Nacogdoches Wastewater Treatment Plant (A), and Lufkin Wastewater Treatment Plant (B). The 2θ values and d-spacing values corresponding to each crystalline phases are also shown. The crystalline phases corresponding to each peak(s) are presented in Table 1, Table 2, respectively.
Analysis of the Crystalline Phases, d-spacing, and h, k, l values of biosolids in NWWTP [1].
| Index | Angle | Net Intensity | Gross Intensity | Rel. Intensity | Mineral | ||
|---|---|---|---|---|---|---|---|
| 0 | 6.217 | 14.20528 | 2756 | 10,258 | 31.40% | 0 0 2 | Vermiculite |
| 1 | 20.756 | 4.27606 | 1703 | 6741 | 19.40% | 1−2 −1 | Alunogen |
| 1 −2 −1 | Hexahydrite | ||||||
| 1−2−1 | Quartz | ||||||
| 2 | 22.663 | 3.92039 | 258 | 4887 | 2.90% | 0 3 1 | Gypsum |
| 3 | 25.201 | 3.53096 | 255 | 4588 | 2.90% | 2 2 1 | Laumontite |
| 4 | 26.422 | 3.37054 | 3254 | 7472 | 37.10% | 3 1 2 | Laumontite |
| 5 | 26.53 | 3.35703 | 8779 | 12,982 | 100.00% | 0 1 1 | Quartz |
| 6 | 27.266 | 3.26809 | 341 | 4425 | 3.90% | 1 0 1 | Quartz |
| 7 | 27.359 | 3.25717 | 296 | 4365 | 3.40% | 1 1 6 | Vermiculite |
| 1 -3 1 | Mirabilite | ||||||
| 8 | 27.886 | 3.19679 | 225 | 4182 | 2.60% | 1 1 2 | Annite Mica |
| 9 | 31.569 | 2.83182 | 196 | 3637 | 2.20% | 0 2 8 | Vermiculite |
| 10 | 32.373 | 2.7633 | 212 | 3602 | 2.40% | 2 −3 −1 | Gypsum |
| 11 | 35.837 | 2.50374 | 274 | 3498 | 3.10% | 3 2 −3 | Vermiculite |
| 1 3 3 | Antigorite T | ||||||
| 1 −3 1 | Talc | ||||||
| 12 | 35.963 | 2.49521 | 171 | 3401 | 1.90% | 1 3 −11 | Antigorite T |
| 13 | 36.148 | 2.48288 | 157 | 3389 | 1.80% | 1 -3 2 | Annite Mica |
| 14 | 36.39 | 2.46693 | 501 | 3726 | 5.70% | 1 1 0 | Quartz |
| 15 | 38.122 | 2.3587 | 157 | 3189 | 1.80% | 0 0 3 | Kaolinite |
| 16 | 38.325 | 2.34672 | 160 | 3168 | 1.80% | 1 -3 1 | Kaolinite |
| 17 | 39.336 | 2.28866 | 502 | 3449 | 5.70% | 1 0 2 | Quartz |
| 0 1 2 | |||||||
| 18 | 40.173 | 2.24291 | 243 | 3181 | 2.80% | 1 1 1 | Quartz |
| 19 | 42.263 | 2.13671 | 265 | 3079 | 3.00% | 0 2 0 | Quartz |
| 20 | 45.719 | 1.98288 | 275 | 2919 | 3.10% | 2 0 1 | Quartz |
| 0 2 1 | |||||||
| 21 | 48.994 | 1.85774 | 131 | 2513 | 1.50% | 0 6 2 | Laumontite |
| 22 | 49.996 | 1.82283 | 1566 | 3964 | 17.80% | 1 1 2 | Quartz |
| 23 | 55.225 | 1.66197 | 145 | 2426 | 1.70% | 0 1 3 | Quartz |
| 24 | 59.809 | 1.54506 | 598 | 2789 | 6.80% | 2 1 1 | Quartz |
| 1 2 1 | |||||||
| 25 | 67.57 | 1.38524 | 305 | 2359 | 3.50% | 1 2 2 | Quartz |
| 2 1 2 | |||||||
| 26 | 68.019 | 1.37718 | 781 | 2833 | 8.90% | 0 2 3 | Quartz |
| 2 0 3 | |||||||
| 27 | 68.16 | 1.37468 | 553 | 2596 | 6.30% | 3 0 1 | Quartz |
| 0 3 1 | |||||||
| 28 | 73.358 | 1.28957 | 239 | 2203 | 2.70% | 0 1 4 | Quartz |
| 1 0 4 | |||||||
| 29 | 75.597 | 1.25684 | 393 | 2319 | 4.50% | 0 3 2 | Quartz |
| 3 0 2 | |||||||
| 30 | 79.662 | 1.20261 | 271 | 1528 | 3.10% | 2 1 3 | Quartz |
| 1 2 3 |
Analysis of the crystalline phases, d-spacing, and h, k, l values of biosolids in LWWTP [1].
| Index | Angle | Net Intensity | Gross Intensity | Rel. Intensity | Mineral | ||
|---|---|---|---|---|---|---|---|
| 0 | 6.196 | 14.25293 | 2843 | 10,629 | 36.20% | 0 0 2 | Vermiculite |
| 1 | 11.645 | 7.59308 | 554 | 4410 | 7.10% | 0 2 0 | Gypsum |
| 2 | 19.881 | 4.46235 | 524 | 4195 | 6.70% | 1 0 1 | Andalusite |
| 3 | 20.825 | 4.26215 | 1469 | 5156 | 18.70% | 0 1 0 | Quartz Gypsum |
| 1 −2 −1 | |||||||
| 4 | 25.287 | 3.51915 | 198 | 3358 | 2.50% | 2 2 1 | Laumontite |
| 5 | 26.622 | 3.34568 | 7847 | 10,898 | 100.00% | 0 1 1 | Quartz |
| 1 0 1 | |||||||
| 6 | 27.008 | 3.29879 | 313 | 3309 | 4.00% | 2 4 1 | Palygorskite |
| 7 | 27.737 | 3.21372 | 792 | 3667 | 10.10% | 2 2 1 | Palygorskite |
| 8 | 29.104 | 3.06578 | 478 | 3225 | 6.10% | 1 4 −1 | Gypsum |
| 9 | 31.083 | 2.87493 | 297 | 2862 | 3.80% | 2 -2 -2 | Vermiculite, |
| 3 −1 −4 | Hexahydrite | ||||||
| 10 | 31.761 | 2.81512 | 131 | 2644 | 1.70% | 1 1 1 | Laumonthite |
| 3 −1 −4 | |||||||
| 11 | 33.327 | 2.68633 | 225 | 2515 | 2.90% | 1 −3 −1 | Annite Mica |
| 12 | 33.411 | 2.67978 | 139 | 2421 | 1.80% | 0 6 1 | Vermiculite |
| 13 | 35.938 | 2.49691 | 150 | 2436 | 1.90% | 2 0 -2 | Actolite |
| 14 | 36.5 | 2.45972 | 537 | 2768 | 6.80% | 1 3 4 | Vermiculite |
| 1 1 0 | Quartz | ||||||
| 15 | 37.734 | 2.3821 | 150 | 2246 | 1.90% | 1 1 0 | Corundum |
| 16 | 39.426 | 2.28366 | 479 | 2517 | 6.10% | Quartz Vermiculite | |
| 17 | 40.251 | 2.23874 | 216 | 2246 | 2.80% | 1 1 1 | Quartz + Palygorskite |
| 4 −2 −2 | |||||||
| 18 | 42.44 | 2.12817 | 254 | 2218 | 3.20% | 3 5 1 | Quartz + Palygorskite |
| 19 | 43.236 | 2.09083 | 121 | 2029 | 1.50% | 0 2 0 | Quartz |
| 20 | 43.647 | 2.07209 | 141 | 2014 | 1.80% | 1 1 3 | Corundum |
| 21 | 45.571 | 1.989 | 126 | 1929 | 1.60% | 2 0 1 | Hexahydrite |
| 0 2 1 | |||||||
| 22 | 45.769 | 1.98085 | 274 | 2070 | 3.50% | 2 0 1 | Quartz |
| 0 2 1 | |||||||
| 23 | 46.944 | 1.93396 | 125 | 1844 | 1.60% | 3 −1 1 | Turquoise |
| 24 | 47.998 | 1.89391 | 137 | 1818 | 1.70% | 0 0 2 | Boehemite |
| 25 | 48.374 | 1.88009 | 106 | 1778 | 1.30% | 4 0 −4 | Laumonite |
| 26 | 50.115 | 1.81878 | 758 | 2421 | 9.70% | 1 1 2 | Quartz |
| 27 | 54.851 | 1.6724 | 318 | 1872 | 4.10% | 2 0 2 | Quartz |
| 0 2 2 | |||||||
| 28 | 59.932 | 1.54218 | 513 | 1930 | 6.50% | 1 2 1 | Quartz |
| 2 1 1 | |||||||
| 29 | 67.736 | 1.38224 | 357 | 1704 | 4.50% | 1 2 2 | Quartz |
| 2 1 2 | |||||||
| 4 4 0 | |||||||
| 30 | 68.112 | 1.37553 | 603 | 1954 | 7.70% | Quartz Vermiculite | |
| 31 | 68.106 | 1.37564 | 625 | 1976 | 8.00% | Quartz Vermiculite | |
| 32 | 73.466 | 1.28794 | 234 | 1546 | 3.00% | 014 | Quartz |
| 104 | |||||||
| 33 | 75.625 | 1.25645 | 133 | 1320 | 1.70% | 032 | Quartz |
| 302 | |||||||
| 34 | 75.702 | 1.25536 | 88.4 | 1266 | 1.10% | 032 | Quartz |
| 35 | 85.016 | 1.14001 | 20.7 | 66.3 | 0.30% | 204 | Quartz |
| 024 |
Fig. 2Representative elution profile of the seven anions and retention times. 1 = F−, 2 = Cl−, 3 = NO2−, 4 = Br−, 5 = NO3−, 6 = PO43−, 7 = SO42−. The standard was diluted X20 times. The Dionex Integrion HPIC ion chromatograph (Thermo Fisher Scientific Inc., USA) was used. A Dionex IonPac AS22 analytical column (2 × 250 mm) thermostated at 30 °C, guard column (IonPac AG22), a Dionex AS 22 Eluent Concentrate (4.5 mM sodium carbonate/1.4 mM sodium bicarbonate) was used.
Fig. 1Aerial photographs of (a) Nacogdoches wastewater treatment plant (NWWTP), and (b) Lufkin wastewater treatment plant (LWWTP). In each of the pictures, 4 clarifiers are observed.
Fig. 4Representative SEM micrograph of LWWTP biosolid showing particle size diameters (magnification 40×, Voltage applied =15 kV).
Fig. 5Representative SEM micrograph of the LWWTP biosolid with measurement of smaller particles; magnification 100×, and 200×.
Fig. 6SEM micrograph of a pore from the NWWTP biosolid with measurement of its diameter; magnification 3 kV (a) and 5 kV (b).
| Subject area | |
| More specific subject area | |
| Type of data | |
| How data was acquired | |
Dionex Integrion HPIC ion chromatograph (Thermo Fisher Scientific Inc., USA) was used for anion analysis. A Bruker AXS D8 Advance diffractometer equipped with an X-ray tube (Cu Kα radiation: λ = 1.54060 Å, 40 kV, and 40 mA) using a Ni filter and one-dimensional LynxEye detector at scanning speed of 2 °/min and 0.0125 ° step sizes and a 1 s/step. A JEOL-JSM 6100 scanning electron microscope equipped with a Horiba energy dispersive X-ray spectroscopy (SEM/EDX) was used. | |
| Data format | Raw, filtered, analyzed |
| Experimental factors | For XRD analysis: Biosolid samples were obtained from Nacogdoches and Lufkin wastewater treatment plant (NWWTP, LWWTP), air dried, and ground to powder. For IC analysis: samples were filtered on a 0.45 μm filter. |
| Experimental features | Wastewater sludge generated from the rural municipal wastewater treatment plants are applied for land. We provide the characterization of the crystalline phases in the biosolids. The powder diffraction file was acquired using Bruker AXS DIFFRAC.EVA program |
| Data source location | Nacogdoches, East Texas, in East Texas, USA latitude: 31° 33′ 31.2444′′ N and longitude 94° 38′ 52.1808′′ W, |
| Data accessibility | All data are available within this article. |
| Related research article | Associated Paper: “Structural Characterization and Evaluation of Municipal Wastewater Sludge (Biosolids) from two Rural Wastewater Treatment Plants in East Texas, USA”, Onchoke, K.K, Franclemont, C.M., Spectrochim Acta A, In press |