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213 protocols using whatman filter paper no 42

1

Analytical Protocol for Trace Elemental Analysis

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Water
Water samples were directly analyzed for the estimation of total arsenic [12 (link)].
Fodder
Fodder samples (1 g) were digested using 15 ml of tri-acid mixture (HNO3, H2SO4, and HClO4 in 10:4:1 ratio) until a transparent solution was obtained [13 ]. After cooling, the digested sample was filtered using Whatman No. 42 filter paper, and the volume was made to 10 ml with doubled distilled water.
Blood
Blood samples (3 ml) were digested after adding 15 ml of tri-acid mixture (HNO3, H2SO4, and HClO4 in 10:4:1 ratio) until a transparent solution was obtained [14 (link)]. After cooling, the digested samples were filtered using Whatman No. 42 filter paper and the volume was made to 10 ml with doubled distilled water.
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2

Soil Heavy Metal Analysis Protocol

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Soil samples were digested in Teflon beakers by taking 1g soil with 15 mL tri acid mixture of HNO3, HClO4 and H2SO4 at a 5:1:1 ratio at a temperature of 100°C. The mixture was heated until a clear solution was formed. After cooling, the digested sample was filtered using Whatman No. 42 filter paper and the volume of the filtrate was made 50 mL by adding double de-ionized water. The filtrate was then analyzed for heavy metals i.e. Pb, Cr, Cd, Ni, Zn, Cu, Fe and Mn by using AAS in air acetylene flame mode [19 ]. The suspension was filtered through Whatman No. 42 filter paper. pH and EC were assayed through digital Cole Parmer 5983 pH meter and EC meter InoLab model E 163694 at room temperature.
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3

Soil Heavy Metal Quantification

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Both total and diethylenetriaminepentaacetic acid (DTPA)-extractable fractions of heavy metals (Ni, Zn, and Fe) were measured in the soil. To analyze the total metal content, three replicates of 1 g of soil were weighed and 10.5 mL of aqua regia were added to each sample according to Kilburn (2000) . The digestion tubes were allowed to stand overnight to equilibrate the aqua regia with the soil and then were put onto a hotplate for 3 h at 110°C. The digests were filtered through Whatman No. 42 filter paper and mixed with deionized water in volumetric flask reaching 25 mL. The concentration of heavy metals in soil extracts was measured by atomic absorption spectrophotometry (AAS; PerkinElmer model 100, MA, USA).
Diethylenetriaminepentaacetic acid-extractable metals were measured by extracting 10 g samples of soil with 20 mL of extracting solution (0.005 M DTPA, 0.01 M CaCl2, 0.1 M Triethanolamine, pH 7.3) according to the procedure of Lindsay and Norvell (1978) (link). The mixtures were agitated on a horizontal shaker for 2 h at room temperature and were then through Whatman No. 42 filter paper prior to analysis by AAS.
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4

Phosphate Desorption from Microplastics

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Desorption experiments following the method of Han et al. [53 ] were undertaken to determine whether MPs could release previously sorbed phosphate and to compare desorption with that from soils. Solids from the initial adsorption experiments were collected on Whatman No. 42 filter paper and washed with 30 mL saturated NaCl to remove free P. Solids were then added to 30 mL of 0.10 M NaNO3. The mixtures were shaken at 180 rpm for 24 h, filtered using Whatman No. 42 filter paper and finally the supernatants were analyzed using ICP-OES to determine P concentration in the solution.
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5

Optimizing Lactic Acid Adsorption Using CMC-CSAC

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A variety of CMC-CSAC adsorbents (5 g) previously prepared as previously stated was mixed with 50 mL cell-free lactic acid fermentation broth (pH 6). The mixture was stirred at room temperature for 150 min before filtering through Whatman filter paper No.42. The liquid portion was kept for analyses of metal ions and lactic acid concentration using atomic adsorption spectrophotometry (AAS), high performance liquid chromatography (HPLC), and ion chromatography (IC).
The optimal contact time was determined. Five g of CMC-CSAC adsorbent grafted with 2% CMC and 20% CA was mixed with 50 mL cell-free lactic acid fermentation broth at room temperature. The contact time was varied (0–24 h). Later, the mixture was filtered through Whatman filter paper No.42. The liquid portion was kept for analyses of metal ions and lactic acid. The effect of the initial pH of the fermentation broth and operating temperature on ion adsorption onto CMC-CSAC was studied. After harvesting, lactic acid fermentation broth had an initial pH of 6. The pH was adjusted to 2 by adding 10 M H2SO4. The adsorption capacity was also investigated by varying the ratio of lactic acid fermentation broth (L) to solid CMC-CSAC adsorbent (S) from 2.5 to 20.
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6

Soil Nitrogen Mineralization and Nitrification

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N mineralization and nitrification were assessed by the modified anaerobic incubation method [27] . Briefly, fresh soil samples (5 g) were placed into a 200 mL plastic bottles, 10 mL deionized water was added to the bottles to thoroughly submerge the soil. The plastic bottles were sealed with stopper to avoid water evaporation during incubation, and placed in a constant temperature (40°C) incubator for 7 days. At the beginning of the incubation experiment, pre-incubation soil was sampled to measure the initial concentrations of NH4+-N and NO3-N. After a week of incubation, the post-incubation soil samples were mixed with 40 mL of 2 M KCl using a 1: 8 soil: extractant (w/v) ratio, shaken for 30 min on a reciprocal shaker; then the extracts were filtered through prewashed Whatman no. 42 filter papers and supernatants were stored at −20°C until analysis of NH4+-N and NO3-N concentrations. The NH4+-N and NO3-N concentrations were separately measured by spectrophotometry using the ammonium indophenol blue method and the cadmium reduction method [28] . All concentrations of NH4+-N and NO3-N were based on dry soil weight and expressed on a mg·g−1 (DW). The N mineralization rate (Nmin) was calculated as the changes in the inorganic N (NH4+-N, NO3-N) content from time zero to 7 days. A similar formula was used to calculate N nitrification rate (Nnitri) [29] , [30] :

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7

Soil Selenium and Sulfur Extraction

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The soil extractable Se and S were determined using two different P solutions (0.016 M KH2PO4 (pH = 4.8) and 0.016 M P-buffer (NaH2PO4/Na2HPO4, pH = 7.5)). KH2PO4 is an established reagent for extracting plant-available S (Zhao and McGrath 1994 (link)). Due to the chemical similarity between SO42− and SeO42−, the reagent is used to extract Se from soil (Stroud et al. 2010 ). The use of P-buffer in this study is a new attempt to investigate the effect of a different pH environment on Se sorption in the soil. A 5 g-DM soil sample was weighed into a 50 mL sample tube followed by adding 25 mL of one of the P solutions and extracted for 1 h at 25 °C. After extraction, the extracts were filtered through Whatman No.42 filter papers. The supernatants were acidified in 5% HNO3 (v/v) before analysis of total Se and S in the extracts using ICP-OES or ICP-MS. The analysis of soil extractable P followed the method of Olsen et al. (1954 ).
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8

Nutrient Concentration Analysis in T. luteum subsp. gabesianum

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All dried parts (including shoots and leaves) of each treatment were ground through a 40-mesh sieve to determine the tissue nutrient concentration in T. luteum subsp. gabesianum. Three samples of fine powder were made corresponding to the three fertilization treatments (ChF, INM, control) applied. Each sample was further divided into three subsamples of ca. 0.25 g each, and each subsample was disorganized by the method of wet oxidation using a triple acid mixture of H2SO4, HNO3, and HClO4 in a ratio of 5:1:1 at 80 °C until a transparent solution was obtained [53 ]. The digested samples were filtered using Whatman No. 42 filter papers and the filtrates were finally complemented with distilled water up to 50 mL. The solutions were analyzed for total P colorimetrically according to the Molybdenum Blue Method by using a Shimadzu spectrophotometer model UV-1201V [54 ]. The total concentrations of magnesium (Mg), potassium (K), calcium (Ca), sodium (Na), copper (Cu), iron (Fe), zinc (Zn), and manganese (Mn) were determined by atomic absorption spectroscopy (Perkin-Elmer Analyst 300). Acetylene gas was used as fuel and air as a supportive agent. An oxidizing flame was used in all cases. Furthermore, for the determination of N, three sub-samples of ca. 0.25g each of the powder were taken from each sample. Total N was determined by the Kjeldahl method [55 ].
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9

Determining the pH Zero Point Charge of Beads

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To determine the pH zero point charge of the beads, pH drift equilibrium technique was employed. Ten conical flasks each containing 50 mL of 0.01 M NaCl was taken and the pH was adjusted from 1 to 10 using NaOH and H2SO4. A known quantity of composite beads was added to each flask and the flasks were equilibrated for 48 h. The final pH measured after 48 h was plotted against the initial pH and the intersection point was taken as pHzpc of the bead.27 (link) For zeta potential analysis, the solution was agitated for 2 h in a mechanical shaker before sonicating. After sonication, the solution was filtered using Whatman no. 42 filter paper and supernatant was collected and analysed for its surface charges in particle size analyser (Horiba Scientific Nanopartica SZ-100, Japan).28
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10

Comprehensive Pomegranate Extraction Protocol

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Leaves and fruits were harvested from Tounsi pomegranate trees in October 2021 from Mahdia region, Tunisia. Variety authenticity was confirmed by taxonomist Dr. Faten Zaouay from the Department of Horticulture, Higher Agronomic Institute, Chott-Meriem (University of Sousse, Tunisia) and a voucher specimen was deposited in our national collection maintained in duplicate at Gabes and Chott-Mariem (Sousse), with the code ‘TNl, TN2, TN3, TN5, TN5”.
Pomegranate extracts were prepared as described by our previous study [11 (link)]. Fruits were washed and hand-peeled. Arils were squeezed using a commercial blender (moulinex, France). The extract juice was centrifuged at 15000 rpm for 15 min. Then the supernatant was recuperated and lyophilized. Leaves, flowers and fruit peel were dried, powdered and extracted with methanol (MeOH) 50 g/250 ml in the dark for 48 hours. Each extract was filtered through Whatman No. 42 filter paper and evaporated to dryness using a rotary evaporator (Heidolph, Germany) under vacuum at 45 °C and stored at − 20 °C for further determination. Pomegranate seeds were dried and powdered. Oil was extracted by the methods of soxhlet. About 30 g seeds were extracted with 200 ml of hexane at room temperature for 6 h. The solvent was removed by evaporation at 40 °C and the oil was flushed with nitrogen stream and stored at − 20 °C in sealed tubes.
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