Understanding the Chemistry of Direct Aqueous Carbonation with Additives Through Geochemical Modelling

Amongst possible mineral carbonation strategies, direct aqueous mineral carbonation using organic salts is perhaps the most promising one. By going to and from between geochemical modelling and experimental results, this paper reviews key findings and conclusions to date about this process. With the magnesium silicate – oxalate system, the paper makes a strong case for the necessity to characterize both solid and liquid phases in order to analyze any aqueous mineral carbonation test results. It is shown that partial information about reaction products, such as liquid phase analysis without characterization of the associated solid phase, can easily lead to flawed conclusions. Proper analysis of solid products is recognized however to complicate experimental work considerably, with many analytical techniques being required to reveal the true nature of the solid phases present in aqueous mineral carbonation chemical systems. Given the complexity of such systems, geochemical equilibrium modelling is found to be an invaluable companion tool for planning and interpretation of experimental results. However, in contrast with the performance of geochemical simulation tools available today, such as the CHESS package used in this work, the lack of thermodynamic data necessary to simulate the behaviour of relevant chemical systems is a real issue that must be addresse

Transport of Pb and Zn by carboxylate complexes in basinal ore fluids and related petroleum-field brines at 100°C: the influence of pH and oxygen fugacity

It is well established through field observations, experiments, and chemical models that oxidation (redox) state and pH exert a strong influence on the speciation of dissolved components and the solubility of minerals in hydrothermal fluids. log [Image: see text] –pH diagrams were used to depict the influence of oxygen fugacity and pH on monocarboxylate- and dicarboxylate-transport of Pb and Zn in low-temperature (100°C) hydrothermal ore fluids that are related to diagenetic processes in deep sedimentary basins, and allow a first-order comparison of Pb and Zn transport among proposed model fluids for Mississippi Valley-type (MVT) and red-bed related base metal (RBRBM) deposits in terms of their approximate pH and [Image: see text] conditions. To construct these diagrams, total Pb and Zn concentrations and Pb and Zn speciation were calculated as a function of log [Image: see text] and pH for a composite ore-brine with concentrations of major elements, total sulfur, and total carbonate that approximate the composition of MVT and RBRBM model ore fluids and modern basinal brines. In addition to acetate and malonate complexation, complexes involving the ligands Cl(-), HS(-), H(2)S, and OH(- )were included in the model of calculated total metal concentration and metal speciation. Also, in the model, Zn and Pb are competing with the common-rock forming metals Ca, Mg, Na, Fe, and Al for the same ligands. Calculated total Pb concentration and calculated total Zn concentration are constrained by galena and sphalerite solubility, respectively. Isopleths, in log [Image: see text] –pH space, of the concentration of Pb and concentration of Zn in carboxylate (acetate + malonate) complexes illustrate that the oxidized model fluids of T. H. Giordano (in Organic Acids in Geological Processes, ed. E. D. Pittman and M. D. Lewan, Springer-Verlag, New York, 1994, pp. 319–354) and G. M. Anderson (Econ. Geol., 1975, 70, 937–942) are capable of transporting sufficient amounts of Pb (up to 10 ppm) and Zn (up to 100 ppm) in the form of carboxylate complexes to form economic deposits of these metals. On the other hand, the reduced ore fluid models of D. A. Sverjensky (Econ. Geol., 1984, 79, 23–37) and T. H. Giordano and H. L. Barnes (Econ. Geol., 1981, 76, 2200–2211) can at best transport amounts of Pb and Zn, as carboxylate complexes, that are many orders of magnitude below the 1 to 10 ppm minimum required to form economic deposits. Lead and zinc speciation (mol% of total Pb or Zn) in the model ore fluid was calculated at specific log [Image: see text] –pH conditions along the 100, 0.01, and 0.001 ppm total Pb and total Zn isopleths. Along the 100 ppm isopleth conditions are oxidized (∑SO(4 )>> ∑H(2)S) with Pb and Zn predominantly in the form of chloride complexes under acid to mildly alkaline conditions (pH from 3 to approximately 7.5), while hydroxide complexes dominate Pb and Zn speciation under more alkaline conditions. Sulfide complexes are insignificant under these oxidized conditions. For more reduced conditions along the 0.01 and 0.001 ppm isopleths chloride complexes dominate Pb and Zn speciation in the SO(4)(2- )field and near the SO(4)(2-)-reduced sulfur boundary from pH = 4 to approximately 7.5, while hydroxide complexes dominate Pb and Zn speciation under alkaline conditions above pH = 7.5 in the SO(4)(2- )field. In the most reduced fluids (∑H(2)S >> ∑SO(4)) along the 0.01 and 0.001 isopleths, sulfide complexes account for almost 100% of the Pb and Zn in the model fluid. Acetate (monocarboxylate) complexation is significant only under conditions of chloride and hydroxide complex dominance and its effect is maximized in the pH range 5 to 7, where it complexes 2 to 2.6% of the total Pb and 1 to 1.25% of the total Zn. Malonate (dicarboxylate) complexes are insignificant along all isopleths. The speciation results from this study show that deep formation waters characterized by temperatures near 100°C, high oxidation states and ∑H(2)S < 0.03 mg L(-1 )([Image: see text] < 10(-6)), high chlorinities (~ 100000 mg L(-1)), and high but reasonable concentrations of carboxylate anions can mobilize up to 3% of the total Pb and up to 1.3% of the total Zn as carboxylate complexes. Furthermore, these percentages, under the most favorable conditions, correspond to approximately 1 to 100 ppm of these metals in solution; concentrations that are adequate to form economic deposits of these metals. However, the field evidence suggests that all of these optimum conditions for carboxylate complexation are rarely met at the same time. A comparison of the composite ore fluid compositions from this study and modern brine data shows that the ore brines, corresponding to log [Image: see text] –pH conditions based on the Anderson (1975) and Giordano (1994) model fluids, are similar in many respects to modern, high trace-metal petroleum-field brines. The principal differences between modern high trace-metal brines and the composite ore fluids of Anderson (1975) and Giordano (1994) relate to their carboxylate anion content. The reported concentrations of monocarboxylate anions (∑monocbx) and dicarboxylate anions (Edicbx) in high trace-metal petroleum-field brines (< 1 to 300 mg L(-1 )and < 1 mg L(-1), respectively) are significantly lower than the concentrations assumed in the modelled brines of this study (∑monocbx = 7 700 mg L(-1 )and ∑dicbx = 300 mg L(-1)). There are also major differences in the corresponding total chloride to carboxylate ratio (∑m(Cl)/∑m(cbx)) and monocarboxylate to dicarboxylate ratio (∑m(monocbx)/∑m(dicbx)). Modern high trace-metal brines have much higher ∑m(Cl)/∑m(cbx )values and, therefore, the contribution of carboxylate complexes to the total Pb and Zn content in these modern brines is likely to be significantly less than the 1 to 3 percent for the composite ore fluids of Anderson (1975) and Giordano (1994). The composite ore-brine based on the Giordano and Barnes (1981) MVT ore fluid is comparable to the high salinity (> 170 000 mg L(-1 )TDS) subset of modern brines characterized by low trace-metal content and high total reduced sulfur (∑H(2)S). A comparison of the Sverjensky (1984) composite ore-brine with modern petroleum-field brines in terms of ∑H(2)S and Zn content, reveals that this ore fluid corresponds to a "border-type" brine, between modern high trace-metal brines and those with low trace-metal content and high ∑H(2)S. A brine of this type is characterized by values of ∑H(2)S, ∑Zn, and/or ∑Pb within or near the 1 to 10 mg L(-1 )range. Based on brine-composition data from numerous references cited in this paper, border-type brines do exist but are rare. The model results and field evidence presented in this study are consistent with other chemical simulation studies of carboxylate complexation in modern petroleum-field brines. Thus, it appears that carboxylate complexation plays a minor, if not insignificant, role as a transport mechanism for Pb and Zn in high salinity Na–Cl and Na–Ca–Cl basinal brines and related ore fluids

Transcriptional regulation of CYP6B1v3, a furanocoumarin-inducible P450 gene from black swallowtail (Papilio polyxenes)

Black swallowtail (Papilio polyxenes) is an oligophagous insect feeding exclusively on plant species which contain toxic furanocoumarins. P. polyxenes owes its tolerance to furanocoumarins to at least one cytochrome P450 isozyme, CYP6B1, which is capable of metabolizing linear furanocoumarins at high efficiency. CYP6B1 is autoregulated as it is transcriptionally induced by xanthotoxin, which the protein is capable of metabolizing.In order to understand transcriptional regulation of this furanocoumarin-inducible system, a CYP6B1v3 gene encoding this P450 was isolated from a P. polyxenes genomic library. The open reading frame of this gene, interrupted by a single intron, is virtually identical to the previously characterized CYP6B1v1 and CYP6B1v2 cDNAs. Northern and RNase protection analyses have demonstrated that CYP6B1v1-3 transcripts are induced in P. polyxenes midguts in response to xanthotoxin and bergapten, two linear furanocoumarins, and to a lesser extent by angelicin, an angular furanocoumarin. To identify regulatory elements in the CYP6B1v3 promoter responsible for xanthotoxin inducibility, chimeric constructs containing the CYP6B1v3 5\sp\prime flanking region linked to CAT reporter sequences were transiently transfected into lepidopteran Sf9 cell cultures. CAT activity analysis indicates that the CYP6B1v3 promoter and the xanthotoxin response cascade are functional in this heterologous system. Transfection of deletion and mutant derivatives of the CYP6B1v3 promoter has identified a positive xanthotoxin-responsive element (XRE) located from $-$136 to $-$119, relative to the transcription start site. This 18-bp region containing a canonical CAAT sequence and T-rich sequences is required for both basal expression and xanthotoxin inducibility of the CYP6B1v3 promoter. Gel shift assays conducted with the XRE-containing probe and Sf9 nuclear extracts have identified a heat-labile protein(s) which binds specifically to this region of the promoter. I have demonstrated that this factor is constitutively present in both control and xanthotoxin-treated Sf9 nuclear and P. polyxenes cell extracts and have termed it constitutive XRE-binding factor (CXF). Phosphorylation of CXF has shown to be partially responsible for its DNA-binding activity. In toto, these data suggest that binding of a constitutively expressed protein(s) is required for both basal and inducible transcription from this promoter and that additional transcription factors are required for transcriptional activation (or derepression) by xanthotoxin.U of I OnlyETDs are only available to UIUC Users without author permissio

Transcriptional regulation of the Papilio polyxenes CYP6B1 gene.

Detoxification of host plant defensive compounds by larval Lepidoptera is mediated by cytochrome P450 monooxygenases (P450s) such as CYP6B1, which is expressed in Papilio polyxenes (black swallowtail) larvae in response to xanthotoxin, a linear furanocoumarin. Baculovirus-mediated expression of two cloned CYP6B1 cDNAs in lepidopteran cell lines has demonstrated that CYP6B1 isozymes primarily metabolize the linear furanocoumarins, xanthotoxin and bergapten, and not angular furanocoumarins. To characterize the regulatory features of the CYP6B1 transcription unit, we have isolated the first full-length CYP6B1v3 genomic DNA clone from P. polyxenes. The open reading frame of this gene is interrupted by a single intron and is virtually identical to the previously characterized CYP6B1 cDNAs. Primer extension and ribonuclease protection analyses have localized the transcription initiation site to a point 28 nucleotides upstream from the AUG initiation codon. RNase protection analyses on RNA from larvae induced by linear and angular furanocoumarins indicate that transcription of the CYP6B1 gene is induced in insects significantly in response to xanthotoxin and only slightly in response to bergapten. Angular furanocoumarins, such as angelicin, which are not appreciably metabolized by the CYP6B1 gene product, do not significantly induce transcription of this gene. We conclude that this P450 gene is transcriptionally regulated in vivo by at least one of the substrates which the encoded protein metabolizes. Transient expression of CAT fusion constructs in transfected Sf9 lepidopteran cells demonstrates that nucleotides -1 to -838 upstream from the CYP6B1v3 transcription initiation site retain basal and xanthotoxin-inducible transcriptional activities in this heterologous cell line. These data clearly indicate that P. polyxenes has adapted to the presence of furanocoumarins in its host plants by evolving P450 isozymes and regulatory cascades which respond to specific toxins

Data from: Phylogenetic analysis reveals positive correlations between adaptations to diverse hosts in a group of pathogen-like herbivores

A jack of all trades can be master of none – this intuitive idea underlies most theoretical models of host-use evolution in plant-feeding insects, yet empirical support for trade-offs in performance on distinct host plants is weak. Trade-offs may influence the long-term evolution of host use while being difficult to detect in extant populations, but host-use evolution may also be driven by adaptations for generalism. Here we used host-use data from insect collection records to parameterize a phylogenetic model of host-use evolution in armored scale insects, a large family of plant-feeding insects with a simple, pathogen-like life history. We found that a model incorporating positive correlations between evolutionary changes in host performance best fit the observed patterns of diaspidid presence and absence on nearly all focal host taxa, suggesting that adaptations to particular hosts also enhance performance on other hosts. In contrast to the widely invoked trade-off model, we advocate a “toolbox” model of host-use evolution in which armored scale insects accumulate a set of independent genetic tools, each of which is under selection for a single function but may be useful on multiple hosts