Sepiolite is a clay mineral, a complex magnesium silicate, a typical formula for which is (OH2)4(OH)4Mg8Si12O30•8H2O. It is formed by blocks and cavities (tunnels) growing in the direction of the fibres. The tunnels, 3.7 x 10.6 Å in cross-section, are responsible for the high specific surface area and sorptive properties of sepiolite. The co-intercalation of 3-methyl cyclohex-2-en-1-one (MCH), the Douglas-Fir beetle anti-aggregation pheromone, with methanol, ethanol, acetone, or benzene into sepiolite tunnels was studied. The resulting nanohybrid materials were characterized by means of various techniques, such as multinuclear solid-state NMR spectroscopy, porosity studies and Thermal Gravimetric Analysis (TGA). This was done in the hope of obtaining slow and controlled release of MCH from the sepiolite tunnels. It was demonstrated by 13C MAS NMR (carbon-13 magic angle spinning nuclear magnetic resonance) that at room temperature there are two different MCH molecules: one MCH inside the tunnels and the other one outside the tunnels of the sepiolite. Heating nanohybrid materials at 60˚C for 20 hours removes the external MCH molecules from the sepiolite. 13C MAS NMR showed that by further heating nanohybrid materials at 120˚C for 20 hours, methanol, ethanol, or acetone peaks were greatly reduced; however, the benzene peak was not reduced. To better understand how benzene acts inside sepiolite, intercalation of d6-benzene, and co-intercalations of d6-benzene with MCH and d6-benzene with pyridine into sepiolite tunnels were carried out, and these samples were studied by the same techniques. Another technique was used in order to see whether the slow and controlled release of MCH from the sepiolite tunnels could be obtained: sepiolite-MCH nanohybrids were treated with 20 ml of 0.5 M HCl solution. It was found that when 1 gram of MCH-sepiolite sample was acid treated at room temperature, about 35% of intercalated MCH was removed from the sepiolite. The role of sepiolite clay was also studied in Maya-Blue representative structure sepiolite-indigo adduct. It is known that upon heating the sepiolite and indigo mixture, the stability that is present in Maya-Blue is achieved. It is still a mystery, however, how exactly indigo and sepiolite interact with each other.

Sepiolite is a clay mineral, a complex magnesium silicate, a typical formula for which is (OH2)4(OH)4Mg8Si12O30•8H2O. It is formed by blocks and cavities (tunnels) growing in the direction of the fibres. The tunnels, 3.7 x 10.6 Å in cross-section, are responsible for the high specific surface area and sorptive properties of sepiolite. The co-intercalation of 3-methyl cyclohex-2-en-1-one (MCH), the Douglas-Fir beetle anti-aggregation pheromone, with methanol, ethanol, acetone, or benzene into sepiolite tunnels was studied. The resulting nanohybrid materials were characterized by means of various techniques, such as multinuclear solid-state NMR spectroscopy, porosity studies and Thermal Gravimetric Analysis (TGA). This was done in the hope of obtaining slow and controlled release of MCH from the sepiolite tunnels. It was demonstrated by 13C MAS NMR (carbon-13 magic angle spinning nuclear magnetic resonance) that at room temperature there are two different MCH molecules: one MCH inside the tunnels and the other one outside the tunnels of the sepiolite. Heating nanohybrid materials at 60˚C for 20 hours removes the external MCH molecules from the sepiolite. 13C MAS NMR showed that by further heating nanohybrid materials at 120˚C for 20 hours, methanol, ethanol, or acetone peaks were greatly reduced; however, the benzene peak was not reduced. To better understand how benzene acts inside sepiolite, intercalation of d6-benzene, and co-intercalations of d6-benzene with MCH and d6-benzene with pyridine into sepiolite tunnels were carried out, and these samples were studied by the same techniques. Another technique was used in order to see whether the slow and controlled release of MCH from the sepiolite tunnels could be obtained: sepiolite-MCH nanohybrids were treated with 20 ml of 0.5 M HCl solution. It was found that when 1 gram of MCH-sepiolite sample was acid treated at room temperature, about 35% of intercalated MCH was removed from the sepiolite. The role of sepiolite clay was also studied in Maya-Blue representative structure sepiolite-indigo adduct. It is known that upon heating the sepiolite and indigo mixture, the stability that is present in Maya-Blue is achieved. It is still a mystery, however, how exactly indigo and sepiolite interact with each other.

Sepiolite is a clay mineral, a complex magnesium silicate, a typical formula for which is (OH2)4(OH)4Mg8Si12O30•8H2O. It is formed by blocks and cavities (tunnels) growing in the direction of the fibres. The tunnels, 3.7 x 10.6 Å in cross-section, are responsible for the high specific surface area and sorptive properties of sepiolite. The co-intercalation of 3-methyl cyclohex-2-en-1-one (MCH), the Douglas-Fir beetle anti-aggregation pheromone, with methanol, ethanol, acetone, or benzene into sepiolite tunnels was studied. The resulting nanohybrid materials were characterized by means of various techniques, such as multinuclear solid-state NMR spectroscopy, porosity studies and Thermal Gravimetric Analysis (TGA). This was done in the hope of obtaining slow and controlled release of MCH from the sepiolite tunnels. It was demonstrated by 13C MAS NMR (carbon-13 magic angle spinning nuclear magnetic resonance) that at room temperature there are two different MCH molecules: one MCH inside the tunnels and the other one outside the tunnels of the sepiolite. Heating nanohybrid materials at 60˚C for 20 hours removes the external MCH molecules from the sepiolite. 13C MAS NMR showed that by further heating nanohybrid materials at 120˚C for 20 hours, methanol, ethanol, or acetone peaks were greatly reduced; however, the benzene peak was not reduced. To better understand how benzene acts inside sepiolite, intercalation of d6-benzene, and co-intercalations of d6-benzene with MCH and d6-benzene with pyridine into sepiolite tunnels were carried out, and these samples were studied by the same techniques. Another technique was used in order to see whether the slow and controlled release of MCH from the sepiolite tunnels could be obtained: sepiolite-MCH nanohybrids were treated with 20 ml of 0.5 M HCl solution. It was found that when 1 gram of MCH-sepiolite sample was acid treated at room temperature, about 35% of intercalated MCH was removed from the sepiolite. The role of sepiolite clay was also studied in Maya-Blue representative structure sepiolite-indigo adduct. It is known that upon heating the sepiolite and indigo mixture, the stability that is present in Maya-Blue is achieved. It is still a mystery, however, how exactly indigo and sepiolite interact with each other.

Sepiolite is a clay mineral, a complex magnesium silicate, a typical formula for which is (OH2)4(OH)4Mg8Si12O30•8H2O. It is formed by blocks and cavities (tunnels) growing in the direction of the fibres. The tunnels, 3.7 x 10.6 Å in cross-section, are responsible for the high specific surface area and sorptive properties of sepiolite. The co-intercalation of 3-methyl cyclohex-2-en-1-one (MCH), the Douglas-Fir beetle anti-aggregation pheromone, with methanol, ethanol, acetone, or benzene into sepiolite tunnels was studied. The resulting nanohybrid materials were characterized by means of various techniques, such as multinuclear solid-state NMR spectroscopy, porosity studies and Thermal Gravimetric Analysis (TGA). This was done in the hope of obtaining slow and controlled release of MCH from the sepiolite tunnels. It was demonstrated by 13C MAS NMR (carbon-13 magic angle spinning nuclear magnetic resonance) that at room temperature there are two different MCH molecules: one MCH inside the tunnels and the other one outside the tunnels of the sepiolite. Heating nanohybrid materials at 60˚C for 20 hours removes the external MCH molecules from the sepiolite. 13C MAS NMR showed that by further heating nanohybrid materials at 120˚C for 20 hours, methanol, ethanol, or acetone peaks were greatly reduced; however, the benzene peak was not reduced. To better understand how benzene acts inside sepiolite, intercalation of d6-benzene, and co-intercalations of d6-benzene with MCH and d6-benzene with pyridine into sepiolite tunnels were carried out, and these samples were studied by the same techniques. Another technique was used in order to see whether the slow and controlled release of MCH from the sepiolite tunnels could be obtained: sepiolite-MCH nanohybrids were treated with 20 ml of 0.5 M HCl solution. It was found that when 1 gram of MCH-sepiolite sample was acid treated at room temperature, about 35% of intercalated MCH was removed from the sepiolite. The role of sepiolite clay was also studied in Maya-Blue representative structure sepiolite-indigo adduct. It is known that upon heating the sepiolite and indigo mixture, the stability that is present in Maya-Blue is achieved. It is still a mystery, however, how exactly indigo and sepiolite interact with each other.

Neste trabalho foi investigado o efeito exercido por microambientes sobre a estabilidade química e fotoquímica de corantes. Em particular, estudaram-se os fatores responsáveis pelo aumento da estabilidade química e fotoquímica de índigo quando em interação com paligorsquita, que compõem o pigmento histórico Azul Maia, sobre o qual ainda havia controvérsias na literatura. Os corantes investigados foram índigo, dehidroíndigo, alizarina, purpurina, luteolina e β-caroteno; os microambientes foram proporcionados pelas argilas paligorsquita, sepiolita, montmorilonita, laponita e HDL de Al3+ e Mg2+ (3:1). Paligorsquita e a sepiolita são as únicas argilas que apresentam microporos em sua estrutura. As técnicas de caracterização empregadas neste trabalho foram: espectroscopia vibracional (Raman e absorção no infravermelho), espectroscopia de absorção no UV-VIS, difratometria de raios X, análise térmica (TG e DSC), CG-MS, HLPC-MS, medidas de área superficial por isoterma de adsorção de N2 e SEM. Duas técnicas com resolução temporal em escala de sub-picosegundos (absorção de transiente e infravermelho resolvido no tempo) foram utilizadas. O sistema índigo+paligorsquita corresponde à mistura dos dois sólidos, seguida de aquecimento, sendo que a partir de 70 °C a coloração da mistura adquire tonalidade esverdeada e também apresenta maior estabilidade química e fotoquímica. Essa estabilidade e também a alteração na cor aumentam com a temperatura de aquecimento da mistura e o intervalo considerado engloba as temperaturas de perda de água zeolítica (70 - 150 °C) e coordenada (170 - 280 °C) da estrutura da argila. Os resultados de espectroscopia vibracional e eletrônica dos simulantes de Azul Maia indicam que o índigo interage através de ligações de hidrogênio com as moléculas de água coordenada. Essa interação, entretanto, só é possível com a remoção da água zeolítica, o que ocorre a partir de 70 °C. Com aquecimento em temperaturas acima de 170 °C o comportamento do espectro eletrônico e vibracional se altera, indicando a formação direta de complexos com os metais presentes nas bordas internas dos microporos. Os resultados de espectroscopia Raman indicam que com a interação por ligação de hidrogênio a simetria molecular do índigo diminua. Os estudos por espectroscopia com resolução temporal mostraram que o índigo apresenta transferência de próton no estado excitado (ESIPT) de um dos amino grupos para a carbonila adjacente; após esta transferência, há a formação da espécie mono-enol a qual relaxa ao estado fundamental após 120 ps, através de intersecção cônica, o que explica a alta fotoestabilidade do corante. No caso da mistura aquecida a 130 °C os resultados, obtidos pela primeira vez para uma molécula imobilizada em argila, confirmam que o índigo encontra-se em um ambiente hidrofílico, considerando o tempo de vida de decaimento do estado excitado (3,0 ps), comparável ao do índigo carmim em solução aquosa (2,7 ps). O tempo de vida também é muito curto, comparado ao em solução de DMSO (120 ps) o que pode explicar a alta estabilidade do corante quando dentro do microcanal da argila. Finalmente, constatou-se que o dehidroíndigo não é responsável pela coloração de simulantes de Azul Maia, a qual resulta de alterações no espectro de absorção no visível do corante que ocorrem com a interação com a argila / In this work, the role played by the microenvironment on the chemical and photochemical stability of dyes was investigated. The factors responsible for the enhanced stability of indigo when interacting with palygorskite were detailed studied; the indigo and palygorskite system constitutes a simulant of Maya Blue, a historical pigment with properties which are controversially described in the literature. The dyes here investigated were indigo, dehydroindigo, alizarin, purpurin, luteolin and β-carotene; the microenvironment was provided by palygorskite, sepiolite, montmorillonite, laponite and a layered double hydroxide (Al3+ e Mg2+, 3:1). Palygorskite and sepiolite are the only clays with micropores in their structure. Several characterization techniques were employed, namely vibrational spectroscopy (Raman and infrared), UV-VIS electronic absorption spectroscopy, X-ray diffractometry, thermal analysis (TG and DSC), CG-MS, HPLC-MS, surface area and porosity determination (N2 isotherm adsorption) and scanning electron microscopy. Two sub-picosecond time resolved techniques (transient absorption and infrared absorption) were also used. The indigo+palygorskite system corresponds to the intimate mixture of both solids, followed by heating; from 70 °C the mixture attains a greenish hue and an enhanced chemical and photochemical stability. Both stability and color change increase with the heating temperature, which also leads to loss of zeolitic and coordinated water (70 to 150 °C and 170 to 280 °C, respectively). Vibrational and electronic spectroscopies indicate that, in the Maya Blue simulants, the dye interacts with the clay through hydrogen bonds with the coordinated water molecules. Such interaction, however, is only possible with the removal of the zeolitic water, which starts at 70 °C. At temperatures above 170 °C, both vibrational and electronic spectral profiles change, indicating that the interaction is now proceeding directly with the metals that are at the internal borders of the micropores. Results from Raman spectroscopy suggest that with the hydrogen bond and metal interaction a symmetry lowering occurs. Time resolved spectroscopy results show that indigo present an excited state intramolecular proton transfer from one of the NH to the adjacent carbonyl group, originating a mono-enol species, which decays to the ground state after 120 ps through a conical intersection. Such fast decay explains the high photochemical stability of indigo. In the case of the ind+paly mixture heated at 130 °C, the time resolved data obtained for the first time for a dye+clay system confirms that indigo is in a hydrophilic environment, taking into account the excited state lifetime (3.0 ps), comparable to indigo carmine in aqueous solution (2.7 ps). The excited state lifetime of indigo in the clay is also very short when compared to the experimental data for the dye in DMSO solution (120 ps), which is possibly an explanation for the dye high stability when inside the clay micropores. Finally, dehydroindigo was not found to be responsible for the color of Maya Blue simulants, which results from the spectral changes in the dye absorption spectrum originated by the interaction with the clay.

Neste trabalho foi investigado o efeito exercido por microambientes sobre a estabilidade química e fotoquímica de corantes. Em particular, estudaram-se os fatores responsáveis pelo aumento da estabilidade química e fotoquímica de índigo quando em interação com paligorsquita, que compõem o pigmento histórico Azul Maia, sobre o qual ainda havia controvérsias na literatura. Os corantes investigados foram índigo, dehidroíndigo, alizarina, purpurina, luteolina e β-caroteno; os microambientes foram proporcionados pelas argilas paligorsquita, sepiolita, montmorilonita, laponita e HDL de Al3+ e Mg2+ (3:1). Paligorsquita e a sepiolita são as únicas argilas que apresentam microporos em sua estrutura. As técnicas de caracterização empregadas neste trabalho foram: espectroscopia vibracional (Raman e absorção no infravermelho), espectroscopia de absorção no UV-VIS, difratometria de raios X, análise térmica (TG e DSC), CG-MS, HLPC-MS, medidas de área superficial por isoterma de adsorção de N2 e SEM. Duas técnicas com resolução temporal em escala de sub-picosegundos (absorção de transiente e infravermelho resolvido no tempo) foram utilizadas. O sistema índigo+paligorsquita corresponde à mistura dos dois sólidos, seguida de aquecimento, sendo que a partir de 70 °C a coloração da mistura adquire tonalidade esverdeada e também apresenta maior estabilidade química e fotoquímica. Essa estabilidade e também a alteração na cor aumentam com a temperatura de aquecimento da mistura e o intervalo considerado engloba as temperaturas de perda de água zeolítica (70 - 150 °C) e coordenada (170 - 280 °C) da estrutura da argila. Os resultados de espectroscopia vibracional e eletrônica dos simulantes de Azul Maia indicam que o índigo interage através de ligações de hidrogênio com as moléculas de água coordenada. Essa interação, entretanto, só é possível com a remoção da água zeolítica, o que ocorre a partir de 70 °C. Com aquecimento em temperaturas acima de 170 °C o comportamento do espectro eletrônico e vibracional se altera, indicando a formação direta de complexos com os metais presentes nas bordas internas dos microporos. Os resultados de espectroscopia Raman indicam que com a interação por ligação de hidrogênio a simetria molecular do índigo diminua. Os estudos por espectroscopia com resolução temporal mostraram que o índigo apresenta transferência de próton no estado excitado (ESIPT) de um dos amino grupos para a carbonila adjacente; após esta transferência, há a formação da espécie mono-enol a qual relaxa ao estado fundamental após 120 ps, através de intersecção cônica, o que explica a alta fotoestabilidade do corante. No caso da mistura aquecida a 130 °C os resultados, obtidos pela primeira vez para uma molécula imobilizada em argila, confirmam que o índigo encontra-se em um ambiente hidrofílico, considerando o tempo de vida de decaimento do estado excitado (3,0 ps), comparável ao do índigo carmim em solução aquosa (2,7 ps). O tempo de vida também é muito curto, comparado ao em solução de DMSO (120 ps) o que pode explicar a alta estabilidade do corante quando dentro do microcanal da argila. Finalmente, constatou-se que o dehidroíndigo não é responsável pela coloração de simulantes de Azul Maia, a qual resulta de alterações no espectro de absorção no visível do corante que ocorrem com a interação com a argila / In this work, the role played by the microenvironment on the chemical and photochemical stability of dyes was investigated. The factors responsible for the enhanced stability of indigo when interacting with palygorskite were detailed studied; the indigo and palygorskite system constitutes a simulant of Maya Blue, a historical pigment with properties which are controversially described in the literature. The dyes here investigated were indigo, dehydroindigo, alizarin, purpurin, luteolin and β-carotene; the microenvironment was provided by palygorskite, sepiolite, montmorillonite, laponite and a layered double hydroxide (Al3+ e Mg2+, 3:1). Palygorskite and sepiolite are the only clays with micropores in their structure. Several characterization techniques were employed, namely vibrational spectroscopy (Raman and infrared), UV-VIS electronic absorption spectroscopy, X-ray diffractometry, thermal analysis (TG and DSC), CG-MS, HPLC-MS, surface area and porosity determination (N2 isotherm adsorption) and scanning electron microscopy. Two sub-picosecond time resolved techniques (transient absorption and infrared absorption) were also used. The indigo+palygorskite system corresponds to the intimate mixture of both solids, followed by heating; from 70 °C the mixture attains a greenish hue and an enhanced chemical and photochemical stability. Both stability and color change increase with the heating temperature, which also leads to loss of zeolitic and coordinated water (70 to 150 °C and 170 to 280 °C, respectively). Vibrational and electronic spectroscopies indicate that, in the Maya Blue simulants, the dye interacts with the clay through hydrogen bonds with the coordinated water molecules. Such interaction, however, is only possible with the removal of the zeolitic water, which starts at 70 °C. At temperatures above 170 °C, both vibrational and electronic spectral profiles change, indicating that the interaction is now proceeding directly with the metals that are at the internal borders of the micropores. Results from Raman spectroscopy suggest that with the hydrogen bond and metal interaction a symmetry lowering occurs. Time resolved spectroscopy results show that indigo present an excited state intramolecular proton transfer from one of the NH to the adjacent carbonyl group, originating a mono-enol species, which decays to the ground state after 120 ps through a conical intersection. Such fast decay explains the high photochemical stability of indigo. In the case of the ind+paly mixture heated at 130 °C, the time resolved data obtained for the first time for a dye+clay system confirms that indigo is in a hydrophilic environment, taking into account the excited state lifetime (3.0 ps), comparable to indigo carmine in aqueous solution (2.7 ps). The excited state lifetime of indigo in the clay is also very short when compared to the experimental data for the dye in DMSO solution (120 ps), which is possibly an explanation for the dye high stability when inside the clay micropores. Finally, dehydroindigo was not found to be responsible for the color of Maya Blue simulants, which results from the spectral changes in the dye absorption spectrum originated by the interaction with the clay.

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