Efficient syntheses of climate relevant isoprene nitrates and (1R,5S)-(−)-myrtenol nitrate

Here we report the chemoselective synthesis of several important, climate relevant isoprene nitrates using silver nitrate to mediate a ’halide for nitrate’ substitution. Employing readily available starting materials, reagents and Horner–Wadsworth–Emmons chemistry the synthesis of easily separable, synthetically versatile ‘key building blocks’ (E)- and (Z)-3-methyl-4-chlorobut-2-en-1-ol as well as (E)- and (Z)-1-((2-methyl-4-bromobut-2-enyloxy)methyl)-4-methoxybenzene has been achieved using cheap, ’off the shelf’ materials. Exploiting their reactivity we have studied their ability to undergo an ‘allylic halide for allylic nitrate’ substitution reaction which we demonstrate generates (E)- and (Z)-3-methyl-4-hydroxybut-2-enyl nitrate, and (E)- and (Z)-2-methyl-4-hydroxybut-2-enyl nitrates (‘isoprene nitrates’) in 66–80% overall yields. Using NOESY experiments the elucidation of the carbon–carbon double bond configuration within the purified isoprene nitrates has been established. Further exemplifying our ‘halide for nitrate’ substitution chemistry we outline the straightforward transformation of (1R,2S)-(−)-myrtenol bromide into the previously unknown monoterpene nitrate (1R,2S)-(−)-myrtenol nitrate.


Introduction
Understanding the chemistry of the biosphere and its interaction with the atmosphere is fundamental to Earth System science. Such is the importance of this topic a whole issue of Chemical Reviews was dedicated to the 'Role of Chemistry in the Earth's Climate' [1].
The quantities of BVOCs released far exceed non-methane hydrocarbon emissions derived from anthropogenic activity (~90 Tg C yr −1 where 1 Tg = 1 × 10 6 tons) [4]. Indeed, although early estimates of isoprene emissions were as high as 1200 Tg C yr −1 [5] these have, in recent years, been revised down to 600 Tg C yr −1 [6]. Be this as it may, a comprehensive understanding of the atmospheric chemistry and kinetics associated with isoprene and its derivatives is largely based on chemical theory and modeling with very little verified measurements. Therefore, the impact of isoprene on air quality and climate change remains highly uncertain.
Isoprene or 2-methylbuta-1,3-diene is a volatile C 5 -organic compound generated by plants to help protect them against 'attack' from bacteria, fungi and parasites. Isoprene also helps to protect against abiotic 'stress' induced by excessive fluctuations in temperature, by drought, exposure to radiation as well as by contact with herbicides and insecticides [7]. Isoprene reacts readily with O 3 , HO • and • NO 3 with the resulting intermediates subsequently reacting with NO X , i.e., nitric oxide and nitrogen dioxide in a process that generates mixtures of isoprene nitrates (IPNs), O 3 and secondary organic aerosols (SOA) [8]. Thus, the formation of IPN mixtures plays a key role in O 3 synthesis and it is this aspect of their chemistry that determines how much NO X is lost or recycled [9].
Taking all of this into account it is clear that isoprene and isoprene nitrates are important. However, what is still not fully understood is the role of individual IPNs (Scheme 1) on atmospheric chemistry [1][2][3]. Evidently, to comprehensively investigate the role of individual IPNs within climate chemistry it is important that any synthetic protocol employed to generate IPNs affords either individual C=C stereoisomers or generates readily separable stereoisomers of the IPNs. Thus although the lack of synthetic standards has hindered a comprehensive understanding of IPN climate chemistry, there has been progress in a number of laboratory, field and theoretical studies that have focused on probing their formation, kinetics, yields and decomposition. By way of example, Teng et al. investigated the branching ratio (α) when C 2 -C 8 alkenes (including isoprene) react with HO • in the presence of oxygen. In this process the generated β-hydroxyperoxy radicals subsequently react with NO affording β-hydroxy nitrates. The results from the Teng laboratory established that increasing the substitution pattern on the alkene affords a higher α or branching ratio. A further interesting observation was identified when deuterated alkenes were employed, in these examples α increased by a factor of ~1.5 [10].
Within the atmosphere a wide range of struturally diverse IPNs have been identified. However, the formation of IPN mixtures has led to uncertainty in quantifying the true effect of isoprene on the NO x cycle and subsequent O 3 enhancement. Shepson et al. sought to deconvolute this process replicating the atmospheric synthesis of IPN using a photochemical reaction chamber to determine IPN yield from isoprene photooxidation and high NO concentration. They compared their results with field observations, collected during the Southern oxidant and Aerosol Study (SOAS) campaign conducted in 2013, and model simulations. These studies identified NO as the limiting factor in IPN production [11].
Schwantes et al. reported a comprehensive study that focused on the oxidation of isoprene with a nitrate radical. Using a variety of detection methods, e.g., CIMS and GC-FID they identified the nitrate radical preferentially reacted at the C1 position of isoprene. The resulting intermediate subsequently reacted with oxygen affording a suite of nitroxyalkylperoxy radicals. Worthy of note and a fundamental reason for initiating the UEA study was the fact that Schwantes et al. make reference to the fact that "synthetic standards are not available, the CIMS sensitivities for most of the isoprene nitrates formed in this work are not known" [12].
Organic nitrates are important in locations where biogenic hydrocarbon emissions mix with anthropogenic NOx sources. It is generally accepted that transport models should include representation of organic aerosols derived from the reaction of monoterpenes with nitrate radicals. With this in mind Pye et al. recently developed a system to study the formation and subsequent aerosol-phase partitioning of organic nitrates derived from both isoprene and monoterpenes. Their studies indicated the concentrations of organic aerosol and gas-phase organic nitrates increased when particulate organic nitrates underwent rapid pseudohydrolysis; a process that generates corrosive nitric acid and non-volatile SOA [13].
Similar to the isoprene studies by Pye et al. the role of organic nitrates derived from terpenes is starting to gain traction. Rindelaub et al. undertook a photochemical reaction chamber study that focused on the hydroxyl radical oxidation of α-pinene under high NO x conditions. α-Pinene is an important contributor to SOA with annual emissions estimated to be 66 Tg C yr −1 . In their study using nitric oxide (NO) the yield of α-pinene derived organic nitrate was determined to be 26 ± 7%, Scheme 1: Simplified overview outlining how a small number of different IPNs are synthesised and are able to undergo transformations within the atmosphere.
interestingly the concentration of organic nitrates was found to be highly dependent on the relative humidity and seed aerosol acidity. Worthy of note this report also highlighted that "unfortunately, standards are unavailable for the expected organic nitrate products (derived from α-pinene)" this, again, reinforces the need for chemical synthesis studies on the formation of climate relevant organic nitrates [14].
Even though the atmospheric synthesis of structure diverse C 5 -IPNs, i.e., 4-10 is thought to be efficient, i.e., up to 15% yield [15] what is not currently fully understood is the mechanism or kinetics of IPN formation, the percentages of individual IPNs generated or how they are synthesised and the products of their decomposition. Answering these important questions requires the combined expertise of synthetic and atmospheric chemists using the former to generate authentic samples of IPNs which can be 'handed over' to the atmospheric chemists for subsequent testing.
A comprehensive and systematic approach to bespoke IPN synthesis has yet to be undertaken. Here we outline preliminary results towards the development of a series of efficient synthetic routes to IPNs that should allow atmospheric chemists to undertake physicochemical analysis of important climate related IPNs.
A comprehensive survey of the literature revealed three general synthesis routes to IPNs. In summary, Shepson et al. [17] reacted isoprene epoxide with concentrated nitric acid (Scheme 2, path A); Kames [20] into the corresponding nitrato alcohols. Shepson substituted ethylene oxide for commercially available isoprene epoxide and generated eight stereo-and structurally Scheme 2: Protocols for the synthesis of O-nitrated alcohols using (±)-isoprene epoxide and 2° alcohols as starting materials.
isomeric IPNs. Within this mixture 3° nitrate rac-7, 1° nitrate rac-8, (E)-13 and (Z)-14 (path A, Scheme 2) were generated and separated in the following ratios 31.5:2.43:2.14:1. From a purely practical point of view the addition of 'fuming' nitric acid to isoprene epoxide is relatively straightforward. However, several drawbacks to using this protocol are immediately evident. Not least the fact that dispensing strongly oxidizing 'fuming' (i.e., >90%) nitric acid onto reactive isoprene epoxide affords the distinct possibility that a dangerous exothermic 'runaway' reaction could take place (cautionary note: experimental section labelled this reaction "highly exothermic") or indeed an explosion if heated (cautionary note: experimental reports 2-nitratoethanol underwent a "violent explosion, possibly detonation"). Furthermore, although the reaction afforded gram quantities of the IPN mixture the separation and purification of this into rac-7, rac-8, (E)-13 and (Z)-14 was restricted to 100 μL aliquots. Furthermore this did not afford the individual products in high purity. Consequently an additional analytical HPLC purification was required for each 'semi-pure' fraction using a substantially smaller 20 μL column. In summary, this route was time consuming, labour intensive and expensive affording only small quantities of IPNs.
In 1993 Kames et al. [18] described the reaction of dinitrogen pentoxide with seventeen low molecular weight alcohols. They demonstrated that dinitrogen pentoxide reacted readily with, for example, 1-propanol, 1-hexanol, rac-2-pentanol, 1-octanol and that rac-2-butanol afforded rac-2-butyl nitrate (rac-15, path B, Scheme 2) although no yields were provided. Unfortunately this protocol requires the pre-synthesis of dinitrogen pentoxide from nitric oxide and 5% ozone in oxygen. Evidently the handling and reaction of different gases as well as the synthesis of dinitrogen pentoxide necessitates access to or the construction of a specialist gas manifold linked up to a pirani-gauge, capacitancepressure transducers and an ozone generator. Additionally once generated the dinitrogen pentoxide requires purification via sublimation and low temperature recrystallization under a continuous stream of ozone and oxygen. Not only is this a timeconsuming process it also requires considerable experimental expertise. Furthermore, although using dinitrogen pentoxide is suited to the small-scale synthesis of volatile O-nitrate esters, such as rac-15, its application to the synthesis of high-boiling diols is more difficult due to their low-vapour pressures.
The goal of our research program was the development of a 'suite of protocols' that afford specific IPNs using straightforward, reliable chemistry. Worthy of note, we also considered the development of efficient synthesis routes to small organic nitrates to have broader benefits to the general synthesis community. By way of example, currently there are very few protocols that afford multi-functional allylic nitrates. This, it would seem, has hindered their exploitation in the development of new synthetic methodology. Furthermore and in a slightly different context there is significant interest in the pharmaceutical sector in generating structure and function diverse O-nitrate esters for use as in vivo NO-donors. In this context particular emphasis has been placed on developing O-nitrate esters as bio- logically active agents that act on acetylcholinesterase (AChE), amyloid-βx-42 (Aβ42) aggregation, cyclooxygenase-II (COX2), serotonin reuptake and specific GAG inhibitors [21][22][23].

Results and Discussion
Initiating our research we wanted to generate O-nitrate esters based on rac-8, (Z)-9, (E)-10 (Scheme 1), (E)-13, (Z)-14, and rac-16 (Scheme 2). Exploring the potential of isoprene as a starting material we considered it to have several advantages: it is cheap, commercially available, easily handled and has the prerequisite C 5 -skeleton that ensures it is a highly desirable and amenable starting material for its chemical transformation into IPNs. Subjecting isoprene (10 mmol) to a racemic Sharpless dihydroxylation [24] afforded the inseparable (flash chromatography) (±)-3-methylbut-3-ene-1,2-diol (rac-17) and (±)-2methylbut-3-ene-1,2-diol (rac-18) in a 3:2 ratio and unoptimized 67% yield (Scheme 3). Investigating O-nitrate ester formation the rac-17/rac-18 mixture was dissolved in dichloromethane, acetonitrile, or ether at 0 °C or −78 °C. To each was added nitric acid (16 M) and concentrated sulfuric acid (18 M), a biphasic organic/inorganic reaction mixture formed [25]. Unfortunately after work-up all of these reactions afforded complex mixtures. Thus although the 1 H NMR and mass spectrometry indicated the desired mono-O-nitrate rac-19 and rac-20 had formed (Scheme 3) and it seemed that the corresponding di-Onitrate esters (not shown) had also formed; all attempts at flash chromatographic separation and purification met with failure; a fact that hindered our ability to confidently analyse and identify individual components. In summary, the seemingly straightfor-ward combination of nitric and sulfuric acid was unsuited to the efficient synthesis of IPNs. Although generating a mixture of rac-17 and rac-18 was broadly acceptable due to their ease of synthesis, our inability to effectively separate the diols or execute a regioselective 1° or 2°m ono-O-nitration was not. Eliminating the former problem Hodgson et al. [26] reported rac-17 could be generated from cheap, commercially available 2,5-dihydrofuran which, after epoxidation with meta-chloroperbenzoic acid (mCPBA), afforded epoxide 21 in a 65% yield. Subsequent reaction of 21 with methyllithium (2.5 equiv, −78 °C, THF) in an alkylative double ring-opening process afforded, exclusively, (±)-3methylbut-3-ene-1,2-diol (rac-17) in a 54% yield (Scheme 4). The next step required the mild regioselective O-nitration of rac-17. Olah et al. reported that nitronium tetrafluoroborate reacts with 2,4,6-trimethylpyridine in acetonitrile at −10 °C affording N-nitro-2,4,6-trimethylpyridinium tetrafluoroborate (22) [27]. Disappointingly, subjecting rac-17 to O-nitration with in situ generated 22 resulted, as judged by 1 H NMR, in a very poor yield (<10%) of a mixture of O-nitrate esters that, potentially, also included the desired rac-16. Indeed, although we explored alternative reaction times, temperatures, solvents and stoichiometry's of 22 our attempts at generating rac-16 were disappointing. Furthermore, employing short or longer reaction times at −78 °C afforded low yields of complex mixtures that proved, essentially, inseparable by flash chromatography.
Treating 34 and 35, independently, to the Olah O-nitration conditions (MeCN, 0 °C and 1.5 equiv of in situ generated 22) the desired mono-O-nitrated adduct 38 was afforded in a quantitative yield in only two hours. On the contrary C=C bond containing 3-methylbut-3-ene-1-ol (35) reacted with 22 (1.5 equiv) affording ( 1 H NMR) a complex mixture that contained a small amount of 39 (Scheme 5). Similar to 34, butanol (36) afforded a quantitative yield of n-butyl nitrate (40) in two hours. Carbon-carbon double bond containing rac-(E)-pent-3-en-2-ol (37) generated a complex mixture (determined via 1 H NMR) of, again, largely unidentifiable compounds. Albeit our compare and contrast study was limited to only a handful of simple substrates it did generate convincing evidence that synthesising C=C containing IPNs using 22 was problematic. A potential reason for the inability of 22 to cleanly generate 39 or 41 was associated with the propensity of nitronium salts to mediate alkene polymerization [28]. An alternative further plausible explanation for failure to isolate the C=C derived O-nitrates focuses on a report by Scheinbaum and Dines who established that alkenes in the presence of acetonitrile and 22 undergo a Ritter reaction affording vicinal nitro acetamido species [29].  Silver nitrate reacts with alkyl, benzyl or acyl halides affording the corresponding alkyl [30], benzyl [31,32] or acyl nitrates [33]. By way of example and relevant to the work reported here Ogawa et al. [34] transformed bromoacetone to 2-oxopropyl nitrate (component of climate mediated IPN decomposition [35]) using silver nitrate in acetonitrile. Initiating the synthesis of 'test substrate' 43 we reacted silver nitrate in acetonitrile with the cheap, commercial and readily available chloroacetone in place of the less accessible and considerably more expensive bromoacetone. After 16 hours at 40 °C the <15% yield of 43 was disappointing; it seemed the enhanced reactivity associated with bromoacetone was a requirement for an efficient 'bromide to nitrate' substitution. Changing tactics we opted to generate the more reactive iodoacetone in situ from chloroacetone (42) and a stoichiometric quantity of tetra-n-butylammonium iodide (TBAI). Gratifyingly the iodoacetone reacted readily with silver nitrate at 60 °C affording 43 (Scheme 6) as a yellow oil in an unoptimized 69% yield. Unfortunately the unstable and reactive properties of 43 meant purification was not straightforward [36]. However installation of the nitrate group was confirmed via comparison of our data with that in the literature [28]. Thus in the 1 H NMR the downfield shift of the -CH 2 Cl group from 4.15 ppm to 4.94 ppm was associated with the installation of NO 3 affording the -CH 2 ONO 2 group. With this positive result in hand application of the halide to nitrate transformation within the context of IPN synthesis was initiated. Interestingly, although silver nitrate has been widely employed for the synthesis of structure and function diverse benzyl nitrates; the analogous reaction affording allylic nitrates using allylic halide starting materials has, surprisingly, been reported only once [37].
The lack of prior art associated with the synthesis of (E)-2methyl-4-bromobut-2-en-1-ol validated the importance of this seemingly valuable starting material and useful building block. Indeed it is not commercially available and has been reported in the patent literature only once. Following the procedure of Gurumurthy et al. [38] isoprene was reacted with N-bromosuccinimide (NBS, 44) in water at 8-10 °C for 2 h. The reaction afforded a mixture of two allylic bromides and two allylic alcohols in a combined 42% yield, these were tentatively assigned as (E)-45, (Z)-46, rac-47 and rac-48 (route A, Scheme 7). All attempts at separating this mixture using flash column chromatography were unsuccessful. Repeating this reaction but with N-chlorosuccinimide (NCS, route B, [39]) or alternatively using iodine and silver(I) oxide (route C, [40]) we considered the possibility that the resulting allylic chlorides or iodides may be more amenable to separation. Utilizing a procedure reported by Koo et al. [39] isoprene and NCS were stirred in aqueous DMF at ambient temperature for 4 hours. 1 H NMR analysis indicated that (E)-49, (Z)-50, rac-51 and rac-52 had formed. Disappointingly our attempts at isolating and purifying the individual components were only partially successful. Thus although rac-51 and rac-52 could be separated, (E)-49 and (Z)-50 could not.
Disappointed with this outcome we opted to react isoprene with a combination of iodine and silver(I) oxide in aqueous acetonitrile. Our intention was to generate a mixture of, hopefully, separable allylic alcohols and allylic iodides. Interestingly this alternative protocol afforded only two of the possible four products. Thus terminal alkene derived 1-iodo-2-methylbut-3-en-2ol (rac-53) and 2-iodo-2-methylbut-3-en-1-ol (rac-54) were afforded in a 9:1 ratio, respectively, and a pleasing 72% yield (route C, Scheme 7). Analysis via 1 H NMR afforded no evidence for the formation of (E)-or (Z)-2-methyl-4-iodo-2-but-2en-1-ol. Needless to say the formation of rac-53 and rac-54 was of little benefit as their separation proved impractical via flash column chromatography.
As noted (Scheme 2) the efficient separation of (E)-13 and (Z)-14 was not possible without recourse to analytical HPLC [9]. Nevertheless we considered it important to validate our proposed 'halide for nitrate' substitution by undertaking a 'test' reaction using silver nitrate and the allylic bromide/allylic alcohol mixture (E)-45-rac-48. Dissolving this in acetonitrile the reactants were protected from light by wrapping the flask in aluminium foil and one equivalent of silver nitrate was added. The reaction was stirred for 5 hours at ambient temperature after which the reaction was complete, a simple filtration removed the silver bromide that had generated. Subsequent sol-vent removal and analysis via 1 H NMR indicated the IPNs had formed. Subjecting the mixture to flash column chromatography and, similar to previous reports, it was not possible to separate (E)-13, (Z)-14, rac-7 or rac-8 and it was therefore not possible to determine, unambiguously, if all of the above had been formed. Nevertheless physicochemical analysis of the 'purified' mixture (54% yield) indicated the O-nitrate esters were present with distinctive FTIR absorption peaks located at 1635 and 1278 cm −1 . Furthermore changes in the 1 H NMR chemical shifts compared to the starting materials as well as GC-MS analysis (negative ion mode) corroborated the O-nitrate ester groups were present.
Separation of the stereoisomers via flash column chromatography was straightforward. Pure (E)-58 and (Z)-59 were afforded with physicochemical properties essentially identical to those reported [48]. Taking (E)-58 and (Z)-59 forward their reduction to (E)-60 and (Z)-61 using DIBAL-H (−78 °C) was uncomplicated. The corresponding (E)-and (Z)-allylic alcohols were afforded in 87% and 81% yields, respectively. The physicochemical properties of (E)-60 were essentially identical to those reported [49]. The potential for (E)-3-methyl-4-chlorobut-2-en-1-ol ((E)-60) to react with silver nitrate generating (E)-10 (Scheme 1) was investigated. Dissolving it in acetonitrile, the flask was wrapped in aluminium foil and one equivalent of silver nitrate added. After stirring for 16 hours at ambient temperature a sample was removed for 1 H NMR analysis. This indicated approximately 15% of (E)-60 had been consumed. Enhancing the sluggish reactivity of (E)-60 a catalytic amount of sodium iodide (10 mol %) was added (presumably generating in situ the corresponding allylic iodide). After stirring for a further 16 hours, the majority of (E)-60 had reacted as judged by TLC and 1 H NMR analysis. Removing the sodium chloride via a simple filtration was more advantageous than the previously employed organic soluble and more expensive TBAI (Scheme 6). Straightforward flash-column purification afforded (E)-10 in an unoptimized 60% yield and with physicochemical properties similar to those reported [9]. Confident our silver nitrate mediated halide substitution protocol was robust, attention switched to incorporating (Z)-3methyl-4-chlorobut-2-en-1-ol ((Z)-61). Employing a sodium iodide enhanced reaction (10 mol %) using 16 mmol of (E)-61 afforded 1.4 g of (Z)-2-methyl-4-hydroxybut-2-enyl nitrate ((Z)-9) in an unoptimized 60% yield. Comparing the 1 H NMR data associated with (E)-10 and (Z)-9 revealed they were, as expected, broadly similar (see Supporting Information File 1). However, subtle chemical shift differences were evident, most notably with those associated with the CH 3 attached to the C=C bond, i.e., 1.75 ppm ((E)-10) and 1.84 ppm ((E)-9); similarly the CH 2 ONO 2 groups were located at 4.84 ppm for (E)-10 and 4.97 ppm for (Z)-9. Substantiating our tentative carbon-carbon double bond stereochemical assignment for (Z)-9 and (E)-10 was important. Homonuclear two-dimensional NOE spectroscopy (NOESY) was used to explore the C=C double bond configuration. (E)-10 displayed two NOE interactions between the alkene proton and the methylene groups of the adjacent -CH 2 OH and -CH 2 ONO 2 (see 'double-headed arrows', Scheme 9). In (Z)-9 the alkene proton had an NOE interaction with the adjacent CH 3 (see red arrow, Scheme 9) and the methylene of the -CH 2 ONO 2 group likewise had an observable interaction with the CH 3 (see purple arrow). However, unlike (E)-10 no interaction was observed between the alkene proton and the methylene of the -CH 2 OH group. Importantly, the lack of an interaction between the (E)-C=C bound hydrogen on 10 and the '(E)-CH 3 ' group afforded good evidence that 10 was indeed a (E)-configured C=C bond.
Furthermore comparison of our 1 H NMR spectra with the one reported by Lee et al. [19] for structural isomer (E)-4-hydroxy-3-methylbut-2-enyl nitrate ((E-)13, Scheme 2) displayed a subtle chemical shift difference centred on the methyl group attached to the C=C bond. By way of example, (E)-13 displayed the methyl at 1.75(7) ppm whilst we observed the methyl group in (E)-10 as a sharp singlet at 1.69 ppm, perhaps more importantly the alkene proton of silver nitrate generated (E)-10 was identified as a triplet (J = 5.8 Hz) at 5.73 ppm compared with 5.64 ppm (J = 7.2 Hz) for (E)-13. We attempted to further substantiate our assignment by undertaking a structure search on SciFinder for (E)-10 comparing the 1 H NMR data available with ours. However, although 5 papers report (E)-10 none, unfortunately, had any 1 H NMR data.
A SciFinder search for (Z)-9 afforded 3 references, similar to (E)-10, none reported any 1 H NMR data that could be used as reference spectra. In addition to (E)-13 Lee et al. described [19] the synthesis and 1 H NMR of (Z)-14 the structural isomer of (Z)-9. Comparing their physicochemical data sets similar but subtle differences were evident. Thus the alkene proton in (Z)-14 was observed as a triplet (J = 7.6 Hz) at 5.45(7) ppm whilst in our synthesised (Z)-9 the similarly positioned proton was also observed as a triplet but with a smaller coupling constant, e.g., J = 6.4 Hz located at 5.82 ppm.
Attempted conversion of the 1° alcohol on rac-70 into the corresponding 1° alkyl bromide failed to generate the desired product, instead an intractable tar was formed. Changing our approach Anzini et al. [22] demonstrated tetra-n-butylammonium nitrate [17] to be a source of nitrate that was capable of efficiently mediating an S N 2 '1° mesylate for nitrate' substitution, i.e., 72 to 73 (Scheme 12).
Generating the 1° mesylate of rac-70 using methanesulfonyl chloride and pyridine afforded rac-71 in a 77% yield after 16 hours at ambient temperature. Unfortunately subjecting it to a 'mesylate for nitrate' substitution akin to our previously successful 'halide for nitrate' substitution, cf. (E)-60 to (E)-10 (Scheme 9) using silver nitrate did not work and starting material rac-71 was returned in a quantitative yield. Furthermore, we did consider employing the elevated reaction conditions (110 °C) reported by Anzini et al. but were not confident that the O-TBDMS protected O-nitrate ester rac-8 if formed would be stable [8]. For this reason we explored transforming rac-71 into O-TBDMS protected rac-8 at ambient temperature using silver nitrate in acetonitrile. Unfortunately in contrast to previous successful 'halide for nitrate' transformations no reaction was observed with mesylate rac-71 even after extended reaction times. Repeating the reaction but substituting the silver salt for tetra-n-butylammonium nitrate TLC analysis did indicate, after 24 hours, a small percentage (i.e., ~10%) of rac-8 had formed with the remainder comprising rac-71. However using flash column chromatography to separate rac-71 from the, presumed, 1° nitrate ester was not possible.
Circumventing the lack of reactivity displayed by rac-71 the in situ synthesis of a 'naked' nitrate containing species, i.e., [K(18-crown-6)NO 3 ] and its application to mesylate displacement was attempted. Premixing potassium nitrate and 18-crown-6 we envisaged would sequester the potassium cation [52] and generate a [K(18-crown-6)NO 3 ] complex. Using acetonitrile as solvent one equivalent of [K(18-crown-6)NO 3 ] was stirred with rac-71. Disappointingly, although a new compound was generated it accounted for only a small percentage of the reaction mixture. The majority of rac-71 had not reacted and due to purification issues this route to O-nitrate ester synthesis was abandoned.
Disappointed with the lack of reactivity displayed by rac-71 we opted instead to tackle the synthesis of (±)-2-hydroxy-3methylbut-3-enyl nitrate (rac-19). Starting from 3-methyl-2buten-1-ol its conversion, on a multigram scale, to (±)-3-(bromomethyl)-2,2-dimethyloxirane (rac-74) was straightforward. Heating rac-74 with a mixture of acetic anhydride and para-toluenesulfonic acid (PTSA, 1 equiv) afforded via, presumably, protonated rac-75 ring-opened and O-acylated (±)-1-bromo-3-methylbut-3-en-2-yl acetate (rac-76) in a 58% yield. Isolation, solvent removal and purification of rac-76 from the reaction byproducts had to be undertaken swiftly because of its relatively rapid decomposition (10-15 minutes). Negating this, a quick flash column was undertaken and the resulting ~75% pure product was taken on 'as is'. Employing silver nitrate in our standard reaction conditions afforded a novel compound presumed to be (±)-3-methyl-1-(nitrooxy)but-3-en-2-yl acetate (rac-77) in an unoptimized 70% yield. The final stage of the synthesis was the hydrolysis of the O-acetate ester using mild, slightly basic reaction conditions. Thus using potassium carbonate in methanol a new alcohol was afforded in an excellent 94% yield. Seeking structure confirmation a search on SciFinder confirmed rac-19 had been previously reported. However inspection of these manuscripts and, more importantly, their electronic supporting information's established that no 1 H or 13 C NMR data associated with rac-19 was available.
It was during these studies that we noticed the 1 H NMR data, reported by Lee et al., for 1° alcohol rac-16 was, within experimental error, identical to the 1 H NMR observed for the supposed 2° alcohol rac-19 (Scheme 13). It seemed that during our attempted synthesis of rac-16 we had in fact generated rac-19. Accounting for this we propose that activation of the 1° alkyl bromide with silver nitrate generates an electrophilic species similar to rac-78 which in the presence of the proximal O-acetate generates a 5-membered electrophilic acyloxonium species based on rac-79/rac-81. The formation of such species from simpler non C=C containing starting materials has been reported and established ( 1 H NMR) by Gopius et al. [52]. Accounting for the exclusive formation of O-acetate rac-83 the trapping of the more stable 2° allyl carbocation intermediate 82 (generated via ring-opening of rac-81) with nitrate is preferable to the formation of the higher energy/more unstable 1° carbocation 80 (generated via ring-opening of rac-79, Scheme 13). Subsequent formation of rac-83 allows its hydrolysis with potassium carbonate in methanol to generate the observed rac-16.
Isoprene and monoterpenes account for a large percentage of the total emissions that are not non-methane VOCs. Furthermore although monoterpene emissions (127 Tg C yr −1 ) are sig-Scheme 13: Attempted synthesis of 2° alcohol containing 1° nitrate ester rac-19 and the unexpected synthesis of (±)-1-hydroxy-3-methylbut-3-en-2-yl nitrate, rac-16. nificant lower than isoprene [6] (viz. 600 Tg C yr −1 ) they are nonetheless gaining in significance and are now considered to be important contributors to climate chemistry [53]. By way of example although α-pinene is slightly less reactive to the hydroxyl radical (HO • ) than isoprene it does, conversely, have a higher reactivity to O 3 and nitrate radicals ( • NO 3 ) making its atmospheric oxidation significant with respect to regional tropospheric O 3 and NO X concentrations. The oxidation products derived from monoterpenes have been demonstrated to be important in generating atmospheric based secondary organic aerosols (SOA's) that have a significant impact on global radiation [54].
Exploiting our methodology further its diversity and application to monoterpene derived O-nitrate ester synthesis was undertaken using (1R,5S)-(−)-myrtenol (84) which was quickly and efficiently converted into the corresponding optically active 1° alkyl bromide 85 which, due to its instability, was used 'as is' [55]. Employing our standard silver nitrate conditions (1R,5S)-(−)-85 was efficiently transformed into optically active O-nitrate ester (1R,5S)-(−)-86 in an unoptimized 80% yield (Scheme 14). The importance of this preliminary result resides in the increased awareness of the role that monoterpene and sesquiterpene nitrates have in climate chemistry. Research, however, on their role is, similar to IPNs, severely limited by the dearth of convenient protocols capable of generating structure and function diverse monoterpene and sesquiterpene nitrates.
Finally, the kinetics and measurement of the IPNs generated within this study and their relationship to aspects of atmospheric chemistry have been reported [56].

Conclusion
Isoprene, monoterpene and sesquiterpene nitrates are gaining recognition for their significant roles in climate chemistry however an efficient route to their synthesis has yet to be developed. Here we report an efficient silver nitrate mediated synthesis procedure that is broadly applicable to the production of soughtafter 'isoprene nitrates'. The general applicability of this procedure has also been confirmed via its application to the first synthesis of a monoterpene nitrate derived from (1R,5S)-(−)myrtenol. In the former examples our protocol proceeds via the application of Horner-Wadsworth-Emmons Chemistry that generates readily functionalized motifs that undergo an all but previously non-existent, allylic 'halide for nitrate' substitution reaction. A consequence of the broader importance of organic nitrates we envisage our 'halide for nitrate' synthesis transformation will be of considerable interest to, not only atmospheric chemists, but also the wider synthetic and medicinal chemistry communities.

Supporting Information
Supporting Information File 1 Experimental.