Conte Pellegrino
Dipartimento di Scienze Agrarie e Forestali, Università degli Studi di Palermo, v.le delle Scienze edificio 4, 90128, Palermo, Italy.
Magn Reson Chem. 2015 Sep;53(9):711-8. doi: 10.1002/mrc.4174. Epub 2014 Oct 30.
Aqueous salt solutions play an important role in nature because of their effects on environmental biogeochemical processes and on structural properties of biomolecules. Upon dissolution, salts split in ions that are solvated. Water in hydration shells is subjected to molecular motions that can be monitored by (1)H T1 NMR relaxometry. This technique allowed the evaluation of the nature of the interactions between water and ions via variable temperature experiments. Examination of relaxometry properties of aqueous solutions at variable salt concentrations allowed acknowledgement of the role played by ions in either structuring or destructuring water aggregates. A mathematical model has been applied on six environmentally relevant salts: NaCl, KCl, CaCl2, CaCO3, NaNO3, and NH4NO3. It was linear only for the concentration dependence of KCl-R1. This model accorded with the one reported in literature where it has been considered valid only for diluted solutions. However, in the present study, the range of linearity for KCl was extended up to the saturation point. The model was modified for NaCl, CaCl2, and CaCO3 by using it as an exponential form in order to account for the nonlinearity of the R1-versus-concentration curves. Nonlinearity was explained by the nonnegligible ion-ion interactions occurring as concentration was increased. Finally, further modification was needed to account for the asymmetric distribution of water around nitrate (in NaNO3 and NH4NO3) and ammonium (in NH4NO3). This study is preliminary to the comprehension of the diffusion mechanisms of ions in water solutions at the equilibrium condition with solid surfaces such as soils and biochar-amended soils.
盐水溶液在自然界中起着重要作用,因为它们对环境生物地球化学过程以及生物分子的结构特性有影响。溶解后,盐会分解成被溶剂化的离子。水合壳中的水会发生分子运动,这可以通过¹H T1 NMR弛豫测量法进行监测。该技术通过变温实验能够评估水与离子之间相互作用的性质。研究不同盐浓度下水溶液的弛豫特性,有助于认识离子在构建或破坏水聚集体中所起的作用。已将一个数学模型应用于六种与环境相关的盐:氯化钠、氯化钾、氯化钙、碳酸钙、硝酸钠和硝酸铵。该模型仅对氯化钾 - R1的浓度依赖性呈线性。此模型与文献中报道的模型相符,在文献中该模型仅被认为对稀溶液有效。然而,在本研究中,氯化钾的线性范围扩展至饱和点。对于氯化钠、氯化钙和碳酸钙,通过将该模型用作指数形式进行修改,以考虑R1 - 浓度曲线的非线性。随着浓度增加,不可忽略的离子 - 离子相互作用导致了非线性。最后,需要进一步修改以考虑硝酸盐(在硝酸钠和硝酸铵中)和铵(在硝酸铵中)周围水的不对称分布。本研究是理解离子在与土壤和生物炭改良土壤等固体表面处于平衡状态的水溶液中扩散机制的初步研究。