Gu Wenlong, Huang Shuangbing, Lei Shan, Yue Jun, Su Zhaoxin, Si Fei
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China; Key Laboratory of Groundwater Remediation of Hebei Province and China Geological Survey, China.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China; Key Laboratory of Groundwater Remediation of Hebei Province and China Geological Survey, China; School of Environmental Studies & State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China.
Sci Total Environ. 2019 Nov 15;691:407-416. doi: 10.1016/j.scitotenv.2019.07.120. Epub 2019 Jul 9.
Leaching dynamics of dissolved organic matter (DOM) from agricultural soil are influenced by the chemistry of irrigation water. This study used multiple spectroscopy methods to investigate the dynamics of DOM in column leaching process by utilizing selected solutions. DOC was leached out by Na solutions more effectively than by Ca, despite the additional contributions of the ligand exchange of SO and the hydrolysis of HCO. The concentration ranking corresponding to solutions is NaSO > NaHCO > NaCl > CaCl. Furthermore, the aromaticity and molecular weights of DOM leached by Na solutions increased with the leaching, whereas contrary trends were reared by Ca. Thus, specific cation substantially affects DOM concentration and composition. Parallel factor analysis of the three-dimensional fluorescence spectra (EEM-PARAFAC) determined the characteristics of DOM components. (1) The long-wavelength, humic-like components (HLC, i.e., C1, C3, and C5) were largely accumulated at the early water saturating stage but attenuated toward dynamic stability in the salt-solution leaching (SSL) stage. (2) Reactive functional group-related HLC (i.e., C2, and C4) remarkably increased in response to the solutions chemistry. (3) The protein-like component (PLC, i.e., C6) was released with insignificant dynamic differences between the solutions. Despite approximately stable DOC concentration at the late stage of each SSL, HLC exhibited accelerating release in sodium salts but declining trend in calcium salt whereas PLC showed a roughly constant dynamic in the both. Ca-bridging reactions with the detachment of OM-Ca-clay complex prompting HLC release and its formation to stabilize the HLC well explain the contrast dynamics of HLC with Na or Ca leaching. The diffusion process that was defined for the slow, lasting and small concentration of leaching of inactive components could contribute to the steady dynamic of PLC, given its insensitivity to either the salt cation. This study identified distinct release kinetics of DOM compositions from those of DOC by EEM-PARAFAC and correspondingly the potential mechanisms, which offers promising advantages in monitoring DOM transport and fractionation in dynamic leaching process.
农业土壤中溶解有机物(DOM)的淋溶动力学受灌溉水化学性质的影响。本研究采用多种光谱方法,利用选定的溶液研究柱淋溶过程中DOM的动力学。尽管SO的配体交换和HCO的水解有额外贡献,但Na溶液比Ca溶液更有效地淋溶出DOC。对应溶液的浓度排序为NaSO>NaHCO>NaCl>CaCl。此外,Na溶液淋溶出的DOM的芳香性和分子量随淋溶增加,而Ca溶液则呈现相反趋势。因此,特定阳离子对DOM的浓度和组成有显著影响。三维荧光光谱的平行因子分析(EEM - PARAFAC)确定了DOM组分的特征。(1)长波长、类腐殖质组分(HLC,即C1、C3和C5)在早期水饱和阶段大量积累,但在盐溶液淋溶(SSL)阶段向动态稳定性衰减。(2)与反应性功能基团相关的HLC(即C2和C4)因溶液化学性质而显著增加。(3)类蛋白组分(PLC,即C6)在不同溶液之间的释放动态差异不显著。尽管在每个SSL阶段后期DOC浓度大致稳定,但HLC在钠盐中表现出加速释放,而在钙盐中呈下降趋势,而PLC在两者中均表现出大致恒定的动态。Ca与OM - Ca - 粘土络合物的桥联反应促使HLC释放,其形成使HLC稳定,很好地解释了HLC在Na或Ca淋溶时的对比动态。对于非活性组分缓慢、持续且浓度较小的淋溶所定义的扩散过程,可能有助于PLC的稳定动态,因为它对盐阳离子均不敏感。本研究通过EEM - PARAFAC确定了DOM组分与DOC不同的释放动力学及其相应的潜在机制,这在监测动态淋溶过程中DOM的迁移和分级方面具有显著优势。