Luo Hui-Long, Chen Juan, Zhang Yun-Hui, Yuan Bei, Yang Bin, Zhang Hao, Du Ping
Technical Center for Soil, Agriculture and Rural Ecology and Environment, Ministry of Ecology and Environment, Beijing 100012, China.
State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Huan Jing Ke Xue. 2022 Jun 8;43(6):3315-3327. doi: 10.13227/j.hjkx.202110112.
Studying the chemical composition and characteristic differences of soil dissolved organic matter (DOM) is significant for understanding the mechanism of Cd immobilization by soil amendments. Soil amendments have been widely applied to contaminated farmlands to reduce the accumulation of heavy metals in crops, but the spectral characteristics of DOM in soils under amendment regulation have rarely been studied. Typical Cd-contaminated paddy soil from South China was collected, three categories of amendments (organic-based, inorganic-based, and lime-based, a total of 11 types) were applied, rice planting pot trials were done, and the effects of different amendments on soil DOM were investigated. The spectral characteristics of rhizosphere soil DOM under the regulation of different amendments were comparatively analyzed using UV-Vis spectroscopy, 3D fluorescence spectroscopy, and parallel factor analysis (PARAFAC). The results showed that the lime-based amendments increased the soil pH and promoted the dissolution of organic matter from the soil solid phase, resulting in a significant increase in soil DOM content. Compared with that of the control, organic-based amendments increased the relative molecular weight and recent autochthonous origin contribution of soil DOM, inorganic-based amendments increased the aromatic content and hydrophobic components of soil DOM, and lime-based amendments increased the chromogenic components and the degree of humification of soil DOM. Four fluorescence components, C1 (255/465), C2 (325/400), C3 (275/390), and C4 (240/460), were identified using PARAFAC and verified with the OpenFluor database, all of which were humic-like. Two types of spectra corroborated with each other, indicating that soil DOM dominated by humus-like matter originated from terrestrial source input. The correlation analysis showed that the fluorescent component C4 of soil DOM could be used to predict Cd accumulation in brown rice in the red limestone soil-rice system. These results will provide a reference for the selection of the appropriate soil amendments.
研究土壤溶解有机 matter (DOM) 的化学组成和特征差异对于理解土壤改良剂固定镉的机制具有重要意义。土壤改良剂已广泛应用于受污染农田,以减少作物中重金属的积累,但在改良调控下土壤中 DOM 的光谱特征鲜有研究。采集了中国南方典型镉污染稻田土壤,施用了三类改良剂(有机类、无机类和石灰类,共 11 种),进行了水稻种植盆栽试验,研究了不同改良剂对土壤 DOM 的影响。利用紫外可见光谱、三维荧光光谱和平行因子分析 (PARAFAC) 对不同改良剂调控下根际土壤 DOM 的光谱特征进行了比较分析。结果表明,石灰类改良剂提高了土壤 pH 值,促进了土壤固相有机质的溶解,导致土壤 DOM 含量显著增加。与对照相比,有机类改良剂增加了土壤 DOM 的相对分子量和近期自生源贡献,无机类改良剂增加了土壤 DOM 的芳香族含量和疏水成分,石灰类改良剂增加了土壤 DOM 的发色成分和腐殖化程度。利用 PARAFAC 识别出四个荧光组分 C1(255/465)、C2(325/400)、C3(275/390) 和 C4(240/460),并通过 OpenFluor 数据库进行了验证,所有这些组分均为类腐殖质。两种光谱相互印证,表明以类腐殖质为主的土壤 DOM 来源于陆源输入。相关性分析表明,土壤 DOM 的荧光组分 C4 可用于预测红壤性水稻土 - 水稻系统中糙米镉的积累。这些结果将为选择合适的土壤改良剂提供参考。