[1] 郑毅. 基于城市黑臭水体治理与水质长效改善的技术分析[J]. 资源节约与环保, 2015(12): 187.
[2] 沈烁, 王育来, 杨长明, 等. 南淝河不同排口表层沉积物DOM光谱特征[J] .中国环境科学, 2014, 34(9): 2351-2361.
[3] 杨楠, 于会彬, 宋永会, 等. 应用多元统计研究城市河流沉积物孔隙水中DOM紫外光谱特征[J]. 环境科学学报, 2014, 34(7): 1751-1757.
[4] 李璐璐, 江韬, 卢松, 等. 利用紫外-可见吸收光谱估算三峡库区消落带水体、土壤和沉积物溶解性有机质(DOM)浓度[J]. 环境科学, 2014, 35(9): 3408-3416.
[5] 赵越, 魏雨泉, 李洋,等. 不同物料堆肥腐熟程度的紫外-可见光谱特性表征[J]. 光谱学与光谱分析, 2015, 35(4): 961-965.
[6] 王齐磊, 江韬, 赵铮, 等. 三峡库区典型农业小流域土壤溶解性有机质的紫外-可见及荧光特征[J]. 环境科学, 2015, 36(3): 879-887.
[7] 吕纯剑, 高红杰, 李晓洁,等. 沈阳市黑臭水体溶解性有机物组分及其光学特征[J]. 环境工程学报, 2019, 13(3): 559-568.
[8] 张甲申, 曹军. 土壤水溶性有机物的紫外光谱特征及地域分异[J]. 土壤学报, 2003, 40(1): 118-122.
[9] 李丹, 何小松, 高如泰, 等. 紫外-可见光谱研究堆肥水溶性有机物不同组分演化特征[J]. 中国环境科学, 2016, 36(11): 3412-3421.
[10] 李会杰. 腐殖酸和富里酸的提取与表征研究[D]. 武汉: 华中科技大学, 2012.
[11] GUO X J, YUAN D H, JIANG J Y, et al. Detection of dissolved organic matter in saline-alkali soils using synchronous fluorescence spectroscopy and principal component analysis[J]. Spectrochim Acta Part A: Molecular and Biomolecular Spectroscopy, 2013, 104(3): 280-286.
[12] YU H B, SONG Y H, PAN H W, et al. Synchronous fluorescence spectroscopy combined with two-dimensional correlation and principle component analysis to characterize dissolved organic matter in an urban river[J]. Environmental Monitoring & Assessment, 2016, 188(10): 579.
[13] DRYER D J, KORSHIN G V, FABBRICINO M. In situ examination of the protonation behavior of fulvic acids using differential absorbance spectroscopy[J]. Environmental Science & Technology, 2008, 42(17): 6644-6649.
[14] MARKAGER S S. Tracing the production and degradation of autochthonous fractions of dissolved organic matter by fluorescence analysis[J]. Limnology and Oceanography, 2005, 50(5): 1415-1426.
[15] YAN M, DRYER D, KORSHIN G V, et al. In situ study of binding of copper by fulvic acid: Comparison of differential absorbance data and model predictions[J]. Water Research, 2013, 47(2): 588-596.
[16] ZHU Y Z, SONG Y H, YU H B, et al. Characterization of dissolved organic matter in Dongjianghu Lake by UV-visible absorption spectroscopy with multivariate analysis[J]. Environmental Monitoring & Assessment, 2017, 189(9): 443.
[17] NISHIJIMA W, KIM W H, SHOTO E, et al. The performance of an ozonation-biological activated carbon process under long term operation[J]. Water Science & Technology, 1998, 38(38): 163-169.
[18] 岳兰秀, 吴丰昌, 刘丛强, 等. 红枫湖和百花湖天然溶解有机质的分子荧光特征与分子量分布的关系[J]. 科学通报, 2005, 50(24): 2774-2780.
[19] BARRETO S R G, NOZAKI J, BARRETO W J. Origin of dissolved organic carbon studied by UV‐vis spectroscopy[J]. Clean- Soil Air Water, 2010, 31(6): 513-518.
[20] 陶澍, 崔军, 张朝生. 水生腐殖酸的可见-紫外光谱特征[J]. 地理学报, 1990, 45(4): 484-489.
[21] HELMS J R, STUBBINS A, RITCHIE J D, et al. Absorption spectral slopes and slope ratios as indicators of molecular weight, source, and photobleaching of chromophoric dissolved organic matter[J]. Limnology & Oceanography, 2008, 53(3):955-969.
[22] CHEN Y, SENESI N, SCHNITZER M. Information provided on humic substances by E4/E6 ratios[J]. Soil Science Society of America Journal, 1977, 41(2): 352-358.
[23] ALBRECHT R, LE P J, TERROM G, et al. Comparison between UV spectroscopy and Nirs to assess humification process during sewage sludge and green wastes co-composting[J]. Bioresource Technology, 2011, 102(6): 4495-4500.