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The Statistical Characteristics of pH Measurement Bias in the Monitoring Data of CMA-ARMN
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摘要: 该文对1992—2011年的酸雨观测资料中存在的pH测量负偏差进行统计分析。结果显示：除西北地区、青藏高原外的大部分酸雨观测站不同程度地出现pH值测量负偏差，总体上南方地区台站的pH测量负偏差问题较北方地区突出；随着测量仪器的更新换型、观测业务规范化管理水平的提升以及一些针对性技术措施的实施，存在pH测量负偏差问题的观测台站比例从20世纪90年代的40%以上下降为25%，观测资料中受pH测量负偏差影响的数据比例由10%下降到2%。pH负偏差的量值与降水pH值之间存在一定依存关系:降水pH值越低，负偏差问题越严重，pH负偏差的主要量值分布区间为-0.6~0，约占负偏差数据的80%。Abstract: Precipitation pH and conductivity are measured routinely in the nation-wide network with more than 300 stations, known as the Acid Rain Monitoring Network (ARMN), under the infrastructure of China Meteorological Administration (CMA) since early 1990s. Previous studies indicate that a systematic negative bias in the pH measurement, caused by the aging of pH electrode, which has weakened the data quality obviously. Characteristics of the bias are investigated to describe the temporal and spatial features of the negative pH measurement bias (NBpH) and to estimate its magnitude with meticulous statistical approaches, based on the monitoring dataset obtained from CMA-ARMN during 1992—2011. The result indicates that 40% stations of CMA-ARMN suffers from NBpH problem in the early 1990s, while this ratio decreases to 25% during 2010—2011. The proportion of data infected with NBpH problem during 2010—2011 reduces to 2% from 10% in the early 1990s. This improvement of pH measurement mentioned above can be attributed to the renewal of pH meter for all CMA-ARMN stations in 2000, the re-approval of Standard Operation Manual of CMA-ARMN in 2005, and the recent trail measures on the pH electrode aging. Also, statistics shows that NBpH problem seldom occurs in the stations over the Northwest China and Qinghai-Tibet Plateau, but frequently occurs in the stations of other regions over China. On the whole, NBpH problem in southern part of China is more serious than those in the northern part of China. This geographical feature of NBpH is related with the behavior of aged pH electrode which shows bigger negative bias when measuring the solution of low pH and low conductivity. Quasi-quantitative estimation of NBpH based on the K-pH inequality principle shows that the magnitude of NBpH for about 80% data ranges from-0.6 to 0, with a few of extremes lower than-3.0. The lower pH is, the larger NBpH tends to be. To avoid NBpH problem in future, substitution of the now-using normal pH electrode in CMA-ARMN with the pH electrode for low ion strength is suggested, together with the corresponding QA/QC (quality assurance/quality control) procedures. In addition, the possibility and the example of data correction with NBpH are discussed.
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图 2 对3个酸雨观测站1992—2006年数据进行K-pH不等式检验的结果
(图中虚线由左至右依次是ΔpH为-0.1，-0.2，-0.4，-0.8，-1.6时，ΔK与pHm的理论关系曲线)
Fig. 2 The K-pH inequality test results of datasets from 3 CMA-ARMN stations
(dashed lines show the relationship of ΔK to pHm, given ΔpH =-0.1, -0.2, -0.4, -0.8, -1.6, respectively )
图 3 1992—2011年以来全国酸雨观测站网pH测量负偏差的整体统计分布
(a)Q(全部台站数据，图中横线为多年平均值)，(b) 酸雨观测站总数，(c) 无pH测量负偏差 (即Q=0) 台站比例 (直线为线性趋势线)
Fig. 3 The statistical tendency of the pH measurement bias of CMA-ARMN from 1992 to 2011
(a)Q(all data, the solid lines show the averaged Q for different periods), (b) the total number of CMA-ARMN stations, (c) percentages of the station withoutNBpH detected in the K-pH inequality check (e.g., Q=0)
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[1] 李洪珍, 王木林.我国降水酸度的初步研究.气象学报, 1984, 42(3):332-339. doi: 10.11676/qxxb1984.038 [2] 丁国安, 徐晓斌, 王淑凤, 等.中国气象局酸雨网基本资料数据集及初步分析.应用气象学报, 2004, 15(增刊):85-94. http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFQ&dbname=CJFD2004&filename=YYQX2004S1012&v=MDE5MDBGckNVUkwyZll1WnBGeXpsVkwzT1BEVGFkckc0SHRXdnJvOUVab1I4ZVgxTHV4WVM3RGgxVDNxVHJXTTE= [3] 汤洁, 徐晓斌, 王淑凤, 等.1992—2006年我国降水酸度的变化趋势.科学通报, 2010, 55(8):705-712. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201008009.htm [4] 王文兴, 许鹏举.中国大气降水化学研究进展.化学进展, 2009, 21(2-3):266-281. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKJ201101002.htm [5] 中国气象局气象探测中心, 中国气象科学研究院.酸雨观测年报 (2010年).2011. http://www.cnki.com.cn/Article/CJFDTOTAL-SYQY201603027.htm [6] 汤洁, 徐晓斌, 巴金, 等.电导率加和性质及其在酸雨观测数据质量评估中的应用.应用气象学报, 2008, 19(4):1-8. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20080401&flag=1 [7] 汤洁, 程红兵, 于晓岚, 等.全国酸雨观测网未知水样考核结果的统计分析.气象, 2007, 33(12):75-83. doi: 10.7519/j.issn.1000-0526.2007.12.011 [8] 汤洁, 俞向明, 程红兵, 等.酸雨观测中pH值测量负偏差来源的分析.应用气象学报, 2010, 21(4):458-463. doi: 10.11898/1001-7313.20100409 [9] 中国气象局.酸雨观测方法 (试行二版).北京:中国气象局, 1992. http://www.cnki.com.cn/Article/CJFDTOTAL-SYQY201603027.htm [10] 中国气象局.酸雨观测业务规范.北京:气象出版社, 2005. http://www.cnki.com.cn/Article/CJFDTOTAL-SYQY201603027.htm [11] 汤洁, 薛虎圣, 于晓岚, 等.瓦里关山地区降水化学特征的初步分析.环境科学学报, 2000, 20(4):420-425. http://www.cnki.com.cn/Article/CJFDTOTAL-HJXX200004007.htm [12] WMO. Manual for the GAW Precipitation Chemistry Programme (Guideline, Data Quality Objectives and Standard Operating Procedures). WMO-TD No.1251, 2004. [13] ASTM International.Standard Test Methods for pH Measurement of Water of Low Conductivity.ASTM D 5464-93 (Reapproved 2001), 2001. [14] 国家质量监督检验检疫总局. GB/T19117-2003《酸雨观测规范》. 北京: 中国标准出版社, 2003. [15] 国家环境保护局. GB/T6920-86水质pH值的测定: 玻璃电极法. 北京: 环境出版社, 1987. [16] 林国元, 江劲军, 朱继承, 等. pH玻璃电极对比观测误差研究.福建地震, 2007, 23(3-4):32-34. http://www.cnki.com.cn/Article/CJFDTOTAL-FJDI2007Z2010.htm [17] 叶宪曾, 张新祥.仪器分析教程.北京:北京大学出版社, 2007. http://www.cnki.com.cn/Article/CJFDTOTAL-SYQY201603027.htm [18] 董胜敏, 王承遇, 潘玉昆. pH玻璃电极的现状与发展.玻璃与搪瓷, 2004, 32(2):53-58. http://www.cnki.com.cn/Article/CJFDTOTAL-BLTC200402010.htm [19] Erich K S. pH Measurement Guide. [2012-03-03]. http://www.hamiltoncompany.com [20] 任芝花, 熊安元, 邹凤玲.中国地面月气候资料质量控制方法的研究.应用气象学报, 2007, 18(4):516-523. doi: 10.11898/1001-7313.20070412 [21] 张强, 涂满红, 马舒庆, 等.自动雨量站降雨资料质量评估方法研究.应用气象学报, 2007, 18(3):365-372. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20070359&flag=1 [22] 张强, 阮新, 熊安元.近57年我国气温格点数据集的建立和质量评估.应用气象学报, 2010, 21(4):385-393. doi: 10.11898/1001-7313.20100401 [23] 巴金. 中国地区酸雨的长期演变及时空分布特征分析. 北京: 中国气象科学研究院, 2008. -
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