基于空间分析荞麦地流域地下水健康风险评价

以云南荞麦地流域为研究区域,对该区域2017年24个地下水样品中5种重金属指标(Cr、Pb、Co、Mn、Hg)和1种无机毒理指标(氟化物)进行测定和分析,并基于半方差模型等地学统计方法,对地下水健康风险评价进行空间分析.结果表明:地下水通过饮水途径所引起的成人和儿童的健康风险分别为9.27×10^-10~4.59×10^-5a^-1和1.10×10^-8~5.46×10^-4a^-1.地下水健康风险评价值以Cr为主导,成人与儿童存在较高的一致性.地下水健康风险存在很强的空间规律性,在南北方向上呈条带状分布.受位于中游的药山镇影响,研究区南部下游地区地下水健康风险显著增加.

Analysis on the Variation of Rainfall Data from Guilin Weather Station during 1957-2007

[Objective] The research aimed to study the variation of rainfall data from Guilin Weather Station during 1957-2007.[Method] Based on the daily rainfall data in Guilin during 1957-2007,the trend,period and mutation of precipitation in Guilin in 51 years were analyzed by using the trend analysis,wavelet analysis and Mann-Kendall non-parameter statistics test method.[Result] The rainfall in Guilin in 51 years presented the rising trend.The rainfall variation was same in the first,second and third quarters of most years,except in the individual year.The rainfall in the fourth quarter had the decrease trend,and the variation was obvious in each year.It illustrated that the rainfall variation in winter was very unstable and had the decrease trend in recent years.But as a whole,the variation of total rainfall in Guilin wasn't obvious and had the rise trend.It illustrated that the climate variation in Guilin in 51 years wasn't obvious.The wavelet analysis showed that the rainfall variation in Guilin had 15-year big period and the small period of 2-3 years.Mann-Kendall non-parameter statistics test showed that the mutation situation of total rainfall in Guilin in 51 years wasn't obvious.But the mutation situations in the second and third quarters were more.The variation in recent 10 years was the most obvious.Maybe it was affected by the global climate variation.[Conclusion] The research provided the theory basis for analyzing the climate variation in Guilin.

云南荞麦地流域地下水水化学特征及物质来源分析

为研究荞麦地流域地下水的水化学特征及物质来源,2017年7月在研究区共采集地下水的水样32个,综合运用聚类分析、因子分析和路径模型分析等方法,分析了荞麦地流域地下水水化学特征,并定性和定量探讨了荞麦地流域地下水水化学的物质来源.结果表明,研究区内水体整体呈弱碱性,Ca^(2+)、Mg^(2+)、SO_4^(2-)、HCO_3^-和N_3O^-等主要阴阳离子具有较高的空间变异性.通过聚类分析可知,研究区内地下水可分为两大类:A类和B类,分别具有两个子集:A_1、A_2、B_1和B_2,并且从A类地下水到B类地下水化学类型开始变得复杂,A类地下水水化学类型均为HCO_3-Ca型,B_1类地下水和B_2类地下水分别有HCO_3-Ca型、HCO_3-Na·Ca型、HCO_3-Na·Ca·Mg型和HCO_3-Ca型、HCO_3-Ca·Mg型、HCO_3-Na·Ca型各3类.为进一步探讨地下水水化学的影响因素,通过因子分析和路径模型分析可确定碳酸盐岩、人类活动、蒸发岩和硅酸盐岩是地下水的主要物质来源.其中人类活动的作用和MgSO_4型蒸发岩的溶解,是形成以碳酸盐岩为地下水化学组分的主要来源,同时具有多元地下水水化学特征的重要原因.