Mustapha Adamu, Aris Ahmad Zaharin, Ramli Mohammad Firuz, Juahir Hafizan
Centre of Excellence for Environmental Forensics, Faculty of Environmental Studies, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia.
ScientificWorldJournal. 2012;2012:294540. doi: 10.1100/2012/294540. Epub 2012 Jul 31.
Robust statistical tools were applied on the water quality datasets with the aim of determining the most significance parameters and their contribution towards temporal water quality variation. Surface water samples were collected from four different sampling points during dry and wet seasons and analyzed for their physicochemical constituents. Discriminant analysis (DA) provided better results with great discriminatory ability by using five parameters with (P < 0.05) for dry season affording more than 96% correct assignation and used five and six parameters for forward and backward stepwise in wet season data with P-value (P < 0.05) affording 68.20% and 82%, respectively. Partial correlation results revealed that there are strong (r(p) = 0.829) and moderate (r(p) = 0.614) relationships between five-day biochemical oxygen demand (BOD(5)) and chemical oxygen demand (COD), total solids (TS) and dissolved solids (DS) controlling for the linear effect of nitrogen in the form of ammonia (NH(3)) and conductivity for dry and wet seasons, respectively. Multiple linear regression identified the contribution of each variable with significant values r = 0.988, R(2) = 0.976 and r = 0.970, R(2) = 0.942 (P < 0.05) for dry and wet seasons, respectively. Repeated measure t-test confirmed that the surface water quality varies significantly between the seasons with significant value P < 0.05.
运用稳健的统计工具处理水质数据集,目的是确定最重要的参数及其对水质随时间变化的影响。在旱季和雨季从四个不同采样点采集地表水样本,并分析其理化成分。判别分析(DA)通过使用五个参数(P < 0.05)在旱季提供了更好的结果,判别能力很强,正确分类率超过96%;在雨季数据中,向前和向后逐步判别分析分别使用五个和六个参数(P值,P < 0.05),正确分类率分别为68.20%和82%。偏相关结果显示,在控制氨(NH₃)形式的氮的线性效应以及旱季和雨季的电导率的情况下,五日生化需氧量(BOD₅)与化学需氧量(COD)、总固体(TS)与溶解固体(DS)之间分别存在强相关(r(p) = 0.829)和中度相关(r(p) = 0.614)。多元线性回归确定了每个变量的贡献,旱季和雨季的显著值分别为r = 0.988,R² = 0.976和r = 0.970,R² = 0.942(P < 0.05)。重复测量t检验证实,不同季节之间地表水水质差异显著,显著值P < 0.05。