Research Article
A Regional Scale Investigation on Groundwater Arsenic in Different Types of Aquifers in the Pearl River Delta, China
Table 2
Principal component (PC) loadings for groundwater samples in granular aquifers.
| Item | PC1 | PC2 | PC3 | PC4 | PC5 | PC6 | PC7 |
| pH | 0.105 | 0.755 | 0.163 | 0.174 | 0.025 | −0.011 | −0.043 | EC | 0.766 | 0.432 | 0.196 | 0.102 | 0.386 | −0.053 | 0.003 | DO | −0.274 | −0.206 | −0.163 | −0.134 | −0.045 | 0.500 | −0.312 | Eh | −0.015 | −0.248 | −0.051 | −0.055 | 0.069 | 0.707 | 0.219 | K+ | 0.314 | 0.286 | 0.046 | −0.044 | 0.804 | −0.035 | 0.038 | Na+ | 0.942 | 0.151 | 0.065 | 0.053 | 0.107 | −0.085 | 0.027 | Ca2+ | 0.324 | 0.753 | 0.239 | 0.158 | 0.314 | −0.233 | −0.043 | Mg2+ | 0.812 | 0.277 | 0.079 | 0.067 | 0.100 | 0.174 | −0.059 | | 0.240 | 0.186 | 0.571 | 0.519 | −0.113 | 0.260 | −0.072 | Fe | 0.125 | 0.060 | 0.244 | 0.672 | −0.141 | −0.324 | 0.123 | | 0.363 | 0.712 | 0.431 | 0.272 | −0.026 | −0.109 | −0.048 | Cl− | 0.945 | 0.092 | 0.010 | 0.039 | 0.178 | −0.057 | 0.030 | | 0.399 | 0.541 | −0.131 | 0.064 | 0.420 | −0.168 | 0.026 | F− | 0.135 | 0.717 | −0.098 | −0.100 | −0.223 | −0.031 | 0.203 | | 0.236 | −0.174 | −0.072 | −0.157 | 0.814 | 0.068 | −0.048 | TDS | 0.675 | 0.530 | 0.294 | 0.138 | 0.350 | −0.129 | −0.026 | TH | 0.535 | 0.692 | 0.217 | 0.148 | 0.283 | −0.125 | −0.054 | I− | −0.021 | 0.136 | 0.361 | 0.684 | 0.088 | 0.039 | 0.186 | | 0.048 | 0.203 | 0.900 | 0.064 | 0.031 | 0.016 | 0.023 | Al | −0.034 | 0.019 | −0.011 | 0.047 | −0.018 | 0.096 | 0.905 | Mn | 0.058 | 0.075 | −0.127 | 0.851 | −0.070 | 0.044 | −0.116 | | 0.252 | 0.338 | 0.218 | 0.376 | −0.156 | 0.541 | 0.063 | As | 0.101 | 0.022 | 0.890 | 0.116 | −0.021 | −0.147 | −0.004 | Eigenvalue | 4.6 | 3.9 | 2.7 | 2.3 | 2.1 | 1.4 | 1.1 | Explained variance (%) | 19.9 | 17.1 | 11.7 | 10.1 | 9.2 | 6.2 | 4.8 | Cumulative% of variance | 19.9 | 37.0 | 48.8 | 58.9 | 68.1 | 74.3 | 79.1 |
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