江苏省里下河地区富硒土壤元素地球化学特征及其成因机制
|
廖启林, 黄顺生, 许伟伟, 崔晓丹, 金洋, 刘玲, 汪媛媛, 李文博, 周强
|
Elemental geochemical characteristics and genetic mechanisms of Se-rich soils in the Lixiahe area in Jiangsu Province
|
LIAO Qi-Lin, HUANG Shun-Sheng, XU Wei-Wei, CUI Xiao-Dan, JIN Yang, LIU Ling, WANG Yuan-Yuan, LI Wen-Bo, ZHOU Qiang
|
|
表3 里下河地区富硒土壤元素旋转成分矩阵
|
Table 3 Rotated component matrix of elements distribution in Se-rich soil from the Lixiahe area
|
|
指标 | PC1 | PC2 | PC3 | PC4 | PC5 | PC6 | Se | 0.506 | 0.621 | 0.251 | -0.153 | -0.238 | -0.126 | OM | 0.142 | 0.871 | 0.208 | -0.249 | -0.113 | 0.009 | pH | -0.080 | -0.214 | -0.193 | 0.862 | 0.025 | -0.002 | CEC | 0.414 | 0.758 | 0.149 | -0.067 | -0.091 | -0.152 | N | 0.100 | 0.874 | 0.175 | -0.205 | -0.097 | 0.058 | P | -0.464 | 0.464 | 0.010 | 0.003 | 0.082 | 0.524 | K | 0.947 | 0.027 | 0.019 | -0.150 | -0.013 | -0.003 | Ca | -0.355 | -0.077 | -0.152 | 0.774 | -0.079 | 0.115 | Mg | 0.826 | -0.061 | -0.049 | 0.364 | -0.025 | 0.105 | Fe | 0.960 | 0.048 | 0.154 | -0.097 | 0.069 | -0.025 | Mn | 0.389 | -0.106 | 0.226 | 0.520 | 0.365 | 0.177 | Mo | 0.164 | 0.141 | 0.216 | -0.166 | 0.094 | 0.541 | B | -0.150 | -0.111 | 0.049 | 0.088 | 0.840 | -0.064 | F | 0.575 | 0.129 | 0.003 | -0.239 | 0.620 | 0.000 | Cl | -0.245 | -0.136 | -0.145 | 0.050 | 0.238 | 0.648 | Cd | 0.186 | 0.598 | 0.302 | 0.050 | -0.026 | 0.424 | As | -0.058 | -0.171 | 0.723 | -0.213 | -0.018 | 0.248 | Hg | -0.413 | 0.182 | 0.559 | 0.032 | 0.137 | -0.185 | Sb | 0.267 | 0.143 | 0.685 | -0.170 | 0.123 | 0.042 | Cu | 0.778 | 0.311 | 0.244 | -0.071 | -0.009 | 0.104 | Pb | 0.392 | 0.135 | 0.763 | -0.163 | -0.166 | -0.049 | Zn | 0.354 | 0.298 | 0.380 | -0.024 | 0.043 | 0.493 | Cr | 0.730 | 0.105 | 0.230 | -0.048 | 0.100 | -0.228 | Ni | 0.951 | 0.096 | 0.152 | -0.096 | -0.014 | -0.094 | Co | 0.959 | 0.032 | 0.082 | -0.078 | 0.092 | -0.032 | V | 0.837 | -0.016 | 0.259 | -0.068 | -0.157 | -0.068 | 特征值 | 9.042 | 3.499 | 2.178 | 2.135 | 1.502 | 1.290 | 方差贡献率/% | 34.775 | 13.459 | 8.377 | 8.213 | 5.776 | 4.960 | 累积方差贡献率/% | 34.775 | 48.235 | 56.611 | 64.824 | 70.600 | 75.560 |
|
|
|