<p indent="0mm">High-precision measurements of <sup>238</sup>U/<sup>235</sup>U and <sup>234</sup>U/<sup>238</sup>U atomic ratios are essential for U-Pb and <sup>230</sup>Th/U dating, as well as for a wide range of Earth and environmental studies. The <sup>238</sup>U/<sup>235</sup>U ratio of a natural material has been considered to be a constant of 137.88 since the 1970s. However, recent advances in analytical techniques, such as TIMS (Thermal Ionization Mass Spectrometry) and MC-ICP-MS (Multiple Collector Inductively Coupled Plasma Mass Spectrometry), allowed the measurement of <sup>238</sup>U/<sup>235</sup>U ratios at a precision of 10<sup>−5</sup>, revealing up to 5‰ variations in terrestrial <sup>238</sup>U/<sup>235</sup>U ratios. <sc>The <sup>234</sup>U/<sup>238</sup>U</sc> ratios are commonly observed at the 10<sup>−4</sup>–10<sup>−5</sup> levels in the natural environment. These large differences in abundance make it impossible to simultaneously measure U isotopes in Faraday cups connected to the standard 10<sup>11</sup> Ω current amplifiers using the MC-ICP-MS. To obtain epsilon precision levels in the <sup>234</sup>U/<sup>238</sup>U measurements, previous studies employed a 10<sup>9</sup> or 10<sup>10</sup> Ω amplifier for the <sup>238</sup>U Faraday cup and a 10<sup>11</sup> Ω amplifier for the <sup>234</sup>U Faraday cup. However, these methods require a large quantity of sample material of <sc>400–1000 ng</sc> <sup>238</sup>U, as the 10<sup>11</sup> Ω amplifier has a relatively low signal/noise ratio. In 2014, Thermo Fisher Scientific launched a new Faraday cup current amplifier with a 10<sup>13</sup> Ω feedback resistor, which offers a signal/noise ratio improved by a factor of five compared with standard 10<sup>11</sup> Ω amplifiers. Therefore, we are attempting to use the new 10<sup>13</sup> Ω amplifier in combination with the 10<sup>11</sup> and 10<sup>12</sup> Ω amplifiers to perform high-precision static measurements of U isotopes with Faraday cups using a small amount of sample. In the present study, we simultaneously used a 10<sup>13</sup> Ω amplifier, two 10<sup>12</sup> Ω amplifiers, and two 10<sup>11</sup> Ω amplifiers for the <sup>234</sup>U, the <sup>233</sup>U and <sup>236</sup>U, and the <sup>235</sup>U and <sup>238</sup>U Faraday cups, respectively. To evaluate the relative gain of the 10<sup>13</sup> Ω current amplifier prior to sample analyses, we repeated the measurements of the <sup>238</sup>U/<sup>235</sup>U ratios in a uranium solution with Faraday cups connected to 10<sup>13</sup> and 10<sup>11</sup> Ω amplifiers. The relative gain of the 10<sup>13</sup> Ω amplifier was calculated as (<sup>238</sup>U<sub>11</sub>/<sup>235</sup>U<sub>13</sub>)/(<sup>238</sup>U<sub>11</sub>/<sup>235</sup>U<sub>11</sub>), where the subscript indicates the resistors of the Faraday cup amplifiers. We also developed approaches to correct for the effects of baseline, memory, tailing, hydride, and mass biases. Using the new static measurement method, we repeatedly measured <sup>234</sup>U/<sup>238</sup>U and <sup>238</sup>U/<sup>235</sup>U ratios for the international uranium standards HU-1 and SRM950a, as well as for the national uranium standards GBW04412 and GBW04428. Our results (presented with ±2<italic>σ</italic>) show that the international standards HU-1 (<italic>n</italic>=10) and SRM950a (<italic>n</italic>=10) have <sup>234</sup>U/<sup>238</sup>U atomic ratios of (54.90±0.03)×10<sup>−6</sup> and (53.88±0.03)×10<sup>−6</sup>, and <sup>238</sup>U/<sup>235</sup>U ratios of 137.765±0.010 and 137.844±0.005, respectively. On the other hand, the national standards GBW04412 (<italic>n</italic>=8) and GBW04428 (<italic>n</italic>=10) have <sup>234</sup>U/<sup>238</sup>U ratios of (101.66±0.04)×10<sup>−6</sup> and (53.86±0.03)×10<sup>−6</sup>, and <sc><sup>238</sup>U/<sup>235</sup>U</sc> ratios of 137.786±0.018 and 137.995±0.008, respectively. Our results are consistent with previously published data and demonstrated high reliability. Our study shows that using the new method we can rapidly measure <sup>234</sup>U/<sup>238</sup>U and <sup>238</sup>U/<sup>235</sup>U ratios with precision of 0.3‰–1‰ and 0.3<italic>ε</italic>–0.7<italic>ε</italic>, respectively, consuming <sc>20–30 ng</sc> uranium within ~20 min. In addition, our method is flexible: The combination of different amplifiers can be easily modified according to the characteristics of the analyzed samples and the required measurement precision.