| 1. | Total field measurement is not always desirable . 总磁场测量不是始终需要的。 |
| 2. | The orthonormality relations also permit us to express the power carried by the total field in terms of the expansion coefficients . 根据正交性我们还可以用展开系数来表示整个场承载的功率。 |
| 3. | Represents a running total field used in the report 表示报表中使用的运行总和字段。 |
| 4. | Contains the runningtotalfielddefinition objects for every running total field in the report 包含报表中的每个运行总计字段的 |
| 5. | This class provides properties for getting information on running total fields in the report 该类提供属性以获取报表中的运行总和字段的信息。 |
| 6. | The component in any direction of the total field intensity figured out from the single horizon is called component of single - layer field intensity 将从单层位出发求得的总场强沿任意方向的分量称为单层场强分量。 |
| 7. | While discussing radiation the total field intensity is integrated along the line basing on the real current which is gained through crosstalk between lines 在分析芯线的辐射发射时利用线间耦合所得的实际电流分布沿线长进行积分,得到场点的发射场强。 |
| 8. | Meanwhile the technology for separating scattering field from total field is improved in this paper , which could eliminate the calculation error and get precise scattering field 论文还改进了时域有限差分方法中的总场散射场的分离技术,消除了原来因为分离带来的计算误差,提高了散射计算的精度。 |
| 9. | In order to show the scattering and complex mode - conversion clearly , the total field is decomposed into longitudinal and transverse parts and the scattered field is obtained by subtracting incident wave from the total field 通过对纵横波的分离和在全波场中对散射波的分离,清晰地显示了裂纹对脉冲超声波的散射和复杂的模式转换。 |
| 10. | Surrounding these special problems met in gas hydrates exploration and through study of high - precision magnetic survey , the sea test by r / v haiyang 1y that is owned by guangzhou marine geological survey in dongsha area of the south china sea , systematical analysis of the test result and combination interpretation of magnetic survey with seismic profile , the authors successfully employ the method to recognize the truth or false of the diapir in seismic profile by integrating total field of high - precision marine magnetic measurement with its gradient change 本文就目前天然气水合物调查中存在的这些特殊技术问题,通过对海上高精度磁力测量技术方法研究、广州海洋地质调查局“海洋四号”船在南海北部东沙海域的海上试验、对试验结果的系统研究分析以及磁测和地震剖面两种手段的综合解释,成功地尝试了用高精度海洋磁测成果中的磁力总场和梯度变化特徵来识别水合物勘探中高分辨率地震剖面上的泥底辟构造真伪的技术方法。 |