采用实时数字仿真系统(RTDS——Real Time Digital Simulation)对太阳能进行并网控制仿真,主电路采用直流-直流(DC-DC)、直流-交流(DC-AC)与LCL滤波电路组成的两级式光伏并网发电结构。通过调节DC-DC电路的占空比来实现光伏电池阵列的...采用实时数字仿真系统(RTDS——Real Time Digital Simulation)对太阳能进行并网控制仿真,主电路采用直流-直流(DC-DC)、直流-交流(DC-AC)与LCL滤波电路组成的两级式光伏并网发电结构。通过调节DC-DC电路的占空比来实现光伏电池阵列的最大功率点跟踪(MPPT——Maximum Power Point Tracking)控制。提出了定电压/定无功(V/Q)控制策略,无需采用复杂的锁相控制技术,成功实现了逆变器的并网控制,保证了输出正弦波形的质量与电网同频、同相的控制要求。展开更多
A Sino\|French refraction\|reflection experiment was conducted in October 1998 in the northeastern edge of the Tibetan Plateau from the Qiang Tang through the north Kunlun block.The successive wide\|angle reflection t...A Sino\|French refraction\|reflection experiment was conducted in October 1998 in the northeastern edge of the Tibetan Plateau from the Qiang Tang through the north Kunlun block.The successive wide\|angle reflection traveltime curves are modeled trying to keep the minimum structure. First results obtained along this 700km transect, show the contrast of crustal structure between the three blocks crossed and the state of the crustal material.North of the Kunlun suture, a change of the Moho depth appears from the Qaidam basin, 55km, to the south approaching the Kunlun range, 65km. But the main crustal characteristic is a great thickness of upper crustal material and the lack of lower crust. This implies a crustal average velocity of 6 2km/s, which is much lower than the worldwide average of 6 45km/s. Interpretations of this crustal column may consider, assuming the crust had been normal that while its upper part thickened the lower one was transported away, underthrust to the south or to depth. Alternatively the velocity in the lower crust may have been changed by metamorphism.展开更多
文摘采用实时数字仿真系统(RTDS——Real Time Digital Simulation)对太阳能进行并网控制仿真,主电路采用直流-直流(DC-DC)、直流-交流(DC-AC)与LCL滤波电路组成的两级式光伏并网发电结构。通过调节DC-DC电路的占空比来实现光伏电池阵列的最大功率点跟踪(MPPT——Maximum Power Point Tracking)控制。提出了定电压/定无功(V/Q)控制策略,无需采用复杂的锁相控制技术,成功实现了逆变器的并网控制,保证了输出正弦波形的质量与电网同频、同相的控制要求。
文摘A Sino\|French refraction\|reflection experiment was conducted in October 1998 in the northeastern edge of the Tibetan Plateau from the Qiang Tang through the north Kunlun block.The successive wide\|angle reflection traveltime curves are modeled trying to keep the minimum structure. First results obtained along this 700km transect, show the contrast of crustal structure between the three blocks crossed and the state of the crustal material.North of the Kunlun suture, a change of the Moho depth appears from the Qaidam basin, 55km, to the south approaching the Kunlun range, 65km. But the main crustal characteristic is a great thickness of upper crustal material and the lack of lower crust. This implies a crustal average velocity of 6 2km/s, which is much lower than the worldwide average of 6 45km/s. Interpretations of this crustal column may consider, assuming the crust had been normal that while its upper part thickened the lower one was transported away, underthrust to the south or to depth. Alternatively the velocity in the lower crust may have been changed by metamorphism.
