【目的】设计日光温室主动蓄放热冠层增温系统(Active heat storage-release system for canopy warming,AHSCW)并进行实地试验,分析该系统对番茄冠层的增温效果,为进一步探讨主动蓄放热热能的高效应用方式和作物局部增温系统的设计提...【目的】设计日光温室主动蓄放热冠层增温系统(Active heat storage-release system for canopy warming,AHSCW)并进行实地试验,分析该系统对番茄冠层的增温效果,为进一步探讨主动蓄放热热能的高效应用方式和作物局部增温系统的设计提供参考。【方法】在第六代主动蓄放热系统基础上设计AHSCW,以太阳能为热源,白天通过水循环将太阳能以热能的形式收集于蓄热水池内,夜间通过冠层增温管道释放热量,对番茄冠层进行局部增温。以使用AHSCW的日光温室为试验温室,未加温的日光温室为对照温室,通过测定太阳辐射强度、番茄冠层空气温度、水温及水泵耗电量参数及不同时期番茄的株高、茎粗和产量,对系统的增温效果进行测试与分析。【结果】白天AHSCW的蓄热量为166~194 MJ,夜间放热量为129~142 MJ,能量利用效率为67%~86%;该系统能够提高番茄冠层区域气温1.4~3.0℃;AHSCW温室果实产量为1.14 kg/m^2,是对照温室(0.64 kg/m^2)的1.77倍。【结论】AHSCW可以明显提高番茄冠层气温,保证番茄的越冬生产,促进番茄生长,增加其产量并可使果实提前成熟上市。展开更多
SHRIMP U-Pb zircon dating on the Xileketehalasu granodiorite porphyry and Kalasayi monodiorite porphyry that intrude middle Devonian Beitashan Formation at the north part of east Junggar region shows that they were fo...SHRIMP U-Pb zircon dating on the Xileketehalasu granodiorite porphyry and Kalasayi monodiorite porphyry that intrude middle Devonian Beitashan Formation at the north part of east Junggar region shows that they were formed at 381±6 Ma and 376±10 Ma respectively. They are interpreted as subduction-related granitic rocks, which is the first report that the isotopic ages for the granitic rocks range from 350 to 390 Ma. Another determined age for the Kalasayi monodiorite porphyry is 408±9 Ma, representing the age of underlain Lower Devonian volcanic rocks. Thus, the U-Pb dates suggest that the northeastward subduction of Junggar ocean from southwest occurred at 408 to 376 Ma (the real inter- val may be larger). Because the ore-bearing porphyry intruded following the formation of the volcanic rocks of middle Devonian Beitashan Formation, their tec- tonic setting is similar to the Andes Mountains that hosts world-class porphyry copper deposits, and the researched area could be regarded as a potential area for prospecting large porphyry copper deposits.展开更多
基金supported by the National Natural Science Foundation of China(Grant No.40072061)National 305 Project(Grant No.2001BA609A-07-02)+1 种基金Program for New Century Excellent Talents in University(Grant No.NCET-04-0728)"973"Project(Grant No.2001 CB409807).
文摘SHRIMP U-Pb zircon dating on the Xileketehalasu granodiorite porphyry and Kalasayi monodiorite porphyry that intrude middle Devonian Beitashan Formation at the north part of east Junggar region shows that they were formed at 381±6 Ma and 376±10 Ma respectively. They are interpreted as subduction-related granitic rocks, which is the first report that the isotopic ages for the granitic rocks range from 350 to 390 Ma. Another determined age for the Kalasayi monodiorite porphyry is 408±9 Ma, representing the age of underlain Lower Devonian volcanic rocks. Thus, the U-Pb dates suggest that the northeastward subduction of Junggar ocean from southwest occurred at 408 to 376 Ma (the real inter- val may be larger). Because the ore-bearing porphyry intruded following the formation of the volcanic rocks of middle Devonian Beitashan Formation, their tec- tonic setting is similar to the Andes Mountains that hosts world-class porphyry copper deposits, and the researched area could be regarded as a potential area for prospecting large porphyry copper deposits.
