| ²é¿´: 192 | »Ø¸´: 3 | |||
| µ±Ç°Ö÷ÌâÒѾ´æµµ¡£ | |||
andyaoÌú¸Ëľ³æ (ÕýʽдÊÖ)
|
[½»Á÷]
ÇóÖú£ºÒ»¶Î·Òë
|
||
| ½¨Á¢¾ßÓжþ½×¾«¶ÈµÄÅÅÎÛº£ÓòÈýάÓÐÏÞÌå»ý¼ÆËãģʽ£¬³É¹¦Ä£ÄâÁËÄϲ¿»Æº£ÄÏͨÊÐβˮÅŷſڸ½½üº£ÓòÈýάÁ÷³¡¡¢Å¨¶È³¡£»·¢ÏָõØÇøµÄ³±Á÷ÐÔÖÊÊôdzº£Ñذ¶Íù¸´Á÷ÐÎʽ£¬Á÷Ïò»ù±¾Óë°¶Ï߯½ÐУ¬µ«Ì²µØÁ÷Ïò»ù±¾Óë°¶Ïß´¹Ö±£»·¢ÏÖÎÛË®´ÓÀ©É¢Æ÷½øÈ뺣ˮºóÑØÀ©É¢Æ÷³¤¶È·½ÏòµÄÏ¡ÊÍÀ©É¢·¶Î§ºÜС£¬¶ø´¹Ö±ÓÚÀ©É¢Æ÷·½ÏòÎÛȾÓðÁ÷µÄ°Ú¶¯·ù¶ÈÏà¶Ô½Ï´ó£¬±í²ã°Ú·ù±Èµ×²ã¿í500Ã××óÓÒ£¬²¢ÔÚ´¹Ö±·½ÏòÉϳÊÏֵײãŨ¶È¸ß¡¢±í²ãŨ¶Èµ×µÄÌØµã¡£ |
» ²ÂÄãϲ»¶
0860004 Çóµ÷¼Á 309·Ö
ÒѾÓÐ4È˻ظ´
²ÄÁÏÀà284µ÷¼Á
ÒѾÓÐ25È˻ظ´
Ò»Ö¾Ô¸211 0703»¯Ñ§ 346·ÖÇóµ÷¼Á
ÒѾÓÐ5È˻ظ´
¿¼Ñе÷¼Á-²ÄÁÏÀà-284
ÒѾÓÐ17È˻ظ´
280Çóµ÷¼Á
ÒѾÓÐ3È˻ظ´
0703»¯Ñ§Çóµ÷¼Á
ÒѾÓÐ18È˻ظ´
µ÷¼Á
ÒѾÓÐ15È˻ظ´
¸´ÊÔµ÷¼Á£¬Ò»Ö¾Ô¸Ö£ÖÝ´óѧ²ÄÁÏÓ뻯¹¤289·Ö
ÒѾÓÐ16È˻ظ´
349ѧ¿Æ»¯Ñ§045106Çóµ÷¼Á£¬»¯Ñ§Àà¶¼¿ÉÒÔ
ÒѾÓÐ7È˻ظ´
086003µ÷¼ÁÇóÖú
ÒѾÓÐ6È˻ظ´
![]() ![]() |
2Â¥2009-03-31 09:10:16
mayong11
Ìú¸Ëľ³æ (Ö°Òµ×÷¼Ò)
- Ó¦Öú: 4 (Ó×¶ùÔ°)
- ½ð±Ò: 5866.8
- ºì»¨: 21
- Ìû×Ó: 3447
- ÔÚÏß: 189.9Сʱ
- ³æºÅ: 485538
- ×¢²á: 2007-12-27
- ÐÔ±ð: GG
- רҵ: Ò©Îﻯѧ

3Â¥2009-03-31 18:02:57
mayong11
Ìú¸Ëľ³æ (Ö°Òµ×÷¼Ò)
- Ó¦Öú: 4 (Ó×¶ùÔ°)
- ½ð±Ò: 5866.8
- ºì»¨: 21
- Ìû×Ó: 3447
- ÔÚÏß: 189.9Сʱ
- ³æºÅ: 485538
- ×¢²á: 2007-12-27
- ÐÔ±ð: GG
- רҵ: Ò©Îﻯѧ
¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï ¡ï
andyao(½ð±Ò+15,VIP+0):лл£¬ÊǺÜÄѰ¡£¬Ö÷ÒªÎÒÒ²²»ÊÇ×öÕâ¸ö¶«Î÷µÄ£¬ÀϰåµÄÈÎÎñ£¬Ã»°ì·¨°¡ 4-1 10:39
andyao(½ð±Ò+15,VIP+0):лл£¬ÊǺÜÄѰ¡£¬Ö÷ÒªÎÒÒ²²»ÊÇ×öÕâ¸ö¶«Î÷µÄ£¬ÀϰåµÄÈÎÎñ£¬Ã»°ì·¨°¡ 4-1 10:39
|
we have set up the computation model of three-dimensional finite volume of the sewage waters with a second order accuracy, we succeed simulatiing the flow field and concentration field near the end of the sea water discharge of the Nantong City in southern of Yellow Sea ; we found that the trend in the region belong to the reciprocating flow form of shallow water, the basic flow parallel with coastline, but the basic flow of beaches vertical with coastline ; we also found that the sewage which went into sea from the diffuser, was minimal dilution along the direction of the diffuser plume. However the amplitude of swing was relatively large in the vertical direction of the diffuser plume, and the amplitude of swing in surface layer wide 500 meters compared with the one in the bottom, and showed the characteristics of the low surface concentration and the high bottom concentrations in the vertical direction. ºÃÄÑ£¬Äã´Õºõ×Å¿´°É |

4Â¥2009-03-31 18:51:27













»Ø¸´´ËÂ¥