| 1. | Study on river patterns of the tarim river
塔里木河干流河道的河型及其成因 |
| 2. | Research on the river pattern change and control of the xiajingjiang river
下荆江河势演变与河势控制研究 |
| 3. | Discussion on river pattern variation of the fenhe river ' s section of entering the yellow river
浅议汾河入黄段河势变迁及影响 |
| 4. | River pattern transformation of wondering river section in the lower reaches of the yellow river
黄河下游游荡性河道的河型转化 |
| 5. | ( 5 ) the theory of dissipative structure is used to explain the change of the river patterns
（ 5 ）应用耗散结构理论解释了河型转化。 |
| 6. | Research on engineering geology of river pattern control in the middle and lower reaches of the yangtze river
论长江中下游河势控制工程的地质研究 |
| 7. | The tendency of river pattern variation in the lower jingjiang river after completion of the three gorges project
三峡水库建成后下荆江河型变化趋势的研究 |
| 8. | Comparison of formation model and channel stability between two different sorts of multiple channel river patterns
两类多河道河流的形成模式及河道稳定性比较 |
| 9. | Abstract : by analyzing the changes of incoming water and sediment in the lower weihe river , in allusion to the question of flood discharge capacity being not enough , control project being short , river pattern can ? t being controlled and the management being loose etc , advise to increase the investment , consummate the measures of flood prevention engineering and non - engineering . strengthen the management , consolidate the consciousness of flood prevention and disaster alleviation , in order to raise recent ability of flood prevention in the lower weihe river
文摘:通过对渭河下游来水来沙变化的分析，针对现状堤防过洪能力不足、控导工程少、河势得不到控制和管理工程等方面存在的问题，提出应加大投入力度，完善防洪工程措施和非工程措施，加强管理，强化防洪减灾意识，提高近期渭河下游防洪能力。 |
| 10. | From ocm layer to 30cm layer , the first rotated loading vector field in every layer reflects the anomalous soil humidity pattern in huai river basin , we call the pattern structure as " huai river pattern " . while from 30cm layer to 50cm layer , the second rotated loading vector field in every layer is also quite similar to " huai river pattern " . in the summer and autumn the " huai river pattern " is still remarkable but the feature is less prominent than that in the springtime
发现春季以30cm为界， 30cm以上各层土壤湿度异常的第一旋转空间模态十分相似，其大值中心主要位于淮河流域，而30cm以下( 30 - 50cm )各层的第二旋转空间模态与之亦十分类似，因此称该模态为“淮河型” ，而夏季和秋季虽然该模态也很显著但特征不如春季突出。 |
