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1)  flow intensity
水流强度
1.
After analysising various measures of flow intensity, it is found that it can be expressed as a generalized form which can be transformed to existing flow intensity by assuming different coefficient and exponents.
在对以往各种水流强度指标进行综合、归纳的基础上,提出了水流强度指标的一般形式,由此推导出通用推移质输沙率公式。
2)  turbulence intensity of flow
水流紊动强度
3)  flow intensity
水流强度指标
1.
Sediment transport and flow intensity indexes;
泥沙输移与水流强度指标
2.
The precision of the sediment transport equations is mostly determined by the selection of flow intensity parameter.
 输沙强度计算公式的精度,在很大程度上取决于水流强度指标的选取。
3.
In fact, the calculation of sediment transport intensity is to set up a relationship between sediment transprot rate and flow intensity parameter.
输沙强度的计算 ,其实质是建立输沙率与水流强度间的关系 ,而现有的输沙公式中所采用的水流强度指标千差万别。
4)  water and soil losses
水土流失强度
1.
Utilizing observed data and analytical methods of time domain and frequency domain in periodic autoregressive model AR(2),the water and soil losses intensities of major observation stations or points in Gansu Province are forecasted The two kinds of forcasting results are analyzed optimally It shows that the results of analytical method of frequency domain are more close to the observed dat
利用实测资料 ,运用周期性自回归模型AR(2 )的时域和频域分析法 ,分别对甘肃省各主要观测站点的水土流失强度 (土壤侵蚀模数 )进行了预测 ,并对两种预测结果进行优化分析 分析结果表明 ,频域分析法预测的结果更接近实测
5)  dimensionless flow intensity
无量纲水流强度
6)  urban soil and water loss intensity
城市水土流失强度
1.
Applied regions of gradation index for traditional soil and water loss intensity and limitations of gradation index for urban soil and water loss intensity in Shenzhen city were generally expounded.
概述了传统水土流失强度分级指标的适用范围及深圳市城市水土流失强度分级指标的局限性。
补充资料:表光合强度(见光合强度)


表光合强度(见光合强度)
forecast of sowing or transplanting time

b iaoguanghe qiangdu表光合强度见光合强度
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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