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maximum flood in Chinese

Pronunciation:
How to pronounce "maximum flood""maximum flood" in a sentence

Translationmobile phoneMobile

  • 最大洪水
  • 最大漲潮流速

Examples

  • And a scaling lognormal model of flood volume is introduced to represent the affection of temporal scale of duration in annual maximum flood volume distributions
    并提出了洪水洪量的對數(shù)正態(tài)分布模型來表征年最大洪量分布中歷時的尺度影響。
  • The maximum flood surface is the turn - point of the rising and falling of the baselevel . once these two surfaces are defined , a intergrated sequence can be classificated . the principle of this area ' s sequence classfication is using seismic data to classificate the third - sequences
    2 、首次將高分辨率層序地層學(xué)的基本理論應(yīng)用于研究區(qū)，在分析巖芯、測井資料及三維地震資料基礎(chǔ)上建立了層序地層等時格架。
  • It is most important to define the sequence boundary and the maximum flood surface for sequence classification . sequence boundary is the turn - point of the falling and rising of the baselevel . the maximum flood surface is the turn - point of the rising and falling of the baselevel
    層序的劃分最重要是確定層序界面和最大洪泛面，層序界面為基準面下降和上升的轉(zhuǎn)折點，而最大洪泛面是基準面上升到下降的轉(zhuǎn)折點，這兩個面一旦確定，就可以劃分一個相對完整的層序。
  • Linnan sub - depression which is mesozoic and cenozoic faulted lacustrine basin is located in the southwestern part of huimin sag , depression of jiyang . it is dominated by lacustrine - fill sub - depression . based on well logs , three - dimension seismic profiles , cores and other basic data , 10 horizons including 6 turnaround surfaces and 4 maximum flooding surfaces are defined from es3 to the lower part of es2 formation , and 1 long - term and 5 intermediate - term base - level cycles which are named from c5 to c1 could be identified , and then the chronostratigraphic framework of the sub - depression is built
    本文以巖心、鉆井、測井、地震資料為基礎(chǔ)，在下第三系沙三段沙二下的一個長期基準面旋回(二級層序)內(nèi)部識別出10個有時間地層對比意義的界面，包括6個基準面下降到上升的轉(zhuǎn)換面(層序界面) ， 4個基準面上升到下降的轉(zhuǎn)換面(湖泛面) ，劃分出c1 - c5五個中期基準面旋回，建立了等時地層格架地層格架。
  • So a new method ? scale analysis method ( or called fractal analysis method ) is applied to study the flood of jialing river basin . the scaling hypotheses is applied to the relationship of annual maximum flood and drainage area . and basing on the scaling lognormal model with two parameters introduced by smith , a lognormal model with three parameters of flood is introduced to represent the scale effect of drainage area in annual flood peak distributions
    在洪水區(qū)域分析中一般采用洪水指標法，但該法的基本假定與實際情況存在矛盾，因此本文采用一種新的分析方法? ?標度分析法(或稱為分形分析法)來研究洪峰的區(qū)域變化，將標度不變性引入年最大洪峰流量? ?匯流面積關(guān)系中，并將其用于嘉陵江流域的洪水，另外，本文在smith提出的具有標度性質(zhì)的二參數(shù)對數(shù)正態(tài)分布模型基礎(chǔ)上創(chuàng)造性地提出了三參數(shù)對數(shù)正態(tài)分布模型來表征年最大洪峰流量分布中匯流面積的尺度影響。

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