涇陽 的英文怎麼說

中文拼音 [jīngyáng]
涇陽 英文
a surname
  • 涇 : 名詞（涇河） short for the jinghe river
  • 陽 : Ⅰ名詞1 （太陽; 日光） the sun 2 （山的南面; 水的北面） south of a hill or north of a river 3 （中...
  1. Study on culture of streptomyces jingyingensis with coke breeze

    利用粉煤灰培養涇陽鏈黴菌的研究
  2. The main region of landslide in southern yuan of jingyang is concentrated on the zhaitou, miaodian and jiangliu village in recent years. the landslide in southern yuan of jingyang can be divided into three period, 1982 - 1984, 1992 - 1993 and 1996 - 1997

    涇陽南塬塬邊黃土滑坡在空間上集中分佈在寨頭村、廟店村和蔣劉村一帶；在時間上表現為三個活躍期（即： 1982 1984年， 1992 1993年和1996 1997年） 。
  3. Abstract : in this paper, the urgent monitoring process and post - seismic tendency analysis about jingyang earthquake are introduced. the anomalous feature of the short leve lling variations in jingyang station during the earthquake preparation process w as specially studied

    文摘:簡要介紹了涇陽4 . 8級地震應急監測情況及震后地震趨勢分析過程，著重分析了這一地震孕育發生過程中涇陽地震臺短水準異常變化特徵。
  4. Based on the introduction of the regional geological background of southern yuan of jingyang and the physical - mechanical properties of the loess, the following contents including time - spatial distribution characteristics of the loess landslide, formation mechanism, environmental evaluation of yuan edge, economic assessment of hazard losses, stability judgment of the slope and prevention - cure measurements are discussed in this thesis

    本論文在簡述了涇陽南塬區域地質環境和土體物理力學性質的基礎上著重論述了區內黃土滑坡時空分佈特徵、形成原因、塬邊斜坡環境演化過程、災害損失經濟評價、邊坡穩定性區劃以及黃土滑坡災害防治措施等幾個方面的內容。
  5. And the influence of the later is more tension than the former. the economic losses by landslide in southern yuan of jingyang are assessed. the assessment result indicates that the total economic losses including direct economic losses ( 8. 4009 million yuan ) and indirect economic losses ( 2. 119 million yuan ) comes to 10. 5116 million yuan from 1980 to 1998

    涇陽南塬塬邊黃土滑坡是由人為因素和自然因素造成的，前者為誘發因素，它比自然因素的作用更為強烈；涇陽南塬塬邊黃土滑坡災害所造成的經濟損失評價表明， 1980 1998年間，滑坡所造成的經濟損失達1051 . 16萬元。
  6. Its sediment is from the upstream of linjiacun and jinghe river mostly, which is a tributary of the weihe river

    泥沙主要來自支流涇河及林家村站以上地區，徑流主要來自林家村站至成陽站區間流域。
  7. We can reach a conclusion, firstly, the gross water capacity, gross sediment capacity and zhang jia shan station of jing - river and xian yang station of wei - rever increase but deposit ratio of lower wei - river decrease. secondly, the sediment deposit of lower wei - river increase in pace with the crease in of sediment from the two station and the level rising of chen village

    結果表明渭河下游淤積比隨著涇河張家山站和渭河咸陽站的總水量、總沙量和水流量的提高而降低；渭河下游淤積量隨兩站來沙量的增加，陳村水位的抬高而增加。
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