右正則環 的英文怎麼說
中文拼音 [yòuzhēngzéhuán]
右正則環
英文
right regular ring-
2 ) let r is a semiprime ring, if r is a left sf - ring whose every special right annihilator is w - ideal, then r is a strongly regular ring
2 )設r是半素環,如果r是左sf -環且r的每個特殊右零化子是w -理想,則r是強正則環。In the fourth chapter, we study the strong regularity of left sf - rings whose every nonzero one - sided ideal contains nonzero weak ideal and every special annihilator is weak ideal, and we prove the following results : l ) strong left ( right ) weakly bounded left sf - rings are strongly regular rings
第四章,主要研究每個非零的單邊理想包含非零的弱理想的左sf -環以及每個特殊零化子是弱理想的左sf -環的強正則性。證明了: 1 )強左(右)弱有界的左sf -環是強正則環。The first chapter, main instead " duo - ring " condition of " every maximal left ideal is gw - ideal " condition, study strongly regularities of gp - v - ring on this condition. lt is shown that ( 1 ) r is strongly regular iff r is left gp - v - ring whose maximal left ideals are gw - ideal. ( 2 ) r is strongly regular iff r is left gp - v - ring whose maximal right ideals are gw - ideal. the second chapter, generalize some results of gp - v - ring to gp - v - ring, discuss regularity of gp - v ' - ring. it is shown that ( 1 ) r is left self - injective regular with non - zero socle iff r is left gp - v - ring with soc ( rr ) = soc ( rr ) and r contains an injective maximal left ideal
第一章主要將「 duo -環」條件替換成「每一極大左(右)理想是gw -理想」條件,研究在此條件下, gp - v -環的強正則性,證明了: ( 1 ) r是強正則環當且僅當r是左gp - v -環且r的每一極大左理想是廣義弱理想; ( 2 ) r是強正則環當且僅當r是左gp - v -環且r的每一極大右理想是廣義弱理想,第二章,主要將gp - v -環上一些結果推廣到gp - v -環上,討論gp - v -環的正則性,證明了: ( 1 ) r是左自內射正則環且soc ( _ rr ) 0當且僅當r是包含內射極大左理想的gp - v -環,且soc ( _ rr ) = soc ( r _ r ) ; ( 2 ) r是正則環且每一極大本質左理想是理想當且僅當r是左gp -內射的左gp - v -環且每一極大本質左理想是理想。Its interannual variation ' s main period is about 4 ~ 5a and the 7 ~ 8a ' s period exist too ; the interdecadal variation ' s main period of the australian high is about 15a. the interannual variation of australian high ( aah ) has correct correlation with antarctic oscillation and enso, and the enso ' s 4a period has the most important influence on the aah. ( 2 ) when the ah becomes stronger, the members of the whole aamcs are stronger following it. that is to say, in the years that the ah is stronger ( compared to the weak years of ah ) and on the horizontal circulation, the members of aamcs, including the ah, the cross - equator flow ( cef ) between 100 and 160 e, the south china sea south - west monsoom ( ssm ), the south sea monsoon rough, the tropical easily flow, subtropical high ( sh ), the mei - yu front, the mid - latitude effect, become stronger, and their positions are more southward ; in the meridional - right circulation, there are five circulations including classic monsoon meridional - cirle circulation and hadley circulation that become stronger in the strong years of ah than in the weak years of ah
本文採用ncep ncar再分析月平均的全球海平面氣壓場、高度場、海表溫度場、高雲量和cmap全球降水資料,以及中國160站逐月降水資料,分析了1948 2002年期間澳大利亞高壓(以下簡稱澳高)的年際和年代際變化以及澳高年際變化對亞澳季風環流系統的影響,結果顯示: ( 1 )澳高存在明顯的年際和年代際變化,澳高年際變化以4 5年的周期變化為主,同時兼有7 8年左右的周期,而澳高的年代際變化則以15年左右的周期變化為主:澳高年際變化同時與南極濤動和enso有正相關,並且enso的4年左右的周期變化對澳高年際變化影響最大。Theorem 3. 3 s is a " d - idempotent semiring, then s is an additive normal idempotent semiring, if and only if s is a pseudo - strong right normal idempotent semiring of left zero semirings
3s是d一冪等半環,則s為加法正規冪等半環,當且僅當s是左零半環的偽強右正規冪等半環The precipitation character of the middle part of viet nam and its relation to the atmospheric circle. the autumn precipitation of the middle part of viet nam has obvious variations in inter - annual and inter - decade scale with clearly quasi 6a, 10a, 15a period ; in heavy rainfall years, there are a positive anomaly over the north - west pacific and a negative anomaly over japan ; while in deficient rainfall years, the anomaly distribution is on the contrary ; 4. the precipitation character of the south part of viet nam and its relation to the atmospheric circle. the research finds that the rainfall of the south part of vietnam usually concentrates in the autumn every year and a clear difference of atmosphere condition exists between that of flood and drought years
越南中部降水變化特徵及其與大氣環流和海溫的關系越南中部秋季降水具有明顯的年際、年代際變化特徵,具有明顯的準6a 、 10a 、 15a左右的周期;越南中部多雨年, 500hpa高度距平場在熱帶西北太平洋為正距平,日本附近上空為負距平;而少雨年則相反;越南中部多雨年,熱帶中東太平洋海溫異常偏高,西太平洋海溫異常偏低;少雨年則相反;越南中部多雨年,登陸越南的臺風頻數偏多;而少雨年則相反。分享友人