有負面記錄后,個人可以采取哪些措施修復自己的信用記錄? - 行測知識

有負面記錄后,個人可以采取哪些措施修復自己的信用記錄?減小字體增大字體有負面記錄后,個人可以采取哪些措施修復自己的信用記錄?

答:個人應(yīng)當在日常生活中注意養(yǎng)成良好的意識和習慣,從根本上避免因出現(xiàn)負面記錄而給自己造成的不利影響。首先是注意養(yǎng)成良好的消費習慣和還款習慣,對于日常消費、貸款和各類繳費,要注意還款期限,避免出現(xiàn)逾期,以誠為本,恪守信用,樹立良好的信用意識。其次是妥善安排有關(guān)信貸活動,并做好關(guān)聯(lián)預警提示。選擇合適的還款方式,采取有效的提醒措施,確保每筆貸款和信用卡按時還款。

如果目前自己的信用報告中存在負面記錄,那么首先是要避免出現(xiàn)新的負面記錄,其次是盡快重新建立個人的守信記錄。商業(yè)銀行等金融機構(gòu)在判斷一個人的信用狀況時,著重考察的是這個人最近的信貸交易情況。如果一個人偶爾出現(xiàn)了逾期還款,但此后都是按時、足額還款,這足以證明其信用狀況正在向好的方向發(fā)展。

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解放軍文職招聘考試會議記錄-解放軍文職人員招聘-軍隊文職考試-紅師教育

發(fā)布時間:2017-09-20 22:52:12會議記錄 是在會議中記錄人員把會議的基本情況(時間、地點、出席人員、主持者、討論的主要問題等),研究和討論的問題,報告、發(fā)言的內(nèi)容,形成的決議等如實記錄下來成為書面材料的一種文書。會議記錄的結(jié)構(gòu)包括會議基本情況、會議內(nèi)容和結(jié)尾三部分組成。會議基本情況包括標題(開會單位、會議名稱、文體)和會議組織情況。會議組織情況包括開會時間、地點、主持人、記錄人、出席人(出席人少的要寫明姓名、職務(wù);出席人多時 可寫出這些人的級別及人數(shù)。重要的級別較高的會議可設(shè)簽到簿),要求寫上姓名、注明職務(wù),列席人、缺席人(寫明姓名、職務(wù)及事由)。會議內(nèi)容包括會議研究、討論的問題,領(lǐng)導報告(有書面材料的可不記),發(fā)言、討論的情況(按發(fā)言先后順序記錄),決議事項、工作安排(如有通過表決的決定,在記錄決定條款時還要記下贊成票、反對票、棄權(quán)票的數(shù)目),遺留問題等。結(jié)尾換行空兩格寫上 散會 。末尾右下方由主持人、記錄者簽名。例文:全縣林業(yè)工作大會時間: 年 月 日地點:通道縣林業(yè)局六樓會議室出席人員:分管林業(yè)副縣長 ,局所有領(lǐng)導,各鄉(xiāng)鎮(zhèn)分管林業(yè)領(lǐng)導,各基層林業(yè)站站長、木材檢查站站長及局機關(guān)全體。(詳見簽到單)缺席人員: (事由), (事由)主持人:記錄人:議題:布置林權(quán)換發(fā)證工作任務(wù)一、 副縣長作題為《 》的工作報告。二、 副局長就換發(fā)證工作的相關(guān)要求及各鄉(xiāng)鎮(zhèn)的任務(wù)作說明。1、2、3、三、 局長對下一階段工作重點作布置:1、加強領(lǐng)導,按時完成林權(quán)換發(fā)證工作任務(wù)。2、及時完成秋季造林驗收,特別是退耕還林小班的復查。3、按時搞好今冬明春造林小班摸底并及時上報造林規(guī)劃設(shè)計。4、(略)5、(略)散會主持人:(簽名)記錄人:(簽名)

解放軍文職招聘考試實驗記錄、報告的基本要求-解放軍文職人員招聘-軍隊文職考試-紅師教育

發(fā)布時間:2017-08-24 14:07:04學生在本課程開始時,必須認真地閱讀本書第一部分有機化學實驗的一般知識。在進行每個實驗時,必須做好預習、實驗記錄和實驗報告。一、預習為了使實驗能夠達到預期的效果,在實驗之前要做好充分的預習和準備,預習時除了要求反復閱讀實驗內(nèi)容,領(lǐng)會實驗原理,了解有關(guān)實驗步驟和注意事項外,還需在實驗記錄本上寫好預習提綱。以制備實驗為例預習提綱包括以下內(nèi)容:(1)實驗目的:(2)主反應(yīng)和重要副反應(yīng)的反應(yīng)方程式;(3)原料、產(chǎn)物和副產(chǎn)物的物理常數(shù);原料用量(單位:g,mL,mol),計算理論產(chǎn)量;(4)正確而清楚地畫出裝置圖:(5)用圖表形式表示實驗步驟。二、實驗記錄實驗記錄本應(yīng)是一裝釘本,不得用活頁紙或散紙。記錄本按照下列格式做實驗記錄:(1)空出記錄本頭幾頁,留作編目用:(2)把記錄本編好頁碼:(3)每做一個實驗,應(yīng)從新的一頁開始:(4)若你對實驗操作沒有變動時,不必再把操作細節(jié)記上。但應(yīng)記錄:試劑的規(guī)格和用量,儀器的名稱、規(guī)格、牌號,實驗的日期,實驗所用去的時間,實驗現(xiàn)象和數(shù)據(jù)。對于觀察的現(xiàn)象應(yīng)忠實地詳盡地記錄,不能虛假。判斷記錄本內(nèi)容的標準,是記錄必須完整,且組織得好和清楚,不僅自己現(xiàn)在能看懂,甚至幾年后也能看懂,而且還使他人能看得明白。如漏記了主要內(nèi)容,就將難于補救了。實驗記錄

解放軍文職招聘考試Recording an earthquake 記錄地震-解放軍文職人員招聘-軍隊文職考試-紅師教育

發(fā)布時間:2017-06-30 23:53:58An earthquake comes like a thief in the night, without warning. It was necessary, therefore, to invent instruments that neither slumbered nor slept. Some devices were quite simple. One, for instance, consisted of rods of various lengths and thicknesses with would stand up end like ninepins. When a shock came, it shook the rigid table upon which these stood. If it were gentle, only the more unstable rods fell. If it were severe, they all fell. Thus the rods, by falling, and by the direction in which they fell, recorded for the severe, they all fell. Thus the rods, by falling, and by the direction in which they fell, recorded for the slumbering scientist the strength of a shock that was too weak to waken him, and the direction from which it came.But instruments far more deliecate than that were needed if any really serious advance was to be made. The ideal to be aimed at was to devise an instrument that could record with a pen on paper, the movements of the ground or of the table as the quake passed by. While I write my pen moves, but the paper keeps still. With practice, no doubt, I could in time learn to write by holding the pen still while the paper moved. That sounds a silly suggestion, but that was precisely the idea adopted in some of the early instruments (seismometers) for recording earthquake waves. But when table, penholder and paper are all moving, how is it possible to write legibly? The key to a solution of that problem lay in an everyday observation. Why does a person standing in a bus or train tend to fall when a sudden start is made? It is because his feet move on , but his head stays still. A simple experiment will help us a little further. Tie a heavy weight at the end of a long piece of string. With the hand to and fro and around but not up and string so that the weight nearly touches the ground. Now move the hand to and fro and around but not up and down. It will be found that the weight a piece of string. With the hand held high in the air, hold the string so that the weight nearly touches the ground. Now move the hand to and fro and around but not up and down. It will be found that ten weight moves but slightly or not at all. Imagine an earthquake shock shaking the floor, the paper, you and your hand. In the midst of all this movement, the weight and the pen would be still. But as the paper moved from side to side under the pen point, its movement would be recorded in ink upon its surface. It was upon this principle that the first instruments were made, but while the drum was being shaken, the line that the pen was drawing wriggled from side to side. The apparatus thus described, however, records only the horizontal component of the wave movement, which is, in fact, much more complicated. If we could actually see the path described by a particle, such as a sand grain in the rock, it would be more like that of a bluebottle path described by a particle, such as a sand grain in the rock, it would be more like that of a bluebottle buzzing round the room; it would be up and down, to and fro and from side to side. Instruments have been devised and can be so placed that all three elements can be recorded in different graphs.When the instrument is situated at more than 700 miles from the earthquake centre, the graphic record shows three waves arriving one after at short intervals. The first records the arrival of longitudinal vibrations. The second marks the arrival of transverse vibrations which travel more slowly and arrive several minutes after the first. These two have travelled through the earth. It was from the study of these that so much was learnt about the interior of the earth. The third, or main. The third, or main wave, is the slowest and has travelled round the earth through the surface rocks.參考譯文地震就像夜間的小偷,不打招呼就來了。因此,有必要發(fā)明一種儀器,既不打盹兒,也不睡覺。有些裝置非常簡單。例如,有一種裝置是由一些長短、粗細不同的木棒組成,就像九柱戲的木棒一樣堅立著,一旦有地震,就會震動豎立在堅硬的桌上的木棒。如果地震輕微,只有不穩(wěn)定的木棒倒下;如果地震劇烈,所有的木棒都會例下。由于地震太弱而未驚醒科學家時,木棒倒下的多少和倒下的方向就為科學家記錄下了地震的強度和地震方向。但是,如果要取得真正重大的進展,需要有比這種裝置精細得多的儀器。理想的目標是設(shè)計出這樣一種儀器:當?shù)卣鸢l(fā)生時,它能用筆在紙上記錄下大地和桌子運動情況。我寫字時,筆是移動的,紙是靜止的。毫無疑問,經(jīng)過練習,我最終能夠?qū)W會筆不動而紙動來寫字。這聽起來似乎是一種愚蠢的想法,但是早期記錄地震波的儀器(地震儀)正是采用了這中思路??墒?,當桌子、夾筆裝置、紙都在移動時,怎么能書寫得清楚呢?可以從我們的日常生活觀察中找到這個問題的答案。一個站在公共汽車或火車上,當車突然開動時,他為什么會傾倒呢?這是因為他的腳動了,而他的頭保持著靜止。再做一個簡單的實驗可以幫助我們進一步理解這個問題。把一個生物拴在一根長繩子的一端,把手高高舉在空中握住繩子,讓重物幾乎接觸地面。然后把手前后左右以及旋轉(zhuǎn)擺動,但不要上下擺動。結(jié)果會發(fā)現(xiàn),重物是動了,但動得很小,甚至沒動。假定把一支筆拴在重物上,筆尖落在地板上的一張紙上,假定地震發(fā)生了,地板、紙、你和你的手都會動,重物和筆卻不動。由于紙在筆下來回運動,紙的表面就會用墨水記錄下地板運動的情況。根據(jù)這一原理,制造出了最初的地震儀器,但是紙是卷在慢慢放置的圓筒上的。只要一切都是靜止的,筆就會劃出一條直線;但是,圓筒受到震動,筆所畫出的線就會就會左右擺動。然而,這里所說的儀器記錄下來的只是地震波運動中的水平部份,地震波的運動實際比這要復雜得多。假如我們真能看到諸如巖石中一個沙粒子的運動軌跡,那就像一只嗡嗡叫的綠頭蒼蠅在屋內(nèi)飛行的軌跡,呈現(xiàn)出上上下下、來來回回、左左右右3種性質(zhì)的運動。已經(jīng)設(shè)計出了一些儀器,它按照一定的安放方式就可測繪出這三種運動的曲線圖。如果把這種儀器安裝在距震源700多英里遠的地方,曲線記錄就能顯示出前后相同的這3種地震波。首先記錄下的是縱向波的到達;然后記錄下的是橫向波的到達,橫向波比縱向波傳播得慢,在縱向波到過幾分鐘后能到達。這珍兩種波都是穿過地球而來的。正是從這兩種波中的研究中,我們可以了解到地球內(nèi)部的許多情況。第三種波,即主波,是最慢的,是圍繞地球通過表面巖石傳來的。