极端暴雨条件下黄土丘陵沟壑区土壤蓄水能力和入渗规律

黄土高原退耕还林还草工程实施后,下垫面环境条件的变化可能对流域水文过程、水文通量、水量平衡以及生态系统产生十分重要的影响。研究极端暴雨条件下剖面土壤蓄水能力和入渗规律,对于阐明流域产汇流过程和影响机制具有重要的科学价值。采用土壤墒情仪对陕北"7·26"特大暴雨事件下黄土丘陵沟壑区草地剖面土壤水分进行了实时动态监测,分析了极端暴雨条件下剖面土壤水分的动态变化和蓄水过程,利用Horton入渗模型模拟了剖面土壤水分湿润锋的运动过程,揭示了极端暴雨条件下剖面土壤水分的入渗规律。结果表明:(1)极端暴雨条件下,黄土丘陵沟壑区坡面草地不同深度层次土壤水分与降雨过程的响应不同,具有层次性和明显的滞后效应,其中,0～140 cm是影响该地区土壤水文过程的关键层次;(2)土壤水分再分配结束时,湿润锋最深深度达140 cm,土壤蓄水量达225.99 mm,较降雨前95.37 mm增加了1.37倍;(3)极端暴雨过程中湿润锋的运动随时间呈对数递减关系,其稳渗速率随容重增加而减小,呈指数函数递减;(4)极端降雨过程中该地区坡面草地的产流机制仍以超渗产流为主,对于揭示流域的产汇流机制和完善水文预报模型具有重要的科学意义。     

2013年夏季内蒙古干旱-半干旱区两次极端降水事件对比

2013年夏季,内蒙古中西部干旱-半干旱区多次出现极端降水事件,引发气象灾害.为探寻其特征及成因,选择“6·30”、“7·14”两次典型极端降水事件,从天气尺度系统、中尺度对流系统、热力动力条件、水汽来源等方面进行对比分析,得到以下结论:①“6 · 30”暴雨是华北小高压前的切变线产生;“7·14”暴雨是“北槽南涡”与台风北上共同作用的结果.②两次暴雨都是中尺度对流复合体(MCS)发展的结果.“6·30”暴雨突发性强,具有局地特点;“7·14”暴雨具有列车效应,持续时间长.③两次暴雨水汽来源不同.“6·30”暴雨水汽来源于南海;“7.14”暴雨是“北槽南涡”加上远距离台风输送的结果.④“6·30”暴雨是高压切变线西侧干、东侧湿,在锋区附近产生上升运动促发不稳定能量释放;高空“干侵入”是“7·14”暴雨的促发机制.⑤东亚夏季风偏强,西北太平洋副热带高压脊线位置偏北,是内蒙古中西部干旱-半干旱区极端降水事件的重要原因.     

基于回购契约的风险厌恶零售商的供应链协调

应用LSTAR模型对我国通货膨胀率的动态特征进行的实证研究结果表明：我国通货膨胀率自身调整有明显的非线性特征，分为显著的低通货膨胀区制和高通货膨胀区制，区制转移的平滑参数较大，转移变量为滞后1期通货膨胀率，转折点为0.01036。同时，我国通货膨胀率存在一定程度的非对称性调整，随冲击大小、方向、区制不同而表现不同。此外，我国通货膨胀率具有较高的持久性，高通货膨胀区制的持久性明显低于低通货膨胀区制。     

Nucleotide sequence homology to bovine viral diarrhea virus 2 (BVDV 2) in the 5′ untranslated region of BVDVs from cattle with mucosal disease or persistent infection in Japan

Cytopathogenic and non-cytopathogenic bovine viral diarrhea viruses (BVDVs) were isolated from cattle with mucosal disease or persistent infection in Japan. These isolates were compared for antigenic properties by cross-neutralization tests with Japanese reference strains of BVDV belonging to classical type 1. Significantly low cross-reactivity to reference strains was noted, indicating the viruses to possibly represent a new serotype in Japan. Thus, to determine the genotype of the isolates, nucleotide sequences of the 5′ untranslated region were determined and compared with those of previously reported BVDV 1 and 2. The isolates were clearly shown to belong to BVDV 2, not to BVDV 1.     

Treatment of Intraoperative Persistent Penile Erection in a Stallion

This case report describes the occurrence of persistent penile erection in a breeding stallion that occurred while the horse was under inhalant anesthesia for a carpal arthroscopy. The horse had no history of breeding problems, and no abnormalities were detected on physical examination, complete blood count, or serum chemistry tests performed prior to surgery. Anesthesia was induced with guaifenesin and ketamine after sedation with xylazine and was maintained with isoflurane in 100% oxygen. Penile erection developed approximately 35 minutes after induction and persisted for over 2 hours despite various physical and pharmacological attempts to alleviate it (massage, cold compresses, intravenous benztropine administration, and intracavernosal phenylephrine). Successful resolution of the erection was obtained by cannulation and drainage of blood from the corpus cavernosum and subsequent irrigation with heparinized sterile saline and infusion of phenylephrine in the corpus cavernosum. The detumescent penis was placed back into the sheath, and purse string sutures were placed in the sheath to ensure the penis would remain inside the sheath during recovery. The stallion's recovery from anesthesia was uneventful, the sutures were removed, and the horse was fitted with a penile sling to prevent additional edema or trauma. The stallion recovered completely from the persistent penile erection. Semen was collected 6 days after the event, and he returned to normal pasture breeding 6 weeks after surgery.     

Diagnostic imaging and pacemaker implantation in a domestic goat with persistent left cranial vena cava

Difficulty was encountered with the insertion of a right atrial pacing lead via the left jugular vein during lead and pacemaker implantation in a clinically normal goat as part of an ongoing rapid atrial pacing – induced atrial fibrillation research project. Fluoroscopic visualization of an abnormal lead advancement path prompted angiographic assessment which revealed a persistent left cranial vena cava (PLCVC) and prominent coronary sinus communicating with the right atrium. Angiography facilitated successful advancement and securing of the pacing lead into the right side of the interatrial septum. Cardiac magnetic resonance imaging/magnetic resonance angiography (MRI/MRA) allowed further characterization of this rare venous anomaly. Even though PLCVC has been reported once in a goat, to the authors' knowledge this is the first report to include MRI/MRA characterization of PLCVC and prominent coronary sinus with successful cardiac pacemaker implantation using the PLCVC.     

黄丘区小流域暴雨径流动力特征对淤地坝配置的响应

为定量揭示淤地坝措施配置对黄丘区小流域暴雨径流形成及演进过程的影响,采用室内小流域人工模拟降雨试验,对不同淤地坝措施布设情景下（无坝、单坝、双坝）小流域不同断面径流的水动力、侵蚀动力特征进行研究。结果表明：径流量与含沙量整体均随时间推移而增大,无淤地坝布设情景下径流量增幅为114.60 cm3/s,双坝情景的径流量增幅仅有70.11 cm3/s;淤地坝对小流域暴雨径流演进过程的影响显著,淤地坝布设后径流流态由主要的紊流-缓流变为以层流-缓流为主,雷诺数Re减小幅度达到12.04%～85.85%;动力参数中径流功率ω和雷诺数Re可以被认为是能够较好描述不同淤地坝布设下侵蚀产沙的动力因子。研究结果对于揭示流域暴雨径流过程及成灾机理具有重要现实意义,可为科学评价水土保持措施调控径流过程的效应提供理论依据。     

2012年7月我国中东部持续性强降水形成机制分析

利用NCEP/NCAR再分析资料,通过对2012年7月中旬我国中东部地区持续性强降水过程中东亚夏季风系统中主要成员的时空变化特征进行分析.结果表明,此次持续性强降水期间,副高北界、南亚高压脊线及中纬度锋区位置相对稳定,长江中下游地区一直处于南亚高压反气旋环流东侧偏北风与西风槽前偏南风之间的风向开口辐散区中;副高南撤时,强降水主要位于584 dagpm线北侧,副高北抬时,强降水主要位于584 dagpm线南侧;此次持续性强降水发生前期,大气为上干下湿不稳定层结,当西风带低槽频频携带冷空气南下影响,同时低空西南急流反复加强,其出口区左侧较强的风速梯度为暴雨的发生发展提供了动力条件;低层干空气的不断侵入,低槽和低涡间的垂直正反环流促使垂直上升运动维持或发展,进而造成持续性强降水;高空西风急流加强(减弱)超前低空西南急流加强(减弱)2～5 d,对持续性强降水有超前指示意义.     

黄河中游水利水保措施减沙效益分析中几个值得注意的问题

河流输沙量的变化受流域降水和下垫面影响很大。采用水文法分析水利水保措施减沙效益时应注意如下问题:降雨量是最重要的基础资料,要认真分析工程实施前后雨量站的分布、代表性及前后期降雨量的可比性;暴雨对产沙的影响很大,暴雨强度是决定产沙量多少的重要参数,选用有效降雨量、有效降雨强度能较好地反映暴雨产沙作用;用径流量预报产沙量要区别地下、地表径流的不同影响;要考虑不同地貌类型区对产沙量的影响。     

青海省玉树州高原暴雨型泥石流形成机制——以称多县拉隆沟泥石流为例

[目的]对青海省玉树州高原暴雨型泥石流形成机制进行研究,旨在为此类泥石流灾害防治及风险减缓提供依据。[方法]以青海省玉树州称多县拉隆沟暴雨型泥石流为例,通过实地调查对其形成因素及形成机制进行研究。[结果]该泥石流主沟道长约3km,流域面积5.25km~2,纵坡比降212‰,高差约600m。物源区发育滑坡方量约为6.50×104 m~3,流域内冲出泥石流物质共约8.5×104 m~3,沟道内物源补给量2.0×104 m~3。[结论]青海省玉树州高原暴雨型泥石流的启动模式可总结为:滑坡—物源形成—固体物质起动—沟道侵蚀—泥石流形成。