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| 1 | POLYMER CHARGE AND MOLECULAR WEIGHT EFFECTS ON TREATED IRRIGATION FURROW PROCESSES显示文摘Application of 5-10 mg L-1 water soluble anionic polyacrylamide (PAM) to furrow irrigation water during flow advance substantially reduces sediment loss and increases net infiltration. We hypothesized that PAM_s solvated molecular conformation influences its irrigation-management efficacy. The study was conducted in Kimberly, Idaho, on Portneuf silt loam (Durinodic Xeric Haplocalcids), under furrowirrigated beans (Phaseolus vulgaris ) at a 1.5% slope. Polyacrylamides with contrasting molecular weight (anionic; 4-7, 12- 15 and 14-17 MDa, i.e. Mg mol-1 ), charge type (neutral, anionic, cationic), and charge density (8, 19, 35 mol %) were tested in two studies. Inflow rate was 23 L min-1 during furrow advance, and 15 L min-1 for the remaining set. Anionic and neutral PAMs were twice as effective as cationic PAMs for controlling sediment loss in new furrows. The order of effectiveness for overall soilloss control was : anionic >neutral >cationic PAM, and efficacy increased with increasing charge density and/or molecular weight. Net furrow infiltration increased by 14 to 19% when PAM treatment molecular weight was reduced from 17 to 4 MDa. General trends suggested that medium and high charge density anionic and neutral PAM produced the greatest increase in infiltration compared with controls.Compared with untreated furrows, neutral PAM gave the greatest season-long net infiltration gains (5%),while charged PAMs tended to increase net infiltration early in the season on new furrows but decreased infiltration on repeat-irrigated furrows later in the season. | R. D. Lentz(USDA-ARS, Northwest Irrigation and Soils Research Laboratory, Kimberly, ID)R. E. Sojka (Landcare Research, New Zealand, Ltd, Palmerston North, New ZealandNote: The manucript of this paper was received in March 1999, Discussion open until March | 2000 | International Journal of Sediment Research2000，15，1： | 13 |
| 2 | Hyperhomocysteinemia, Oxidative Stress, and Cerebral Vascular Dysfunction显示文摘 | Frank M. Faraci Steven R. Lentz | 2004 | Stroke: Journal of the American Heart Association2004，，2： | 4 |
| 3 | Methods for the development and assessment of atrial fibrillation and heart failure dog models显示文摘与动物的发展报导 Medtronic 经验的目的用为 AF 模型,的为 CHF.Methods 的为 AF 和 microemboli 的高率的踱步为 atrial 纤维性颤动( AF )和长期的心失败( CHF )当模特儿一根 atrial 皮带被纳入 Medtronic 协同作用 neurostimulator ,它被规划在开关责任 cycle.Atrial natnuretic 肽( ANP )在 50 Hz 刺激,大脑 natriuretic 肽( BNP )和N终端职业人员大脑 natriuretic 肽( NT-proBNP )皮脂腺囊瘤;在精选时间 points.For CHF 模型,的 assayed 在 62,400 beads/mL 的 90 m 聚苯乙烯 microspheres 的连续注射( Polybead , Polysciences 公司)被执行导致全球局部缺血,有每周监视的任何一个和 embolization 时间表(集团 1 , n = 25 )或与监视的双周刊和 emboliation 时间表(集团 2 , n36 ) .Echocardiograms 每周与 ventriculograms 和磁性的回声成像扫描一起被使用估计心脏的功能和 ANP , BNP 和 NT-proBNP 是为 AF 模型的 monitored.Results ,为 CHF 模型,遇见 CHF 端点的日子在集团 2 .For 在集团 1 和 89 是 116 AF 和 CHF 模型, NT-proBNP 与在为动物的搜索的研究人员为估计基于设备的治疗的安全和功效建模的我们为 AF 和 CHF 狗模型的发展和评价的经验可以帮助的疾病 states.Conclusion 的发展相关很好。 | Jon F Urban Renee L Gerhart Jason R Krzeszak Corey R Leet Linnea R Lentz Carolyn B McClay | 2011 | Journal of Geriatric Cardiology2011，8，3： | 3 |
| 4 | Effects of text illustrations: A review of research显示文摘 | W. Howard Levie Richard Lentz | 1982 | Educational Communication & Technology1982，，4： | 3 |
| 5 | Classical tidal harmonic analysis including error estimates in MATLAB using T_TIDE显示文摘 | Rich Pawlowicz Bob Beardsley Steve Lentz | 2002 | Computers and Geosciences2002，，8： | 3 |
| 6 | 用MATLAB的T_TIDE程序进行包含误差估计的经典潮汐调和分析 | Rich Pawlowicz Bob Beardsley Steve Lentz 李进武 | 2012 | 地壳构造与地壳应力2012，0，2： | 2 |
| 7 | Mineralogy and geochemistry of Nb-,Ta-,Sn-,U-,Th-,and Zr-bearing granitic rocks from Abu Rusheid shear zones,South Eastern Desert,Egypt显示文摘Granite-hosted,Nb-,Ta-,Sn-,U-,Th-,and Zr(Hf)-bearing mineralization from the Abu Rusheid shear zones occurs about 97 km southwest of the town of Marsa Alam,South Eastern Desert,Egypt.The SSE-trending brittle-ductile Abu Rusheid shear zones crosscut the peralkalic granitic gneisses and cataclastic to mylonitic rocks(mylonite,protomlyonite,and ultramylonite).The northern shear zone varies in width from 1 to 3 m with a strike length of >500 m,and the southern shear zone is 0.5 to 8 m wide and >1 km long.These shear zones locally host less altered lamprophyre and locally sheared granitic aplite-pegmatite dykes.The rare-metal minerals,identified from the peralkalic granitic gneisses and cataclastic to mylonitic rocks are associated with muscovite,chlorite,quartz,fluorite,pyrite,magnetite,and rare biotite that are restricted to the Abu Rusheid shear zones;these are columbite-tantalite and pyrochlore(var.betafite) in the northern shear zone and ferrocolumbite in the southern shear zone.Cassiterite occurs as inclusions in the columbite-tantalite minerals.U-and Th-minerals(uraninite,thorite,uranothorite,ishikawaite,and cheralite) and Hf-rich zircon coexist.Magmatic(?) zircon contains numerous inclusions of rutile,fluorite,U-Th and REE minerals,such as uranothorite,cheralite,monazite,and xenotime.Compositional variations in Ta/(Ta+Nb) and Mn/(Mn+Fe) in columbite range from 0.07-0.42 and 0.04-0.33,respectively,and Hf contents in zircon from 1.92-6.46 of the two mineralized shear zones reflect the extreme degree of magmatic fractionation.Four samples of peralkalic granitic gneisses and cataclastic to mylonitic rocks from the southern shear zone have very low TiO2(0.02 wt%-0.04 wt%),Sr [(15-20)×10-6],and Ba [(47-78)×10-6],with high Fe2O3T(0.94 wt%-1.99 wt%),CaO(0.14 wt%-1.16 wt%),alkalis(9.2 wt%-10.1 wt%),Rb [(369-805)×10-6],Zr [(1033-2261)×10-6],Nb [(371-913)×10-6],U [(51-108)×10-6],Th [(36-110)×10-6],Ta [(38-108)×10-6],Pb [(39-364)×10-6],Zn [(21-424)×10-6],Y [(8-304)×10-6],Hf [(29-157)×10-6],and ∑REE [(64-304)×10-6],especially HREE [(46-167)×10-6].Three samples from the northern shear zone also have very low TiO2(0.03 wt%),Sr [(11-16)×10-6],and Ba [(38-47)×10-6],with high Fe2O3T(1.97 wt%-2.91 wt%),CaO(0.49 wt%-1.01 wt%),alkalis(7.2 wt%-8.3 wt%),Rb [(932-978)×10-6],Zr [(1707-1953)×10-6],Nb [(853-981)×10-6],Ta [(100-112)×10-6],U [(120-752)×10-6],Th [(121-164)×10-6],Pb [(260-2198)×10-6],Zn [(483-1140)×10-6],Y [(8-304)×10-6],Hf [(67-106)×10-6],and ∑REE [(110-231)×10-6],especially HREE [(91-177)×10-6].The very high Rb/Sr(57.5-88.9),and low Zr/Hf(16.9-25.6),Nb/Ta(7.7-9.8),and Th/U(0.21-1.01) are consistent with very frac-tionated fluorine-bearing granitic rocks that were altered and sheared.The field evidence,textural relations,and compositions of the ore minerals suggest that the main mineralizing event was magmatic(629+/-5 Ma,CHIME monazite),with later hydrothermal alteration and local remobilization of the high-field-strength elements. | Ali M.A. Lentz D.R. Hall D.C. | 2011 | Chinese Journal Of Geochemistry2011，30，2： | 2 |
| 8 | Diagnostic and Therapeutic Endoscopy in Children and Adolescents with Cancer显示文摘 | Stephan Buderus Hannah Sonderkö tter Gudrun Fleischhack Michael J. Lentze | 2012 | Pediatric Hematology-Oncology2012，，5： | 2 |
| 9 | Mineralogy, geochemistry and age dating of shear zone-hosted Nb-Ta-, Zr-Hf-, Th-, U-bearing granitic rocks in the Ghadir and El-Sella areas, South Eastern Desert, Egypt显示文摘The rare metal minerals of mineralized altered granites within the Ghadir and El-Sella shear zones, are represented by betafite, U-minerals (uraninite and uranophane), zircon, monazite, xenotime, and rutile in the Ghadir shear zone. While they are columbite-tantalite minerals as ferrocolumbite, pyrochlore, and fergusonite, Th-minerals (cheralite, uranothorite, and huttonite monazite), Hf-zircon, monazite and xenotime in the El-Sella shear zone. Hf-zircon in the El-Sella and Ghadir shear zones (increasing from the core to the rim) contains high inclusions of U-Th, and REE minerals such as cheralite, uranothorite, huttonite monazite and xenotime especially in the El Sella shear zone. The rare-metal minerals, identified from peralkminous granites of the shear zones are associated with muscovite, quartz, chlorite, fluorite, magnetite, and biotite that are restricted to the two shear zones. Uraninite (low Th content) occurring in the Ghadir shear zone indicates the hydrothermal origin, but there are thorite, uranothorite, cheralite, and Hf-zircon in the El Sella shear zone, also indicating the hyrothermal proccess after magmatic origin. Compositional variations of Ta/(Ta+Nb) and Mn/(Mn+Fe) in columbite from 0.07-0.42 and 0.04-0.33, respectively, and Hf contents in zircon are so high as to be 12%, especially in the rim in the El Sella shear zone. This feature re-flects the extreme degree of magmatic fractionation. Four samples from the altered granites of the Ghadir shear zone also are very low in TiO2 (0.04 wt%-0.17 wt%), Sr [(82-121)×10-6], and Ba [(36-380)×10-6], but high in Fe2O3T (0.46 wt%-0.68 wt%), CaO (0.64 wt%-1.23 wt%), alkalis (8.59 wt%-8.88 wt%), Rb [(11-203)×10-6], Zr [(98-121)×10-6], Nb [(9-276)×10-6], Ta [(2-139)×10-6], U [(14-63)×10-6], Th [(16-105)×10-6], Pb [(13-32)×10-6], Zn [(7-8)×10-6], Y [(15-138)×10-6], Hf [(3-9)×10-6], and ∑REE [(81-395)×10-6, especially LREE [(70-322)×10-6]. They are very high in Zr/Hf (15.07-85.96) and Nb/Ta (7.17-21.48), and low in Rb/Sr (2.56-3.36) and Th/U (0.096-3.36). Four samples of the altered granites from the El Sella shear zone are very low in TiO2 (0.23 wt%-0.38 wt%), Sr [(47-933)×10-6], and Ba [(82-175)×10-6] , with high Fe2O3T (1.96 wt%-2.87 wt%), CaO (0.43 wt%-0.6 wt%), alkalis (4.46 wt%-10.7 wt%), Rb [(109-313)×10-6], Zr [(178-1871)×10-6], Nb [(11-404)×10-6], U [(56-182)×10-6], Th [(7-188)×10-6], Ta [(0.5-57)×10-6], Pb [(12-28)×10-6], Zn [(1-13)×10-6], Y [(62-156)×10-6], Hf [(3-124)×10-6], and ∑REE [(101-184)×10-6], especially HREE [(7-139)×10-6]. This is consistent with the very fractionated, fluorine-bearing granitic rocks that were altered and sheared in the El Sella shear zone. Zr/Hf (14.23-39.79) and Nb/Ta (1.98-7.01) are very high, and Rb/Sr (0.14-1.7) and Th/U (0.25-2.5) are low in the Ghadir shear zone. Field evidence, textural relations, and the composi-tion of ore minerals suggest that the main mineralizing event was magmatic (615+/-7 Ma, and 644+/-7 Ma CHIME monazite), especially in the El Sella shear zone, with later hydrothermal alteration and local remobilization of the high-field-strength elements. | Ali M.A. Lentz D.R.2 | 2011 | Chinese Journal Of Geochemistry2011，30，4： | 2 |
| 10 | Does homocysteine promote atherosclerosis 显示文摘 | Lentz SR | 2001 | Arterioscler Thromb Vasc Biol2001，21，9： | 1 |
| 11 | Food/susceptor interface temperatures during microwave heating显示文摘 | LENTZ R R CROSSETT T M | 1988 | Microwave World1988，9，5： | 1 |
| 12 | Cerebral vascular dysfunction during hypercholesterolemia显示文摘 | Kitayama J Faraci MR Lentz SR | 2007 | Stroke2007，38，7： | 1 |
| 13 | Dry Bay Fire Model Enhancements 显示文摘 | Martin L Lentz Andrew Pascal Michael R Weisenbach | 2002 | AIAA PAPER2002 - 14962002，，： | 1 |
| 14 | Pain,psy-chological variables,sleep quality,and natural killercell activity in midlife women with and without fibro-myalgia显示文摘 | LANDIS C A LENTZ M J TSUJI J | 2004 | Brain Behav Immun2004，18，： | 1 |
| 15 | Homocysteine and vascular disfunction 显示文摘 | Lentz SR | 1997 | Rev Life Sci1997，6，： | 1 |
| 16 | Insecticide treatments for tarnished plant bug control and effect on beneficials显示文摘 | LENTZ G L | 1982 | ESA Insecticide and Acaricide Test1982，，： | 1 |
| 17 | Mechanisms of thrombosis in hyperhomocysteinemia显示文摘 | Lentz SR | 1998 | Curr Opin Hematol1998，5，5： | 1 |
| 18 | Receiver behavior in direct steam generation with parabolic troughs显示文摘 | Almanza R Lentz A Jimenez G | 1997 | Solar Energy1997，61，4： | 1 |
| 19 | Mechanisms of homocysteine-induced atherothrombosis 显示文摘 | Lentz SR | 2005 | J Thromb Haemost2005，3，8： | 1 |
| 20 | Outcomes following artificial sphincter implantation after prior unsuccessful male sling显示文摘 | Lentz AC Peterson AC Webster GD | 2012 | J Urol2012，187，6： | 1 |
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