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| 1 | 四川紫色土区土壤养分径流和泥沙流失特征研究显示文摘对四川紫色土区土壤养分径流和泥沙流失特征进行了研究 ,结果表明 :土壤氮素主要随径流流失 ,主要土内径流和地下径流携带NO3 N所造成 ;土壤磷主要随泥沙流失 ,泥沙中的养分有明显的富集现象 ,但不同流域以及不同雨次的富集系数明显不同 ;同时泥沙N、P的富集系数与泥沙浓度有一定的关联 ,一般是泥沙浓度高 ,N富集系数低 。 | 李宪文 史学正 Coen Ritsema | 2002 | 资源科学2002，24，6： | 24 |
| 2 | Analytical product study of medicine by different ICP-MS applications 显示文摘 | Krystek P Ritsema R | 2004 | Journal of Trace Elements in Medicine and Biology2004，18，1： | 1 |
| 3 | GIS and Models of Accessibility Potential:An Application in Planning显示文摘 | Ritsema Van Eck J R | 1995 | International Journal of Geographical Information Systems1995，9，1： | 1 |
| 4 | GIS and mod- els of accessibility potential An application in planning显示文摘 | GEERTMAN S C M RITSEMA VAN ECK J R | 1995 | In ternational Journal of Geographical Information Systems1995，9，1： | 1 |
| 5 | The spatial con-figuration of airline networks in Europe显示文摘 | Burghouwt G Hakfoort J Ritsema Van Eck J | 2003 | Journal of Air Trans-port Management2003，9，5： | 1 |
| 6 | Ethylene modulates the role of NONEXPRESSOR OF PATHOGENESIS-RELATED GENES1 in cross talk between salicylate and jasmonate signaling显示文摘 | LEON-REYES A SPOEL S H DE LANGE E S ABE H KOBAYASHI M TSUDA S MILLENAAR F F WELSCHEN R A M RITSEMA T PIETERSE C M J | 2009 | Plant Physiology2009，149，： | 1 |
| 7 | Accessibility analysis and spatial com-petition effects in the context of GIS supported service loca-tion planning 显示文摘 | Ritsema J R Jong T | 1999 | Computer Environment and Urban Sys-tems1999，23，1： | 1 |
| 8 | The spectral-element method, Beowulf computing and global seismology显示文摘 | KOMATITSCH D RITSEMA J TROMP J | 2002 | Science2002，298，5599： | 1 |
| 9 | GIS and Model of Ac- cessibility, an Application in Planning 显示文摘 | Geertman SCM Ritsema Van Eck | 1995 | International Journal of Geographical Information Systems1995，，9： | 1 |
| 10 | Evidence for strong shear velocity reductions and velocity gradients in the lower mantle beneath Africa显示文摘 | Ritsema J Ni S Helmberger D V | 1998 | Geophysical Research Letters1998，25，： | 1 |
| 11 | Interactions between ridges and plumes显示文摘 | Montagner J P Ritsema J | 2001 | Science2001，294，： | 1 |
| 12 | Complex shear velocity structure beneath African and Iceland 显示文摘 | Ritsema J van Heijst H J Woodhouse J H | 1999 | Science1999，286，： | 1 |
| 13 | LISEM: A single-event physically based hydrological and soil erosion model for drainage basins 显示文摘 | De Roo A P J Wesseling C G and Ritsema C J | 1996 | Hydrological Processes1996，10，8： | 1 |
| 14 | Electromagretic prospecting forgroundwater in Precambrian terrains in the Repubilc of Upper Volta 显示文摘 | Palacky G J Ritsema I L DE Joug SJ | 1982 | Geophysical Prospecting1982，29，： | 1 |
| 15 | Accessibility analysis and spa- tial competition effects in the context of GIS supported servicelo- cation planning 显示文摘 | Ritsema J R Van Eck T de Jong | 1999 | Computers Environment and Urban Systems1999，23，： | 1 |
| 16 | LISEM:A single-event physically based hydrological and soil erosion model for drainage ba-sins I:theory,input and output显示文摘 | DeRoo APJ Wesseling C G Ritsema C J | 1996 | Hydrological Processes1996，10，8： | 1 |
| 17 | A new wireless underground network system for continuous monitoring of soil water contents显示文摘 | Ritsema C J Kuipers H Kleiboer L | 2009 | Water Resources Research2009，45，： | 1 |
| 18 | The meaning of the Tp-Te interval and its diagnostic value 显示文摘 | Kors J A Ritsema van Eek H J Van Herpen G | 2008 | J Eleetrocardiol2008，41，6： | 1 |
| 19 | GIS and model of accessibility: An application in planning显示文摘 | Geertman S CM Ritsema Van Eck | 1995 | International Journal of Geographi- cal Information Systems1995，9，： | 1 |
| 20 | Focal depth estimates of earthquakes in the Himalayan-Tibetan region from teleseismic waveform modeling显示文摘We estimate the focal depths and fault plane solutions of 46 moderate earthquakes in the Himalayan- Tibetan region by modeling the broadband waveforms of teleseismic P waves. The depths of 38 of these earth-quakes range between 0-40 km, with a peak at ~5 km. One earthquake is located within the lower crust of the Indian shield. The remaining eight earthquakes occurred between depths of 80-120 km and are all located in the Pamir-Hindu Kush and the Indo-Myanmar deep seismic zones. None of the earthquakes outside these deep seismic zones are located in the mantle. Global centroid moment tensor (CMT) solutions indicate that most earthquakes in northern Tibet and northern India had thrust-faulting mechanisms and that normal and strike-slip faulting earthquakes occurred primarily in central Tibet. These mechanisms are consistent with the predominantly NNW-SSE compression in the direction of current Himalayan-Tibetan continental collision. | Ling Bai Jeroen Ritsema Junmeng Zhao | 2012 | Earthquake Science2012，25，5： | 1 |
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