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| 1 | Retention and transport of calcium nitrate in variable charge subsoils显示文摘 | Qafoku N.P Sumner M.E | | 0，，： | 1 |
| 2 | Adsorption and desorption of indifferent ions in variable charge subsoils:The possible effect of particle interactions on the counter-ion charge density显示文摘 | Qafoku N.P Sumner M.E | | 0，，： | 1 |
| 3 | Variable charge soils:their mineralogy,chemistry and management显示文摘 | Qafoku N.P Van Ranst E Noble A Baert G | | 0，，： | 1 |
| 4 | Variable charge soils: Their mineralogy, chemistry and management 显示文摘 | Qafoku N P Van R Noble A | 2004 | Adv Agron2004，84，： | 1 |
| 5 | Geochemical,mineralogical and microbiological characteristics of sediment from a naturally reduced zone in a uranium-contaminated aquifer显示文摘 | Campbell K M Kukkadapu R K Qafoku N P | 2012 | Applied Geochemistry2012，，27： | 1 |
| 6 | Terrestrial Nanoparticles and Their Controls on Soil-/Geo-Processes and Reactions显示文摘 | Nikolla P. Qafoku | 2010 | Advances in Agronomy2010，，： | 1 |
| 7 | Pathways of aqueous Cr(VI) attenuation in a slightly al- kaline oxic subsurface 显示文摘 | QAFOKU N P DRESEL P E MCKINLEY J P | 2009 | Environ Sci Technol2009，43，4： | 1 |
| 8 | Variable charge soils: their mineralogy, chemistry and management 显示文摘 | Qafoku N P Van R Noble A | 2004 | Adv Agron2004，84，： | 1 |
| 9 | Foam delivery ofcalcium polysulde to the vadose zone for chromium (VI) immobilization: a laboratory evaluation 显示文摘 | Zhong L IL Qafoku N P Szecsody J E | 2009 | Vadose Zone Journal2009，8，4： | 1 |
| 10 | In Situ X-Ray Diffraction Study of Na+ Saturated Montmorillonite Exposed to Variably Wet Super Critical Co2 显示文摘 | Ilton E S Sehaef H T Qafoku O | 2012 | Environmental science technology2012，46，7： | 1 |
| 11 | Variable charge soils:Their mineralogy,chemistry and management显示文摘 | Qafoku N P Van R Noble A | | 0，，： | 1 |
| 12 | Kinetic desorption and sorption of U( VI ) during reactive transport in a contaminated Hanford sed- iment显示文摘 | QAFOKU N P ZACHARA J M LIU C | 2005 | Environmental Science & Technology2005，39，9： | 1 |
| 13 | Anion transport in columns of variable charge subsoils:nilrate and chloride显示文摘 | Qafoku Nikolla P Malcolm E | 2000 | Joumal of Environmental Quality2000，29，2： | 1 |
| 14 | Anion Transport in Columns of Variable Charge Subsoils:Nitrate and Chloride显示文摘 | Nikolla P Malcolm E | 2000 | Journal of Environmental Quality2000，29，2： | 1 |
| 15 | Arsenate displacement from fly ash in amended soils显示文摘 | Qafoku N P Kukier U Sumner M E | 1999 | Water Air Soil Pollution1999，114，12： | 1 |
| 16 | Anion transport in columns of variable charge subsoils:nitrate and chloride显示文摘 | Qafoku Nikolla P Malcolm E | 2000 | Journal of Environmental Quality2000，29，2： | 1 |
| 17 | Geochemical Implications of Gas Leakage Associated with Geologic CO2 Storage-A Qualitative Review显示文摘 | Harvey O Qafoku N Cantrell K | 2013 | Environmental Science & Technology2013，47，1： | 1 |
| 18 | Foam delivery of calcium polysulfide to the vadose zone for chromium (VI) immobilization: A laboratory evaluation 显示文摘 | Zhong L R Qafoku N P Szecsody J E | 2009 | Vadose Zone Journal2009，8，： | 1 |
| 19 | Anion transport through columns of highly weathered acid soil:Adsorption and retardation显示文摘 | Bellini G Sumner M.E Radcliffe D.E Qafoku N.P | | 0，，： | 1 |
| 20 | Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia显示文摘The Java Island, Indonesia with abundant amount of pyroclastic deposits is located in the very active and dynamic Pacific Ring of Fires. Studying the geochemical weathering indices of these pyroclastic deposits is important to get a clear picture about weathering profiles on deposits resulting from the eruption of Mt. Merapi. Immediately after the first phase of the eruption (March to June 2006), moist and leached pyroclastic deposits were collected. These pyroclastic deposits were found to be composed of volcanic glass, plagioclase feldspar in various proportions, orthopyroxene, clinopyroxene, olivine, amphibole and titanomagnetite. The total elemental composition of the bulk samples (including trace elements and heavy metals) was determined by wet chemical methods and X-ray fluorescence (XRF) analyses. Weathering of the pyroclastic deposits was studied using various weathering indices. The Ruxton ratio, weathering index of Parker, Vought resudual index and chemical index of weathering of moist pyroclastic deposits were lower than those of the leached samples, but the alteration indices (chemical and plagioclase) were slightly higher in the moist compared to the leached pyroclastic deposits. | Dian Fiantis Malik Nelson Eric Van Ranst Jusop Shamshuddin Nikolla P. Qafoku | 2009 | Journal of Mountain Science2009，6，3： | 0 |
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