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| 1 | Origin of clay minerals on section of Luochuan loesspalaeosol in Shaanxi Province,northwest China显示文摘Crystallinity,polytype,and morphology of clay minerals in the Luochuan loess-palaeosols in Shaanxi Province,northwest China were studied in order to have an insight into their origin using X-ray diffraction(XRD)analysis and scanning electron microscopy(SEM)methods.The SEM observations showed that the morphology of some illites seems to be lath-shaped crystals.An analysis of illite crystallinity(IC)on the Luochuan section indicated that the origin of illite was related to the rocks of an anchizone.Most illite in the Luochuan loess-palaeosol section were of 2M1 polytype,but some were of 1M polytype formed by weathering of feldspar in the process of pedogenesis.Illite in the Luochuan section has undergone both physical and chemical weathering.These results revealed that most illite were of detrital origin related to the source area of an anchizone,but parts of the illite were of an authigenic origin formed during pedogenesis after sedimentation.Chlorites in the samples of the Luochuan section were mainly composed of irregular flaky grains and their crystallinity was good.These showed that chlorite had the detrital origin formed by physical weathering.Kaolinite crystallinity was relatively good.The value of CIA on the Luochuan section ranges from 61.9 to 69,and therefore kaolinite could not be formed during weathering and pedogenesis.These results indicated that the kaolinite had a detrital origin.Morphology of smectite seems to be capillaceous.The XRD patterns of all samples contained diffraction peaks at 1.5218Å(nontronite)and 1.5052Å(montmorillonite),thus indicating an intermediate composition between trioctahedral and dioctahedral smectite.The smectite crystallinity was very poor.These results revealed that smectite in the study area was authigenic rather than detrital origin. | Chang Dok Won HanLie Hong Kum Ryong Pak | 2020 | Frontiers of Earth Science2020，14，4： | 0 |
| 2 | Physical clogging experiment of sand gravel infiltration with Yellow River water in the Yufuhe River channel of Jinan, China显示文摘To make sense of physical clogging during Yellow River water spreading in the strong leakage zone of the Yufuhe River,a laboratory sand column experiment was undertaken and the heterogeneous sand gravel with a uniformity coefficient of 25.2 from the Yufuhe River was used as an infiltration medium.Under either the condition of raw sand or washed sand,physical clogging tests were conducted with constant hydraulic heads of 10 cm and 30 cm and inflow suspension concentrations of 200 mg/L,500 mg/L,and 1000 mg/L.The fine particles in the suspension and in the raw sand were considered exogenous and endogenous particles,respectively.Rapid clogging was observed in the porous medium when the inflow concentrations of the exogenous particles were high,and increased hydraulic head led to serious clogging.This result indicated that the Yufuhe River has a strong recharge capability with respect to clogging.The analysis of particle content shows that endogenous fine particles(diameter 1–10 mm and 50–74 mm)had less mobility and generally accumulated in the sand column,whereas particles with diameter 10–50 mm had greater mobility in the sand column.And the distribution of exogenous fine particles size after movement is relatively uniform in the sand column.Field observations indicated that the filtration effect of the aquifers have greatly improved the water quality of recharge water in the strong leakage zone of the Yufuhe River,and test data of turbidity also verified the results of the sand column experiments. | Qingyang ZHENG Weiping WANG Shuai LIU Shisong QU | 2020 | Frontiers of Earth Science2020，14，2： | 0 |
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