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Journal of china university of geosciences 2002年第1期13卷 58-66,94页

作者： mushtak talib jabbarfaculty of earth resources , china university of geosciences , wuhan 430074 Faculty of earth resources China University of Geosciences Wuhan 430074

In this study, the remote sensing is applied to the examination of the relationship between desertification and normalized difference vegetation index (NDVI) in the context of northern Shaanxi Province. This relationship is also examined using spatial analysis methods. A strong negative correlation is found in the largest area desert, indicating that the relationship between desert and NDVI is not a simple linear one and that the correlation coefficient between NDVI and vegetation abundance is significant. The normalized difference vegetation index (NDVI) was compared with other vegetation index-based methodologies. NDVI is a valuable first-cut indicator for such systems, although the analysis and interpretation of its relationship to desertification are complex and also based on the detailed analysis of its relationship to ecological zone, vegetation type and season. Conclusions thus made would help to upgrade the methodology as an effective tool for early-warning desertification in the northern Shaanxi Province where a drought is a recurring threat. This methodology includes the integration of NDVI with other socio-economic and bio-physical indicators in CIS, the complementation of desert area data with satellite data, and the analysis of the relationship between NDVI and specific climatic zones, for each season and vegetation type.

关键词： desert desertification remote sensing NDVI china.

Soil Loss by Wind Erosion for Three Different Textured Soils Treated with Polyacrylamide and Crude Oil, Iraq

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Journal of china university of geosciences 2001年第2期12卷 113-116页

作者： mushtak talib Jabbar Faculty of earth resources, china university of geosciences, wuhan 430074 Faculty of earth resources China University of Geosciences

The study is conducted to estimate the resistance of three soils (EL Hartha clay loam, Barjisiya sandy loam and the soil near the sand dunes in Sheikh sa'ad area sandy soil) to wind erosion, it is also aimed at getting full acquaintance of the relationship between the soil loss and the physical and chemical features of soil. In addition to the experiment of some soil stabilizers, polyacrylamide (PAM) concentration of 0.2 % and crude oil in concentration of 1 % in order to reduce or prevent wind erosion. The study shows that the amendment increased the dry soil aggregate >1 mm, mean weight diameter and soil moisture. It is clear that polyacrylamide had greater effect than that of crude oil, besides the great effectiveness of these amendments in decreasing bulk density and relations of soil loss.

关键词： three location in Iraq stabilizers wind erosion soil physical properties.

Study of Sand Dunes and Their Effect on Desertification of Cultivated Lands in Shaanxi Province, china Using Remote Sensing Techniques

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Journal of china university of geosciences 2002年第3期13卷 234-239页

作者： mushtak talib Jabbar Hu Guangdao Chen Jianguo Faculty of earth resources, china university of geosciences, wuhan 430074 Faculty of earth resources China University of Geosciences Wuhan 430074

About half of the arid and semi-arid lands in the world are deserts thatcomprise various types of aeolian sand dunes deposits. In Shaanxi Province, aeolian sand dunes coverconsiderable areas of the Yulin desert and northern Jinbian. Sand dunes are moving in the main winddirection and converting some agricultural area to wasteland. Remote sensing of sand dunes helps inthe understanding of aeolian process and desertification. Remote sensing data combined with fieldstudies are valuable in studying sand dunes, regional aeolian depositional history. In particular,active and inactive sand dunes of the north Shaanxi Province were studied using remote sensing andgeographic information system. In this study, we describe the Landsat thematic mapper (TM) images,covering north Shaanxi Province, which were used to study the distribution, shape, size, trends,density and movement of sand dunes and their effect on desertification of cultivated *** was made depending on soil erodibility factor (Ⅰ) and local climatic factor (C) duringthe period (June to September). The result indicates that soil erosion caused sand drift of 8.957 5,7. 03 ton for Yulin and Jinbian, respectively. The mean sand dunes movement rate were 4.37, 3.11 m,whereas, monthly sand dune advance rate were 1. 092 5, 0. 777 5m, for the two locations,respectively. The study reveals that cultivated lands extended obliquely to the direction of sanddune movement are extremely affected, while other segments that extend parallel to the direction ofthe movement are not affected. Accordingly the north Shaanxi Province was divided into areas ofdifferent classes of potential risk. Moreover, blown sands and sand movement from neighboringhighlands also affect the area of western desert.

关键词： sand dunes desertification remote sensing crust index china

Improving the Efficiency of Water Splitting and Oxygen Reduction Via Single-Atom Anchoring on Graphyne Support

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Energy & Environmental Materials 2024年第5期7卷 276-286页

作者： Shamraiz Hussain talib Beenish Bashir Muhammad Ajmal Khan Babar Ali Sharmarke Mohamed Ahsanulhaq Qurashi Jun Li Advanced Materials Chemistry Center (AMCC) Khalifa University of Science and Technology Department of Chemistry Khalifa University of Science and Technology Department of Chemistry and Biochemistry George Mason University Interdisciplinary Research Center for Refining and Advanced Chemicals King Fahd University of Petroleum & Minerals Department of Chemistry and Engineering Research Center of Advanced Rare-earth Materials of Ministry of Education Tsinghua University Department of Chemistry and Guangdong Provincial Key Laboratory of Catalytic Chemistry Southern University of Science and Technology

Single-atom catalysts （SACs） have received significant interest for optimizing metal atom utilization and superior catalytic performance in hydrogen evolution reaction（HER）, oxygen evolution reaction （OER）, and oxygen reduction reaction （ORR）. In this study, we investigate a range of single-transition metal （STM1=Sc1, Ti1, V1,Cr1, Mn1, Fe1, Co1, Ni1, Cu1, Zr1, Nb1, Mo1, Ru1, Rh1, Pd1, Ag1, W1, Re1, Os1, Ir1, Pt1,and Au1） atoms supported on graphyne （GY） surface for HER/OER and ORR using first-principle calculations. Ab initio molecular dynamics （AIMD） simulations and phonon dispersion spectra reveal the dynamic and thermal stabilities of the GY surface. The exceptional stability of all supported STM1atoms within the H1cavity of the GY surface exists in an isolated form, facilitating the uniform distribution and proper arrangement of single atoms on GY. In particular, Sc1, Co1, Fe1, and Au1/GY demonstrate promising catalytic efficiency in the HER due to idealisticΔGH*values via the Volmer-Heyrovsky pathway. Notably, Sc1and Au1/GY exhibit superior HER catalytic activity compared to other studied catalysts. Co1/GY catalyst exhibits higher selectivity and activity for the OER, with an overpotential（0.46 V） comparable to MoC2, IrO2, and RuO2. Also, Rh1and Co1/GY SACs exhibited promising electrocatalysts for the ORR, with an overpotential of 0.36 and0.46 V, respectively. Therefore, Co1/GY is a versatile electrocatalyst for metal-air batteries and water-splitting. This study further incorporates computational analysis of the kinetic potential energy barriers of Co1and Rh1in the OER and ORR.

关键词： Oxygen Reduction Reaction Graphyne Support Hydrogen Evolution Reaction Oxygen Evolution Reaction Single-Atom Catalyst Water Splitting

Using Remote Sensing and GIS Techniques to Study Soil Degradation Processes in North Shaanxi Province,china

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Journal of china university of geosciences 2003年第4期14卷 356-362页

作者： mushtak talib Jabbar Faculty of earth resources China University of Geosciences

Satellite image data and thematic map data were used to provide comprehensive views of surface-bound conditions such as soil and vegetation degradation. The current work applies a computerized parametric methodology, developed by FAO, UNEP and UNESCO to assess and evaluate soil degradation at 1∶250 000 mapping scale. The study area is located in the arid and semi-arid zone of the northern part of Shaanxi Province in china, a region with considerable agricultural potential; Landsat TM images were utilized to provide recent data on land cover and use of the area. ARC/INFO and ArcView softwares were used to manage and manipulate thematic data, to process satellite images, and tabular data source. ER mapper software is utilized to derive the normalized difference vegetation index (ND VI) values while field data to estimate soil erodibility ( SE ) factor. A system is established for rating soil parameters, slope, climate factor and human factor activity. The rating values serve as inputs into a modified universal soil loss equation (USLE) to calculate the present state and risk for soil degradation processes, namely soil wind erosion. The produced maps and tabular data show the risk and the present status of different soil degradation processes. The study area, in general, is exposed to high risk of wind erosion and high hazards of water erosion. Several desertification maps were produced, which reflect the desertification types persisting in the study area. Wind erosion, water erosion, vegetation degradation, physical degradation and salinization are the basic desertification maps, and others are combinations of these basic maps. In terms of statistic analysis, 33.75 % of the total land area (120.330 0 ha) is considered as sand or sand dune, and not included in our analysis of desertification. About 29.41 % of the total land area has slight or moderate desertification and 37.465 % is facing severe desertification.

关键词： soil degradation desertification GIS remote sensing china.

Composition and source apportionment of dust fall around a natural lake

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Journal of Environmental Sciences 2015年第7期27卷 143-155页

作者： Mohd talib Latif Sofia Aida Ngah Doreena Dominick Intan Suraya Razak Xinxin Guo Thunwadee Srithawirat Idris Mushrifah School of Environmental and Natural Resource Sciences Faculty of Science and Technology Universiti Kebangsaan Malaysia Institute for Environment and Development (LESTARI) Universiti Kebangsaan Malaysia Centre for Atmospheric Chemistry University of Wollongong Department of Environmental Engineering Faculty of Engineering and Green Technology Universiti Tunku Abdul Rahman Department of Environmental Science Faculty of Science and Technology Pibulsongkram Rajabhat University Pusat Penyelidikan Tasik Chini (PPTC) Faculty of Science and Technology Universiti Kebangsaan Malaysia

The aim of this study was to determine the source apportionment of dust fall around Lake Chini, Malaysia. Samples were collected monthly between December 2012 and March2013 at seven sampling stations located around Lake Chini. The samples were filtered to separate the dissolved and undissolved solids. The ionic compositions（NO-3, SO2-4, Cl-and NH＋4） were determined using ion chromatography（IC） while major elements（K, Na, Ca and Mg） and trace metals（Zn, Fe, Al, Ni, Mn, Cr, Pb and Cd） were determined using inductively coupled plasma mass spectrometry（ICP-MS）. The results showed that the average concentration of total solids around Lake Chini was 93.49 ± 16.16 mg/（m2·day）. SO2-4, Na and Zn dominated the dissolved portion of the dust fall. The enrichment factors（EF） revealed that the source of the trace metals and major elements in the rain water was anthropogenic, except for Fe. Hierarchical agglomerative cluster analysis（HACA） classified the seven monitoring stations and 16 variables into five groups and three groups respectively. A coupled receptor model, principal component analysis multiple linear regression（PCA-MLR）, revealed that the sources of dust fall in Lake Chini were dominated by agricultural and biomass burning（42%）,followed by the earth＇s crust（28%）, sea spray（16%） and a mixture of soil dust and vehicle emissions（14%）.

关键词： Trace metal Major element Anion Source apportionment Lake Ghini Malaysia

The Representation of Soil Moisture−Atmosphere Feedbacks across the Tibetan Plateau in CMIP6

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Advances in Atmospheric Sciences 2023年第11期40卷 2063-2081页

作者： Joshua talib Omar V.MÜLLER Emma J.BARTON Christopher M.TAYLOR Pier Luigi VIDALE U.K.Centre of Ecology and Hydrology WallingfordOX108BBU.K. National Centre for Atmospheric Science ReadingRG66BBU.K. Consejo Nacional de Investigaciones Científicas y Técnicas(CONICET) Centro de Estudios de Variabilidad y Cambio Climático(CEVARCAM)Facultad de Ingeniería y Ciencias HídricasUniversidad Nacional del LitoralSanta FeArgentina National Centre for earth Observation WallingfordOX108BBU.K. Department of Meteorology University of ReadingReadingRG66BBU.K.

Thermal processes on the Tibetan Plateau(TP)influence atmospheric conditions on regional and global *** this,previous work has shown that soil moisture−driven surface flux variations feed back onto the *** soil moisture is a source of atmospheric predictability,no study has evaluated soil moisture−atmosphere coupling on the TP in general circulation models(GCMs).In this study,we use several analysis techniques to assess soil moisture−atmosphere coupling in CMIP6 simulations including:instantaneous coupling indices;analysis of flux and atmospheric behaviour during dry spells;and a quantification of the preference for convection over drier *** these metrics we partition feedbacks into their atmospheric and terrestrial *** with previous global studies,we conclude substantial inter-model differences in the representation of soil moisture−atmosphere coupling,and that most models underestimate such *** on dry spell analysis,most models underestimate increased sensible heat during periods of rainfall *** example,the model-mean bias in anomalous sensible heat flux is 10 W m−2(≈25%)smaller compared to *** dry-spell sensible heat fluxes lead to a weaker atmospheric *** also find that most GCMs fail to capture the negative feedback between soil moisture and deep *** poor simulation of feedbacks in CMIP6 experiments suggests that forecast models also struggle to exploit soil moisture−driven *** improve the representation of land−atmosphere feedbacks requires developments in not only atmospheric modelling,but also surface processes,as we find weak relationships between rainfall biases and coupling indexes.

关键词： model evaluation land-atmosphere feedbacks Tibetan Plateau precipitation surface energy balance

Mssbauer and XRD characterization of contaminated sediments by coal mining drainage in Neath Canal, South Wales, UK

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Acta Geochimica 2006年第S1期 137-138页

作者： Akihito Kuno talib Abdulameer Mahdi David J. Evans Masaaki Miyahara Yoshio Takahashi Motoyuki Matsuo Hiroshi Shimizu Graduate School of Arts and Sciences The University of Tokyo 3-8-1 Komaba Meguro-ku Tokyo 153-8902 Japan GRC School of Engineering Cardiff University Cardiff CF24 0YH United Kingdom Department of Biological Chemistry John Innes Centre Norwich Research Park Norwich NR4 7UH United Kingdom Department of earth and Planetary Systems Science Hiroshima University Higashi-Hiroshima 739-8526 Japan

Mssbauer and XRD characterization of contaminated sediments by coal mining drainage in Neath Canal, South Wales, UK

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Chinese Journal Of Geochemistry 2006年第B08期25卷 137-138页

作者： Guodong ZHENG Akihito Kuno talib Abdulameer Mahdi David J. Evans Masaaki Miyahara Yoshio Takahashi Motoyuki Matsuo Hiroshi Shimizu Lanzhou Center for Oil ＆ Gas resources Institute of Geology ＆ Geophysics Chinese Academy of Sciences Lanzhou 730000 China Department of earth and Planetary Systems Science Hiroshima University Higashi-Hiroshima 739-8526 Japan GRC School of Engineering Cardiff University Cardiff CF24 0YH United Kingdom Graduate School of Arts and Sciences The University of Tokyo 3-8-1 Komaba Meguro-ku Tokyo 153-8902 Japan Department of Biological Chemistry John Innes Centre Norwich Research Park. Norwich NR4 7UH United Kingdom