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(1) SCI刊物论文
代表性SCI论文
1. Liu Zaihua, Svensson U, Dreybrodt W, Yuan Daoxian, Buhmann D, 1995. Hydrodynamic control of inorganic calcite precipitation in Huanglong Ravine, China: Field measurements and theoretical prediction of deposition rates. Geochimica et Cosmochimica Acta, 59(15): 3087-3097.
2. Liu Zaihua and Dreybrodt W, 1997. Dissolution kinetics of calcium carbonate minerals in H2O-CO2 solutions in turbulent flow: the role of the diffusion boundary layer and the slow reaction H2O+CO2«H++HCO3-. Geochimica et Cosmochimica Acta, 61(14): 2879-2889.
3. Liu Zaihua and Zhao Jinbo, 2000. Contribution of carbonate rock weathering to the atmospheric CO2 sink. Environmental Geology, 39(9): 1053-1058.
4. Liu Zaihua, Groves C, Yuan Daoxian, Meiman J, Jiang Guanghui, He Shiyi, 2004. Hydrochemical variations during flood pulses in the southwest China peak cluster karst: Impacts of CaCO3-H2O-CO2 interactions. Hydrological Processes, 18(13):2423-2437.
5. Liu Zaihua, Li Qiang, Sun Hailong, Wang Jinliang, 2007. Seasonal, diurnal and storm-scale hydrochemical variations of typical epikarst springs in subtropical karst areas of SW China: soil CO2 and dilution effects. Journal of Hydrology, 337(1-2): 207-223.
6. Dorale J, Liu Zaihua*, 2009. Limitations of Hendy Test criteria in judging the paleoclimatic suitability of speleothems and the need for replication. The Journal of Cave and Karst Studies, 71(1): 73-80.
7. Sun Hailong, Liu Zaihua*, 2010. Wet-dry seasonal and spatial variations in the δ13C and δ18O values of the modern endogenic travertine at Baishuitai, Yunnan, SW China and their paleoclimatic and paleoenvironmental implications. Geochimica et Cosmochimica Acta, 74(3): 1016-1029.
8. Liu Zaihua, Dreybrodt W, Wang Haijing, 2010. A new direction in effective accounting for the atmospheric CO2 budget: Considering the combined action of carbonate dissolution, the global water cycle and photosynthetic uptake of DIC by aquatic organisms. Earth-Science Reviews, 99(3-4):162-172.
9. Liu Zaihua, Sun Hailong, Lu Baoying, Liu Xiangling, Ye Wenbin, Zeng Cheng, 2010. Wet-dry seasonal variations of hydrochemistry and carbonate precipitation rates in a travertine-depositing canal at Baishuitai, Yunnan, SW China: Implications for the formation of biannual laminae in travertine and for climatic reconstruction. Chemical Geology, 273(3-4): 258-266.
10. Zhao Min, Zeng Cheng, Liu Zaihua*, Wang Shijie, 2010. Effect of different land use/land cover on karst hydrogeochemistry: A paired catchment study of Chenqi and Dengzhanhe, Puding, Guizhou, SW China. Journal of Hydrology, 388(1-2):121-130.
11. Liu Zaihua, Dreybrodt W, Liu Huan, 2011. Atmospheric CO2 sink: silicate weathering or carbonate weathering? Applied Geochemistry, 26s: 292-294.
12. Yan Hao, Sun Hailong, Liu Zaihua*, 2012. Equilibrium vs. kinetic fractionation of oxygen isotopes in the two low-temperature travertine-depositing systems with distinct hydrodynamic conditions at Baishuitai, Yunnan, SW China. Geochimica et Cosmochimica Acta 95: 63-78.
13. Yang Rui, Liu Zaihua*, Zeng Cheng, Zhao Min, 2012. Response of epikarst hydrochemical changes to soil CO2 and weather conditions at Chenqi, Puding, SW China. Journal of Hydrology 468-469: 151-158.
14. Wang Haijing, Yan Hao, Liu Zaihua*, 2014. Contrasts in variations of the carbon and oxygen isotopic composition of travertines formed in pools and a ramp stream at Huanglong Ravine, China: Implications for paleoclimatic interpretations. Geochimica et Cosmochimica Acta 125: 34-48.
15. Sun Hailong, Liu Zaihua*, Yan Hao, 2014. Oxygen isotope fractionation in travertine-depositing pools at Baishuitai, Yunnan, SW China: Effects of deposition rates. Geochimica et Cosmochimica Acta 133c: 340-350.
16. Liu Zaihua*, Dreybrodt W, 2015. Significance of the carbon sink produced by H2O-carbonate-CO2-aquatic phototroph interaction on land. Science Bulletin 60 (2): 182-191.
17. Liu Huan, Liu Zaihua*, Macpherson G, Yang Rui, Chen Bo, Sun Hailong, 2015. Diurnal hydrochemical variations in a karst spring and two ponds, Maolan karst experimental site, China: biological pump effects. Journal of Hydrology 522, 407-417.
18. Zhao Min, Liu Zaihua*, Li Hongchun*, Zeng Cheng, Yang Rui, Chen Bo, Yan Hao, 2015. Response of dissolved inorganic carbon (DIC) and 13CDIC to changes in climate and land cover in SW China karst catchments. Geochimica et Cosmochimica Acta 165: 123-136.
19. Yang Rui, Chen Bo, Liu Huan, Liu Zaihua*, 2015. Carbon sequestration and decreased CO2 emission caused by terrestrial aquatic photosynthesis: insights from diurnal hydrochemical variations in an epikarst spring and two spring-fed ponds in different seasons. Applied Geochemistry 63 (3): 248-260
20. Zeng C, Liu Z*, Yang J, Yang R, 2015. A groundwater conceptual model and karst- related carbon sink of a glaciated alpine karst aquifer, Southwestern China. Journal of Hydrology 529, 120-133.
21. Zeng Cheng, Liu Zaihua*, Zhao Min, Yang Rui, 2016. Hydrologically-driven variation in karst process-related carbon sink flux: insights from high-resolution monitoring of three typical karst catchments in the subtropical karst area of SW China. Journal of Hydrology 533: 74–90.
22. Yan Hao, Schmitt A*, Liu Zaihua*, Sophie G, Sun Hailong, Chen Jiubin, Chabaux F, 2016. Calcium isotopic fractionation during travertine deposition under different hydrodynamic conditions at Baishuitai (Yunnan, SW China). Chemical Geology 426:60-70.
23. Zeng Sibo, Jiang Yongjun*, Liu Zaihua*, 2016. Assessment of climate impacts on the karst-related carbon sink in SW China using MPD and GIS. Global and Planetary Change 144: 171-181.
24. Yang Mingxing, Liu Zaihua*, Sun Hailong, Yang Rui, Chen Bo, 2016. Organic carbon source tracing and DIC fertilization effect in the Pearl River: insights from lipid biomarker and geochemical analysis. Applied Geochemistry 73: 132-141.
25. Yan Hao, Liu Zaihua*, Sun Hailong, 2017. Effect of in-stream physicochemical processes on the seasonal variations in δ13C and δ18O values in laminated travertine deposits in a mountain stream channel. Geochimica et Cosmochimica Acta 202: 179-189.
26. Liu Zaihua*, Zhao Min, Yang Rui, Sun Hailong, Chen Bo, Yang Mingxing, Zeng Qingrui, Zeng Haitao, 2017. “Old” carbon entering the South China Sea from the carbonate-rich Pearl River Basin. Applied Geochemistry 78: 96-104.
27. Chen Bo, Yang Rui, Liu Zaihua*, Sun Hailong, Yan Hao, Zeng Qingrui, Zeng Sibo, Zeng Cheng, 2017. Coupled control of land uses and aquatic biological processes on the diurnal hydrochemical variations in five ponds at the Shawan Karst Test Site: implications for the carbonate weathering-related carbon sink. Chemical Geology 456:58-71.
28. Zeng Qingrui, Liu Zaihua*, Chen Bo, Hu Yundi, Zeng Sibo, Zeng Cheng, Yang Rui, He Haibo, Zhu Hui, Cai Xianli, Chen Jia, Ou Yi, 2017. Carbonate weathering-related carbon sink fluxes under different land uses: A case study from the Shawan Simulation Test Site, Puding, Southwest China. Chemical Geology 474: 58-71.
29. Liu Zaihua, Macpherson GL, Groves G, Martin JB, Yuan Daoxian, Zeng Sibo, 2018. Large and active CO2 uptake by coupled carbonate weathering. Earth-Science Reviews 182, 42-49.
30. Min Zhao, Yundi Hu, Cheng Zeng, Zaihua Liu*, Rui Yang, Bo Chen, 2018. Effects of land cover on variations in stable hydrogen and oxygen isotopes in karst groundwater—A comparative study of three karst catchments in Guizhou Province, Southwest China. Journal of Hydrology 565, 374-385.
31. Yundi Hu, Zaihua Liu*, Min Zhao, Qingrui Zeng, Cheng Zeng, Bo Chen, Chongying Chen, Haibo He, Xianli Cai, Yi Ou, Jia Chen, 2018. Using deuterium excess, precipitation and runoff data to determine evaporation and transpiration: A case study from Shawan Karst Test Site, Puding, Guizhou, China. Geochimica et Cosmochimica Acta 242, 21-33.
32. Zeng Sibo, Liu Huan, Chen Bo, Liu Zaihua*, Cheng Zeng, Min Zhao, Hailong Sun, Qingrui Zeng, Rui Yang, Mingxing Yang, Yundi Hu, 2019. Seasonal and diurnal variations in DIC, NO3- and TOC concentrations of spring-pond ecosystems under different land-uses at Shawan Karst Test Site, SW China: Carbon limitation of aquatic photosynthesis. Journal of Hydrology 574: 811-821.
33. Sibo Zeng, Zaihua Liu*, Georg Kaufmann*, 2019. Sensitivity of global carbonate weathering carbon-sink flux to climate and land-use changes. Nature Communications 10: 5749.
34. Hao Yan*, Zaihua Liu*, Hailong Sun, 2020. Large degrees of carbon isotope disequilibrium during precipitation-associated degassing of CO2 in a mountain stream. Geochimica et Cosmochimica Acta 273: 244-256.
35. Haibo He, Zaihua Liu*, Chongying Chen, Yu Wei, Qian Bao, Hailong Sun, Hao Yan, 2020. Sediment records of biological carbon pump effect in Fuxian Lake, Yunnan, China during the past century: Implication for the sensitivity of carbon sink by the coupled carbonate weathering to climate and land-use changes. Science of the Total Environment 720: 137539.
36. Hu, Y., Liu, Z.*, Ford, D.*, Zhao, M., Bao, Q., Zeng, C., Gong, X., Wei, Y., Cai, X., Chen, J., 2020. Conservation of oxygen and hydrogen seasonal isotopic signals in meteoric precipitation in groundwater: an experimental tank study of the effects of land cover in a summer monsoon climate. Geochimica et Cosmochimica Acta 284: 254-272.
37. Bao Qian, Liu Zaihua*, Min Zhao, Yundi Hu, Dong Li, Cuihong Han, Yu Wei, Song Ma, Yi Zhang, 2020. Primary productivity and seasonal dynamics of planktonic algae species composition in karst surface waters under different land uses: A case study from the Shawan Karst Test Site, Puding, SW China. Journal of Hydrology 591:https://doi.org/10.1016/j.jhydrol.2020.125295
38. Zeng Sibo*, Liu Zaihua*, Nico Goldscheider, Simon Frank, Cheng Zeng, Qingrui Zeng, Hailong Sun, 2020. Control of temperature, runoff and land-cover on carbonate weathering: comparisons between different karst catchments. Hydrogeology Journal:https://doi.org/10.1007/s10040-020-02252-5
其它SCI论文
1. Liu Z, Yuan D, Shen Z, 1991. Effect of coal-mine waters of variable pH on springwater quality: A case study. Environmental Geology and Water Science, 17(3):219-225.
2. Liu Z and He D, 1994. Two Mechanisms of tufa formation in the cement grouting tunnels at Wujiangdu Hydropower Station of Guizhou. Chinese Science Bulletin, 39(17): 1468-1472.
3.Yuan D, Li B, Liu Z, 1995. Karst in China. Episodes, 18(1-2):62-65.
4. Dreybrodt W, Lauckner J, Liu Z, Svensson U, Buhmann D, 1996. The kinetics of reaction CO2 +H2O« H++HCO3- as one of the rate limiting steps for the dissolution of calcite in the system CaCO3-CO2 -H2O. Geochimica et Cosmochimica Acta, 60(18): 3375-3381.
5. Liu Z and He D, 1998. Special speleothems in cement-grouting tunnels and their implications of the atmospheric CO2 sink. Environmental Geology, 35(4):258-262.
6. Liu Z, Yuan D, He S, Zhang M, Zhang J, 2000. Geochemical features of the geothermal CO2-water-carbonate rock system and analysis on its CO2 sources. Science in China(D), 43(6):569-576.
7. Liu Z, Dreybrodt W, 2001. Kinetics and rate-limiting mechanisms of dolomite dissolution at various CO2 partial pressures. Science in China(B), 44(5):500-509.
8. Liu Z, 2001. Role of carbonic anhydrase as an activator in carbonate rock dissolution and its implication for atmospheric CO2 sink. Acta Geologica Sinica, 75(3):275-278.
9. Liu Z, Zhang M, Li Q, You S, 2003. Hydrochemical and isotope characteristics of spring water and travertine in the Baishuitai area (SW China) and their meaning for paleoenvironmental reconstruction. Environmental Geology, 44(6):698-704.
10. Yoshimura K, Liu Z, Cao J, Yuan D, Inokura Y, Noto M, 2004. Deep source CO2in natural waters and its role in extensive tufa deposition in the Huanglong Ravines, Sichuan, China. Chemical Geology, 205(1-2):141-153.
11. Liu Z, Groves C, Yuan D, Meiman J, 2004. South China Karst Aquifer Storm-Scale Hydrogeochemistry. Ground Water, 42(4):491-499.
12,Liu Z, Yuan D, Dreybrodt W, 2005. Comparative study of dissolution rate-determining mechanisms of limestone and dolomite. Environmental Geology, 49 (2):274-279.
13. Liu Z, Li Q, Sun H, Liao C, Li H, Wang J, Wu K, 2006. Diurnal Variations of Hydrochemistry in a Travertine-depositing Stream at Baishuitai, Yunnan, SW China. Aquatic Geochemistry, 12(2):103-121.
14. Liu Z, Li H, You C, Wan N, Sun H, 2006. Thickness and stable isotopic characteristics of modern seasonal climate-controlled sub-annual travertine laminas in a travertine-depositing stream at Baishuitai, SW China: implications for paleoclimate reconstruction. Environmental Geology, 51(2):257-265.
15. Li H, Ku T, Yuan D, Wan N, Ma Z, Zhang P, Bar-Matthews M, Ayalon A, Liu Z, Zhang M, Zhu Z, Wang R, 2007. Stable isotopic compositions of waters in the karst environments of China: Climatic implications. Applied Geochemistry, 22(8): 1748–1763.
16. Liu Z, Dreybrodt W, Wang H, 2008.A possible important CO2 sink by the global water cycle. Chinese Science Bulletin, 53 (3): 402-407.
17. Li Q, Sun H, Han J, Liu Z, Yu L, 2008. High-resolution study on the hydrochemical variations caused by the dilution of precipitation in the epikarst spring: an example spring of Landiantang at Nongla, Mashan, China. Environmental Geology, 54(2): 347–354.
18. Liu Z, Liu X, Liao C, 2008. Daytime deposition and nighttime dissolution of calcium carbonate controlled by submerged plants in a karst spring-fed pool: insights from high time-resolution monitoring of physico-chemistry of water. Environmental Geology, 55(6): 1159-1168.
19. Liu Y, Liu Z*, Zhang J, He Y, Sun H, 2010. Experimental study on the utilization of DIC by Oocystis solitaria Wittr and its influence on the precipitation of calcium carbonate in karst and non-karst waters. Carbonates and Evaporites, 25(1):21-26.
20. Wang H, Liu Z*, Zhang J, Sun H, An D, Fu R, Wang X, 2010. Spatial and temporal hydrochemical variations of the spring-fed travertine-depositing stream in the Huanglong ravine, Sichuan, SW China. Acta Carsologica, 39(2): 247-259.
21. Liu Z, 2011. Is pedogenic carbonate an important atmospheric CO2 sink? Chinese Science Bulletin, 56(35): 3743-3747.
22. Lian B, Yuan D, Liu Z, 2011. Effect of microbes on karstification in karst ecosystems. Chinese Science Bulletin, 56 (35): 3794–3796.
23. Zhang J, Wang H, Liu Z*, An D, Dreybrodt W, 2012. Spatial-temporal variations of travertine deposition rates and their controlling factors in Huanglong Ravine, China - a world’s heritage site. Applied Geochemistry, 27(1):211-222.
24. Zeng C, Gremaud V, Zeng H, Liu Z*, Goldscheider N, 2012. Temperature-driven meltwater production and hydrochemical variations at a glaciated alpine karst aquifer: implication for the atmospheric CO2 sink under global warming. Environmental Earth Sciences, 65:2285–2297.
25. Zhou G, Huang J, Tao X, Luo Q, Zhang R, Liu Z, 2015. Overview of 30 years of research on solubility trapping in Chinese karst. Earth-Science Reviews, 146, 183-194.
26. Kele S, Breitenbach SFM, Capezzuoli E, Meckler AN, Ziegler M, Millan IM, Kluge T, Deák J, Hanselmann K, John CM, Yan H, Liu Z, Bernasconi SM, 2015. Temperature dependence of oxygen- and clumped isotope fractionation in carbonates: a study of travertines and tufas in the 6-95°C temperature range. Geochimica et Cosmochimica Acta 168, 172-192.
27. Zhao M, Li H, Liu Z, Mii H, Sun H, Shen C, Kang S, 2015. Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave. Journal of Asian Earth Sciences 114(3): 549-561.
28. Haibo He, Zaihua Liu*, Chongying Chen, Yu Wei, Qian Bao,Hailong Sun,Yundi Hu, Hao Yan, 2019. Influence of the biological carbon pump effect on the sources and deposition of organic matter in Fuxian Lake, a deep oligotrophic lake in southwest China. Acta Geochim 38: 613–626.
(2) 其它期刊英文论文
1. Dreybrodt, W., Svensson, U., Liu Zaihua, and Yuan, D.X., 1994. Influence of hydrodynamic conditions and water chemistry on the formation of tufa in Huanglong, Sichuan. Cave & Karst Science, 21:3389
2. Liu Zaihua, Yuan, D.X., and He, S.Y., 1997. Stable carbon isotope geochemical and hydrochemical features in the system of Carbonate-H2O-CO2 and their implications -- Evidence from several typical karst areas of China. Acta Geologica Sinica 71(4): 446-454
3. Kano A, Liu Z, Takashima C, Kawai T, Hori M. 2004. Paleoclimate analysis using tufa deposits-a case study in Niangziguan, Shanxi Province, China. Earth Science (Chikyu Kagaku) 58:305-316
4. Liu Zaihua, Sun Hailong, Hongchun Li, Naijung Wan, 2011. d13C, d18O and deposition rate of tufa in Xiangshui River, SWChina: implications for land-cover change caused by climate and human impact during the late Holocene. Geological Society, London, Special Publications, 352: 85–96. DOI: 10.1144/SP352.7
5. Liu Z, 2013. Review on the role of terrestrial aquatic photosynthesis in the global carbon cycle. Procedia Earth and Planetary Science 7: 513–516.
6. Yang R, Zhao M, Zeng C, Chen B, Liu Z*, 2014. Spatiotemporal variations of soil CO2 in Chenqi, Puding, SW China: The effects of weather and LUCC. In B. Andreo et al. (eds.), Hydrogeological and Environmental Investigations in Karst Systems, Environmental Earth Sciences 1, 191-205. Springer-Verlag, Berlin Heidelberg.
(3) 中文期刊(包括核心期刊)论文
代表性论文
1. 刘再华, 贺殿彬, 1994.贵州乌江渡水电站灌浆廊道中钙华的两种成因机制. 科学通报, 39(12):1114-1117
2. 刘再华,袁道先,何师意,张美良,张加桂,2000. 地热CO2-水-碳酸盐岩系统的地球化学特征及其CO2来源.中国科学(D辑),30(2):209-214
3. 刘再华,2000.大气CO2的两个重要的汇. 科学通报,45(21);2348-2351
4. 刘再华,W. Dreybrodt, 2001. 不同CO2分压条件下的白云岩溶解动力学机理.中国科学(B辑),31(4):377-384
5. 刘再华,Wolfgang Dreybrodt,王海静,2007. 一种由全球水循环产生的可能重要的CO2汇. 科学通报,52(20):2418-2422
6. 刘再华,2011. 土壤碳酸盐是重要的大气CO2汇吗? 科学通报 56(26): 2209-2211.
7. 刘再华,2012. 岩石风化碳汇研究的最新进展和展望 (特邀评述). 科学通报 57(2-3): 95-102.
8. 刘再华, 2014. 表生和内生钙华的气候环境指代意义研究进展(特邀评述). 科学通报, 59(23): 2229-2239.
9. 曾庆睿,刘再华*, 2017. 玄武岩风化是重要的碳汇机制吗?科学通报 62(10) : 1041-1049.
10. 陈崇瑛, 刘再华*, 2017. 喀斯特地表水生生态系统生物碳泵的碳汇和水环境改善效应. 科学通报 62(30): 3440-3450.
其它论文
1. 刘再华, 1989. 娘子关泉群水的来源再研究.中国岩溶, 8(3):200-207
2. 刘再华, 1990.岩溶水文地球化学研究中 pH值野外测定的必要性. 中国岩溶, 9(4):310-317
3. 刘再华, 1991.表层岩溶带的水温特征及其与下部包气带的对比 --以桂林岩溶水文地质试验场为例. 中国岩溶, 10(4):277-282
4. 刘再华, 1992. 桂林岩溶水文地质试验场岩溶水文地球化学的研究. 中国岩溶, 11(3):209-217
5. 刘再华, 袁道先,W. Dreybrodt, U. Svensson, 1993.四川黄龙钙华的形成. 中国岩溶, 12(3):185-191
6. 刘再华,贺殿彬, 1994.贵州乌江渡水电站帷幕灌浆廊道中的钙华及其成因. 中国岩溶, 13(1):37-40
7. 刘再华,袁道先,何师意. 1997. 不同岩溶动力系统的碳稳定同位素和地球化学特征及其意义¾以我国几个典型岩溶地区为例. 地质学报, 71(3):281-288
8. 刘再华, W. Dreybrodt. 1998. 流动CO2-H2O系统中方解石溶解动力学机制--扩散边界层效应和CO2转换控制. 地质学报, 72(4):340~348
9. 刘再华,W.Dreybrodt, 1998. DBL理论模型及方解石溶解、沉积速率预报. 中国岩溶, 17(1):1-7
10. 刘再华, 何师意, 袁道先, 1998. 土壤中的CO2及其对岩溶作用的驱动. 水文地质工程地质,25(4):42~45
11. 刘再华,袁道先,何师意,1999. 岩溶动力系统水化学动态变化规律分析. 中国岩溶, 18(2):103-108
12. 刘再华,2000. 外源水对灰岩和白云岩的侵蚀速率野外试验研究-以桂林尧山为例. 中国岩溶, 19(1):1-4
13. 刘再华,袁道先,2000. 我国典型表层岩溶系统的地球化学动态特征及其环境意义.地质论评 , 46(3):324-327.
14.刘再华,2000. 碳酸盐岩岩溶作用对大气CO2 沉降的贡献. 中国岩溶,19(4):293-300
15.刘再华,2001. 一种特殊的碳酸盐沉积及其环境意义. 地学前缘,8(1):197-201
16. 刘再华,2001. 碳酸酐酶对碳酸盐岩溶解的催化作用及其在大气CO2沉降中的意义. 地球学报,22(5):477-480
17. 刘再华,2001. 对黎廷宇先生等所著“黔中碳酸盐岩和非碳酸盐岩上覆土壤CO2来源的对比研究”一文的商榷. 中国岩溶,20(4):260
18.刘再华,张美良, 游省易,李强,2002. 云南白水台钙华景区的水化学和碳氧同位素特征及其在古环境重建研究中的意义. 第四纪研究,22(5):459-467
19. 刘再华,W. Dreybrodt. 2002. 方解石沉积速率控制的物理化学机制及其古环境重建意义. 中国岩溶,21(4):252-257
20. 李强, 戴亚南, 游省易, 刘再华, 2002. 云南白水台钙华沉积成因及主要沉积类型研究. 中国岩溶,21(3):178-181
21. 戴亚南, 游省易, 李强, 刘再华, 2002. 云南白水台泉华台地旅游业可持续发展浅析. 中国岩溶,21(3):227-232
22. 刘再华,袁道先,何师意, 曹建华, 游省易,W. Dreybrodt,U. Svensson,K. Yoshimura,R. Drysdale, 2003. 四川黄龙沟景区钙华的起源和形成机理研究. 地球化学,32(1):1-10
23. 刘再华,Chris Groves,袁道先,Joe Meiman,姜光辉,何师意, 2003. 水-岩-气相互作用引起的水化学动态变化研究—以桂林岩溶试验为例. 水文地质工程地质,30(4):13-18
24. 游省易,李强, 刘再华, 2003. 云南白水台钙华景区水的物理化学动态变化研究. 中国岩溶,22(2):110-117
25. 戴亚南,刘再华,2003. 响水河钙华形成的水化学特征与碳稳定同位素研究. 热带地理,23(4):324-328
26. 刘再华,张美良,游省易,李强,孙海龙,汪进良,吴孔运, 2004. 碳酸钙沉积溪流中地球化学指标的空间分布和日变化特征—以云南白水台为例. 地球化学, 33(3):269-278
27. 刘再华, 戴亚南, 林玉石,2004. 水化学和钙华碳氧稳定同位素方法在古环境重建中的应用. 第四纪研究,24(4):447-454
28. 刘再华, 李强,汪进良,吴孔运,孙海龙,2004. 桂林岩溶试验场钻孔水化学暴雨动态和垂向变化解译. 中国岩溶, 23(3):169-176
29. 吴孔运,孙海龙,汪进良,刘再华,2004. 重庆金佛山岩溶作用驱动因素初探. 中国岩溶, 23(3):247-252
30. 赵景波; 袁道先; 李胜利; 刘再华, 2004. 陕西长安杨万村黄土岩溶泉研究. 干旱区研究,4:
31. 刘再华, W. Dreybrodt, 韩军, 李华举.2005. CaCO3-CO2-H2O岩溶系统的平衡化学及其分析. 中国岩溶,24(1):1-14
32.刘再华 , K.Yoshimura , Y. Inokura ,M. Noto , 曹云,2005.四川黄龙沟天然水中的深源CO2 与大规模的钙华沉积. 地球与环境, 33(2):1-10
33. 刘再华,李强,孙海龙,汪进良,吴孔运,2005.云南白水台钙华水池中水化学日变化及其生物控制的发现. 水文地质工程地质, 35(6):10-15
34.赵景波; 肖军; 李瑜琴; 岳应利; 刘再华, 2005. 陕西秦岭翠华山泉水化学成分研究. 第四纪研究 5:
35. 刘再华,吴孔运,2006. 外源水中碳酸盐岩侵蚀速率的精确测定及其控制机理研究. 地球化学,35(1):103-110
36. 刘再华,Wolfgang Dreybrodt, 2006. 灰岩和白云岩溶解速率控制机理的比较研究. 地球科学,31(3):411-416
37. 刘再华, 李红春, 游镇烽, 万乃容, 孙海龙,刘香玲,2006. 云南白水台现代内生钙华微层的特征及其古气候重建意义. 地球学报,27(5):479-486
38. 曹云,李红春,刘再华,袁道先,沈立成,2006. 重庆市北温泉与四川康定温泉水之地球化学特征对比. 中国岩溶,25(2):112-120
39. 吕保樱,刘再华(通信作者),廖长君,孙海龙,2006. 水生植物对岩溶水化学日变化的影响——以桂林岩溶水文地质试验场为例. 中国岩溶,25(4):335-340
40.李 强,孙海龙,韩 军,刘再华,余龙江,2006.降水对广西马山兰电堂泉水化学动态变化观测研究.水科学进展,17(5):733-737
41. 姜殿强, 刘再华, 申宏岗, 廖长君,2007.岩溶生态环境条件下不同生境铁皮石斛多糖含量的比较研究.中国岩溶,26(3):226-229
42. 杨 霄, 刘再华(通信作者), 曹建华, 张云鸽,2008.岩溶区和非岩溶区玉米光合作用与锌含量和碳酸酐酶关系的对比研究. 中国岩溶,27(2):103-107.
43. 孙海龙,刘再华(通信作者),吕保樱,叶文炳,刘香玲,曾成,王海静,2008.云南白水台雨水线及钙华δ18O的季节和空间变化特征.地球化学,37(6):542-548
44. 孙海龙,刘再华(通信作者),吕保樱,叶文炳,刘香玲,曾成,王海静,2008.云南白水台现代钙华δ13C的季节和空间变化特征研究. 地球与环境,36(4): 324-329
45. 刘再华,2008. 再论黄龙钙华的成因. 中国岩溶, 27(4):388-390
46. 王海静,刘再华(通信作者),曾成,刘香玲,孙海龙,安德军,唐淑,张清明, 2009.四川黄龙沟源头泉水及其下游溪水的水化学变化研究. 地球化学,38(3):307-314
47. 曾成,赵敏,叶文炳,闫志为,刘彦,蒋丽娟,刘再华(通信作者), 2009.基于谱分析的岩溶地下河系统短时间尺度水化学变化研究——以茂兰自然保护区板寨地下河系统为例.水文地质工程地质, (3): 39-44,50
48. 曾成,刘再华(通信作者),孙海龙,王海静,吕保樱, 2009. 水力坡度对溪流钙华沉积的影响. 地球与环境,37(2):103-110
49. 赵敏,曾成,叶文炳,刘再华(通信作者), 2009. 不同土地利用分布格局下的岩溶泉水化学变化研究. 地球与环境,37(3):214-220
50. 赵敏, 曾成, 刘再华(通信作者), 2009. 不同土地利用对岩溶地下水溶解无机碳及其碳同位素的影响. 地球化学,38(6):565-572
51. 刘再华,孙海龙,张金流,2009. 山西娘子关泉钙华记录的MIS12/11以来的气候和植被历史. 地学前缘(约稿),16(5):99-106
52. 刘再华,田友萍, 安德军,王海静,唐淑,张金流,孙海龙,刘彦,张清明, 2009. 世界自然遗产-四川黄龙钙华景观的形成与演化. 地球学报(创刊30周年特刊约稿), 30(6):841-847
53. 刘彦,刘再华(通信作者), 2010. 卵囊藻对DIC的利用及其对钙离子沉积影响的研究. 地球化学, 39(2):191-196
54. 张金流,刘再华(通信作者),安德军,2010. 世界遗产—四川黄龙钙华景观研究进展与展望. 地球与环境,38(1): 79-84.
55. 熊志斌,令孤克鸿,覃汉标,赵敏,曾成,刘再华,2010.茂兰保护区板寨河头原生林与小七孔卧龙坝次生林物种多样性比较. 贵州科学28 (2 ):60-65.
56. 晏浩,刘再华 (通信作者), 2011. 层状钙华及其地球化学指标的古气候环境意义. 第四纪研究,31(1): 88-95.
57. 曾成, 赵敏, 杨睿, 刘再华, 罗洪远, 2011. 不同土地利用下岩溶水系统水化学日动态强度小波分析. 水文地质工程地质, 38(1): 86-93.
58. 曾成,赵敏,杨睿,刘再华(通信作者), 2011. 高寒冰雪覆盖型和湿润亚热带型岩溶水系统碳汇强度对比. 气候变化研究进展(地质碳汇专刊约稿),7(3):162-170
59. 王海静,张金流,刘再华(通信作者),台永东, 2011. 基于水化学和同位素特征的四川黄龙沟泉群分类研究. 地球学报,32(3):367-372
60. 刘再华, Wolfgang DREYBRODT, 刘洹,2011. 大气CO2汇: 硅酸盐风化还是碳酸盐风化的贡献?第四纪研究(风化碳汇专刊约稿),31(3):426-430
61. 张金流,王海静, 刘再华*,2011. 旅游活动对黄龙景区磷酸盐浓度和水藻生长的影响. 地球学报, 32:463-468
62. 连宾,袁道先,刘再华,2011. 岩溶生态系统中微生物对岩溶作用影响的认识. 科学通报,56:2158 ~ 2161
63. 刘再华,王海静,刘彦,台永东,付如贤,汪孝萍, 2011. 5-12 汶川地震对黄龙世界遗产地源泉水文地球化学的影响¾高分辨率和高精度的水文地球化学监测证据. 中国岩溶,30(3):248-252
64. 张信宝,刘再华,王世杰,陈喜,2011. 锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制. 山地学报 29(5):529-533
65. 刘再华,2011. 岩溶作用及其碳汇强度计算的“入渗-平衡化学法”--兼论水化学径流法和溶蚀试片法. 中国岩溶 30(4):17-20
66. 曾成,赵敏,杨睿,刘再华*,2012. 缺土的板寨原始森林区岩溶地下河系统的水-碳动态特征. 地球科学 37(2): 253-262
67. 赵敏,曾成,杨睿,刘再华*, 2012. 贵州普定灯盏河岩溶泉的硫同位素季节变化特征. 地球科学与环境学报,34(3):83-88
68. 王海静,张金流,刘再华*,2012. 四川黄龙降水氢氧同位素对气候变化的指示意义. 中国岩溶,31(3):253-258
69. 刘再华,2012. 碳酸盐风化碳汇与森林碳汇的对比--碳汇研究思路和方法变革的必要性. 中国岩溶,31(4):1-4
70. 晏浩,刘再华,邓贵平,孙海龙,张金流,2013. 四川九寨沟景区钙华起源初探,中国岩溶, 32(1): 15-22.
71. 孙海龙,刘再华*,晏浩,杨睿,曾成,王海静, 2013. 不同方法萃取的溶解无机碳的δ13C值比较分析. 中国岩溶, 32(1): 117-122.
72. 曾成,刘再华, 2013. 建设岩溶水—碳通量大型模拟试验场的构想. 资源环境与工程 27(2): 196-200.
73. 曾成,赵敏,杨睿,刘再华*,2014. 岩溶作用碳汇强度计算的溶蚀试片法和水化学径流法比较. 水文地质工程地质,41(1):106-111.
74. 陈波, 杨睿, 刘再华*, 晏浩,赵敏, 2014. 水生光合生物对茂兰拉桥泉及其下游水化学和d13CDIC昼夜变化的影响. 地球化学 43(4): 375-385.
75. 李玲珑, 刘再华*, 2015. 洞穴滴水—CaCO3体系氧碳同位素组成的气候意义研究进展和问题. 地球与环境, 43(2): 223-232.
76. 李玲珑,刘再华*,2015.不同植被条件下岩溶地下水δ13CDIC的差异研究—以贵州夜郎洞、天钟洞和普定岩溶水碳通量模拟试验场为例.第四纪研究 35(4):913-921.
77. 朱辉,曾成,刘再华*,曾庆睿,李玲珑, 2015. 岩溶作用碳汇强度变化的土地利用调控规律--普定岩溶水—碳通量大型模拟试验场研究. 水文地质工程地质 42(6):123-128.
78. 曾成,赵敏,杨睿,刘再华*, 2017. 贵州典型岩溶流域水循环驱动的岩溶碳汇通量及其主控因素分析. 地球与环境45:74-83
79. 孙海龙,刘再华*,杨睿,陈波,杨明星,曾庆睿,2017. 珠江流域水化学组成的时空变化特征及对岩石风化碳汇估算的意义. 地球与环境45:57-65
80. 杨明星, 刘再华*, 孙海龙, 杨睿, 陈波, 2017. 基于生物标志物法的珠江流域有机碳溯源及DIC施肥效应研究. 地球与环境 45:46-56
81. 倪健,王世杰,刘再华,闫俊华, 2017. 中国喀斯特碳循环. 地球与环境 45:1
82. 王世杰,刘再华,倪健,闫俊华,刘秀明,2017. 中国南方喀斯特地区碳循环研究进展. 地球与环境 45:2-9