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Volume 40 Issue 4
Aug.  2021
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Article Navigation >  CARSOLOGICA SINICA  > 2021  >  40(4): 580-591
SHI Xiao, YANG Yan, LI Yidong, TIAN Ning, Ye Zhimao, LI Jiancang, DUAN Junwei. Analysis of temporal and spatial variations of CO2 migration in the soil cave system in karst critical zone：A case study of Jiguan cave, western Henan[J]. CARSOLOGICA SINICA, 2021, 40(4): 580-591.
Citation: SHI Xiao, YANG Yan, LI Yidong, TIAN Ning, Ye Zhimao, LI Jiancang, DUAN Junwei. Analysis of temporal and spatial variations of CO2 migration in the soil cave system in karst critical zone：A case study of Jiguan cave, western Henan[J]. CARSOLOGICA SINICA, 2021, 40(4): 580-591.
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Analysis of temporal and spatial variations of CO2 migration in the soil cave system in karst critical zone：A case study of Jiguan cave, western Henan

  • 1.

    Chongqing Key Laboratory of Karst Environment ， School of Geographical Sciences，Southwest University/Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station

  • 2.

    Henan Jiguan Cave Tourism Development Co. ，Ltd

  • Publish Date: 2021-08-25
    Abstract
  • In order to understand the characteristics of CO2 water-soil-gas at different scales in the karst area of Jiguan cave，western Henan，and to explore the relationship of CO2 migration in the karst critical zone system， we used the solid-state sensor method to monitor the change of overlying soil CO2 with high time resolution and collected the data every 15 minutes in Jiguan cave，Henan， from May 2019 to October 2020. Combined with monthly air CO2 data collected in the cave， the chemistry index of cave water， and monitoring data of rainfall and temperature for a systematic and comprehensive analysis，the result showed that，（1）The soil CO2 concentration，the air CO2 collected in the cave，and the chemistry index of cave water had obvious seasonal changes，all of which are high in summer and autumn and low in winter and spring.（2）On the day and night scale，the soil CO2 concentration during the day was higher than that at night.The difference between day and night was the largest in summer and the smallest in winter. The day and night change lagged behind air temperature and soil temperature by about 6 hours.The changes of air CO2 collected in the cave，the concentration of water ions in the cave ，and the chemistry index of cave water were synchronized in the day and night changes.（3）Under the scale of heavy rainfall（single rainfall was 42.2 mm），soil moisture and soil temperature can respond to rainfall changes in time，while the response of soil CO2 changes to rainfall lagged about 2 hours.Changes in cave water and cave CO2 were similar to changes in soil CO2.（4）The correlation coefficients of soil CO2，soil temperature and soil moisture based on monthly average values were 0.67and 0.031，respectively. In the vertical direction，the order of seasonal change of CO2 concentration was soil> cave> atmosphere. The lag of soil CO2 on air temperature and soil temperature day and night was affected by the photosynthesis intensity of the overlying vegetation. CO2 is mainly degassed and deposited in the cave water transportation，replenishing the air CO2 in the cave. During heavy rainfall，soil CO2 is controlled by soil temperature and humidity changes，but is more dominated by soil temperature on a long-term scale，with less soil moisture influences.In order to understand the characteristics of CO2 water-soil-gas at different scales in the karst area of Jiguan cave，western Henan，and to explore the relationship of CO2 migration in the karst critical zone system， we used the solid-state sensor method to monitor the change of overlying soil CO2 with high time resolution and collected the data every 15 minutes in Jiguan cave，Henan， from May 2019 to October 2020. Combined with monthly air CO2 data collected in the cave， the chemistry index of cave water， and monitoring data of rainfall and temperature for a systematic and comprehensive analysis，the result showed that，（1）The soil CO2 concentration，the air CO2 collected in the cave，and the chemistry index of cave water had obvious seasonal changes，all of which are high in summer and autumn and low in winter and spring.（2）On the day and night scale，the soil CO2 concentration during the day was higher than that at night.The difference between day and night was the largest in summer and the smallest in winter. The day and night change lagged behind air temperature and soil temperature by about 6 hours.The changes of air CO2 collected in the cave，the concentration of water ions in the cave ，and the chemistry index of cave water were synchronized in the day and night changes.（3）Under the scale of heavy rainfall（single rainfall was 42.2 mm），soil moisture and soil temperature can respond to rainfall changes in time，while the response of soil CO2 changes to rainfall lagged about 2 hours.Changes in cave water and cave CO2 were similar to changes in soil CO2.（4）The correlation coefficients of soil CO2，soil temperature and soil moisture based on monthly average values were 0.67and 0.031，respectively. In the vertical direction，the order of seasonal change of CO2 concentration was soil> cave> atmosphere. The lag of soil CO2 on air temperature and soil temperature day and night was affected by the photosynthesis intensity of the overlying vegetation. CO2 is mainly degassed and deposited in the cave water transportation，replenishing the air CO2 in the cave. During heavy rainfall，soil CO2 is controlled by soil temperature and humidity changes，but is more dominated by soil temperature on a long-term scale，with less soil moisture influences.

     

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    • References(45)
  • [1]
    袁道先. 岩溶作用对环境变化的敏感性及其记录［J］.科学通报， 1995， 40（13）： 1210-1213.
    [2]
    王世杰， 刘再华， 倪健， 等， 中国南方喀斯特地区碳循环研究进展［J］.地球与环境， 2017， 45（1）： 2-9.
    [3]
    马明国， 汤旭光， 韩旭军， 等， 西南岩溶地区碳循环观测与模拟研究进展和展望［J］.地理科学进展， 2019，38（8）： 1196-1205.
    [4]
    Jobbagy E G， Jackson R B. The vertical distribution of soil organic carbon and its relation to climate and vegetation［J］.Ecological Applications， 2000， 10（2）： 423-436.
    [5]
    Raich J W， Potter C S. Global Patterns of Carbon-Dioxide Emissions from Soils［J］.Global Biogeochemical Cycles， 1995， 9（1）： 23-36.
    [6]
    Rosenzweig C， Hillel D. Soils and global climate change： Challenges and opportunities［J］.Soil Science， 2000， 165（1）： 47-56.
    [7]
    张绍云， 周忠发， 殷超， 等， 喀斯特地区土壤-洞穴CO2时空迁移变化特征［J］.土壤通报， 2016， 47（5）： 1238-1244.
    [8]
    殷超， 周忠发， 田衷珲， 等，土壤CO2与喀斯特洞穴CO2季节变化响应分析［J］.水土保持学报，2017，31（4）：304-310，317.
    [9]
    Yuan D X， Zhang C. Karst Processes and the Carbon Cycle： Final Report of IGCP 379.Geological Publishing House， 2002： 3-4.
    [10]
    蓝芙宁， 王文娟， 吴华英， 等. 不同土地利用方式下土壤CO2时空分布特征及其影响因素：以湘西大龙洞地下河流域为例［J］.中国岩溶， 2017， 36（4）： 427-432.
    [11]
    梁福源， 宋林华， 王静. 土壤CO2浓度昼夜变化及其对土壤CO2排放量的影响［J］.地理科学进展， 2003（2）： 170-176.
    [12]
    赵景波， 袁道先， 马占武， 等. 西安地区4-5月份土壤CO2释放规律研究［J］.中国岩溶， 2000，19（4）： 19-23.
    [13]
    Zimmermann M， Meir P， Bird M， et al. Litter contribution to diurnal and annual soil respiration in a tropical montane cloud forest［J］.Soil Biology & Biochemistry， 2009. 41（6）： 1338-1340.
    [14]
    Liu Z H， Dreybrodt W. Significance of the carbon sink produced by H2O-carbonate-CO2-aquatic phototroph interaction on land［J］.Science Bulletin， 2015， 60（2）： 182-191.
    [15]
    郭小娇， 龚晓萍， 汤庆佳， 等. 典型岩溶山坡土壤剖面水分对降雨响应过程研究［J］.中国岩溶， 2016， 35（6）： 629-638.
    [16]
    张川， 张伟， 陈洪松， 等. 喀斯特典型坡地旱季表层土壤水分时空变异性［J］.生态学报， 2015，35（19）： 6326-6334.
    [17]
    颜蒙蒙， 周洲， 王济， 等. 喀斯特地区土壤水分随降雨的动态变化研究：以贵阳市花溪区为例［J］.中国岩溶， 2016， 35（4）： 446-452.
    [18]
    夏发生， 王益权， 刘军， 等. （土娄）土剖面CO2释放通量的变异特征［J］.干旱地区农业研究， 2010， 28（1）： 117-121，135.
    [19]
    吴韦， 贾亚男， 蒋勇军， 等. 典型岩溶槽谷区土壤CO2浓度变化对隧道建设的响应：以重庆市中梁山岩溶槽谷为例［J］.生态学报， 2019， 39（16）： 6146-6157.
    [20]
    李光超， 曹建华， 张会， 等. 典型岩溶区板栗树下土壤CO2迁移动态研究：以广西隆安县岩溶区为例［J］.安徽农业科学， 2015，43（9）： 318-320，370.
    [21]
    蓝芙宁， 王文娟， 覃小群， 等. 土地利用和覆被变化对岩溶区土壤CO2浓度的影响［J］.中国岩溶， 2011，30（4）： 449-455.
    [22]
    冯天骄， 卫伟， 陈利顶， 等. 黄土丘陵区小流域不同整地措施长期影响下的土壤水力学特性［J］.环境科学， 2017，38（9）： 3860-3870.
    [23]
    Sheng H， Yang Y S， Yang Z J， et al. The dynamic response of soil respiration to land-use changes in subtropical China.Global Change Biology， 2010， 16（3）： 1107-1121.
    [24]
    王静， 宋林华， 向昌国， 等.不同植被类型覆盖下土壤CO2浓度对洞穴景观的影响［J］.地理研究， 2004，23（1）： 71-77.
    [25]
    黄芬， 吴夏， 杨慧， 等. 桂林毛村地下河流域岩溶关键带碳循环研究［J］.广西科学， 2018，25（5）： 515-523.
    [26]
    吴泽燕， 章程， 蒋忠诚， 等.岩溶关键带及其碳循环研究进展［J］.地球科学进展， 2019，34（5）： 488-498.
    [27]
    张萍， 杨琰， 孙喆， 等. 河南鸡冠洞CO2季节和昼夜变化特征及影响因子比较［J］.环境科学， 2017， 38（1）： 60-69.
    [28]
    田宁， 杨琰， 袁海英， 等. 鸡冠洞CO2和222Rn变化特征以及与旅游活动关系研究［J］.地球与环境，2020，48（2）：210-219.
    [29]
    任小凤， 杨琰， 彭涛， 等， 豫西鸡冠洞洞穴水及现代沉积物Mg，Sr和Ba记录及其意义［J］.中国岩溶，2014，33（1）：57-63.
    [30]
    梁沙， 杨琰， 张娜， 等，岩溶关键带微量元素运移的时空变化：以豫西鸡冠洞为例［J］.环境科学，2017，38（10）：4130-4140.
    [31]
    游贤慧， 杨琰， 徐刚， 等， 喀斯特槽谷区土壤CO2浓度的短时变化及影响因素研究［J］.地球与环境，2019， 47（1）：16-25.
    [32]
    Ferlan， Mitja， Ogrinc， et al. Soil CO2 sources above a subterranean cave-Pisani rov （Postojna Cave， Slovenia）［J］. Journal of soil & sediments， 2017， 17：1883-1892.
    [33]
    王世岩，杨永兴，杨波.三江平原典型湿地土壤温度变化及其影响因子分析［J］.地理研究，2003（3）：389-396.
    [34]
    张慧智，史学正，于东升，等.中国土壤温度的季节性变化及其区域分异研究［J］.土壤学报，2009，46（2）：227-234.
    [35]
    付皓宇，井长青，郭文章，等.准噶尔盆地南缘荒漠草地土壤温、湿度分层变化特征［J］.草业科学，2020，37（6）：1035-1046.
    [36]
    AlvalóR C S， Gielow R， da Rocha H R， et al. Intradiurnal and seasonal variability of soil temperature， heat flux， soil moisture content， and thermal properties under forest and pasture in Rondnia［J］. Journal of Geophysical Research： Atmospheres， 2002， 107（D20）： LBA-1- LBA 10-20.
    [37]
    宋长春，王毅勇.湿地生态系统土壤温度对气温的响应特征及对CO2排放的影响［J］.应用生态学报，2006（4）：4625-4629.
    [38]
    Zheng D ， Hunt E R ， Running S W . A daily soil temperature model based on air temperature and precipitation for continental applications［J］. Journal of Applied Entomology， 1993， 123（2）：183-191.
    [39]
    Barron‐Gafford G A， Scott R L，Jenerrette G D， et al. The relative controls of temperature， soil moisture， and plant functional group on soil CO2 efflux at diel， seasonal， and annual scales［J］. Journal of Geophysical Research： Biogeosciences， 2011， 116，G01023.
    [40]
    Savage K， Davidson E A， Tang J. Diel patterns of autotrophic and heterotrophic respiration among phenological stages［J］. Global Change Biology， 2013， 19（4）：1151-1159.
    [41]
    Chen D， Molina J A E， Clapp C E， et al. Corn Root Influence on Automated Measurement of Soil Carbon Dioxide Concentrations［J］. Soil Science， 2005， 170（10）：779-787.
    [42]
    Jassal R S ， Black T A ， Drewitt G B ， et al. A model of the production and transport of CO2 in soil： predicting soil CO2 concentrations and CO2 efflux from a forest floor［J］. Agricultural & Forest Meteorology， 2004， 124（3）：219-236.
    [43]
    赵瑞一， 吕现福， 蒋建建， 等， 土壤CO2及岩溶碳循环影响因素综述［J］.生态学报.2015， 35（13）： 4257-4264.
    [44]
    张红星， 王效科， 冯宗炜， 等. 干湿交替格局下黄土高原小麦田土壤呼吸的温湿度模型［J］.生态学报，2009， 29（6）：028-3035.
    [45]
    周小平， 王效科， 张红星， 等. 黄土高原小麦田土壤呼吸季节和年际变化［J］.生态学报， 2013， 33（23）： 7525-7536.
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