Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China

HOU Manfu; LIU Yuting; ZHANG Jie; HE Luyan; LIANG Jiangyi

doi:10.11932/karst2023y010

Volume 42 Issue 4

Nov. 2023

Turn off MathJax

Article Contents

Article Navigation > CARSOLOGICA SINICA > 2023 > 42(4): 842-852

HOU Manfu, LIU Yuting, ZHANG Jie, HE Luyan, LIANG Jiangyi. Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China[J]. CARSOLOGICA SINICA, 2023, 42(4): 842-852. doi: 10.11932/karst2023y010

Citation:

HOU Manfu, LIU Yuting, ZHANG Jie, HE Luyan, LIANG Jiangyi. Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China[J]. CARSOLOGICA SINICA, 2023, 42(4): 842-852. doi: 10.11932/karst2023y010

Citation:

HOU Manfu, LIU Yuting, ZHANG Jie, HE Luyan, LIANG Jiangyi. Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China[J]. CARSOLOGICA SINICA, 2023, 42(4): 842-852. doi: 10.11932/karst2023y010

PDF( 1574 KB)

Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China

doi: 10.11932/karst2023y010

HOU Manfu^{1, 2
,},
LIU Yuting^{1, 2},
ZHANG Jie³,
HE Luyan^{1, 4},
LIANG Jiangyi¹

1.
College of Environment and Resources, Guangxi Normal University, Guilin, Guangxi 541004, China
2.
Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection, Ministry of Education(Guangxi Normal University), Guiling, Guangxi 541004, China
3.
School of Geography and Resource Science of Neijiang Normal University, Neijiang, Sichuang 641100, China
4.
Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, Jilin 130102, China

Received Date: 2022-04-19
Available Online: 2023-03-07

Abstract

Abstract

Carbonate rock weathering has great carbon sink potential. Vegetation is an important driven factor of carbonate rock dissolution. However, the relationship between vegetation types and carbonate weathering is still left unknown. In order to reveal the effects of forest types on carbonate rock weathering, the dissolution rates of carbonate rocks at different slope positions in two typical subtropical karst forests were compared in details based on the in-situ dissolution tests of standard rock test pieces, and the corresponding relationship between the rates and soil CO₂ content (pCO₂) and soil water content (SWC) were analyzed based on seasonal measured data.The study area is located in the suburb of Guilin, South China, which has a subtropical seasonal climate with an average annual temperature of 20.2 ℃ and an average annual precipitation of 1,996.0 mm. Precipitation is concentrated from April to September, synchronous with the high temperature in summer. The landforms of peak cluster depressions and peak forest plain around the study area are the most typical in the world and were added to the UNESCO's World Heritage List in 2014. Stretching from the foot to the place near the peak of limestone hills, Cycolobalanopses glauca forest and Platycarya strobilacea forest, the representatives of subtropical karst forests, were selected as research objects in the study area. The community dominated by C. glauca is widely distributed in the karst region of N25°-N31° and E105°-E120°, and is the most important climax community in the subtropical karst region of China. P. strobilacea is one of the most common dominant species or constructive species in evergreen and deciduous broad-leaved forests, forming a more widely distributed forest type than C. glauca forest in the subtropical karst area.Standard rock test pieces were respectively placed in the air 100 cm above ground, on the surface of soil, -20 cm, -50 cm, and -70 cm (if possible) in the soil of downhill slope, middle hill slope and uphill slope from 30/11/2014 to 17/12/2017 in each forest type. The soil pCO₂ and SWC of each test place were measured seasonally.The results show that the dissolution rate of carbonate rock in C. glauca forest (5.22 ± 0.99 mg·cm⁻²·a⁻¹) was significantly higher than that in P. strobilacea forest (3.58 ± 2.59 mg·cm⁻²·a⁻¹). In vertical profile, the dissolution rate under soil experienced a decrease after an increase, peaking at 20 cm below ground in C. glauca forest while the rate kept rising with the increase of soil depth in P. strobilacea forest. The differential of dissolution rates did not show consistency at different slope positions of the two forest types. There was no significant difference in rates at three slope positions in C. glauca forest, but the rate was significantly higher on the middle slope than those on the upper and down slopes in P. strobilacea forest. The dissolution rates of the two forests well corresponded to their SWC, but were opposite with their soil pCO₂. The dissolution rates at different slope positions and in vertical profiles well corresponded to soil pCO₂.There are significant differences in dissolution rates among different forest types in the subtropical karst area, which can be explained by SWC. There is not a consistent pattern on dissolution rates of slope positions between the two forest types, but their differences could be explained by soil pCO₂. Our results highlight the importance of distinguishing the influence of community types, their SWC and soil pCO₂ on dissolution rates of carbonate rock in the subtropical karst area.
- standard tablet,
- carbonate weathering,
- dissolution rate,
- forest type,
- carbon sink

FullText(HTML)

References(47)

References

[1]	Yuan Daoxian, Zhu Dehao, Weng Jintao, Zhu Xuewen, Han Xingrui, Wang Xunyi, Cai Guihong, Zhu Yuanfeng, Cui Guangzhong, Deng Ziqiang. Karst of China[M]. Beijing: Geological Publishing House, 1991.
[2]	Liu Z H, Dreybrodt W, Wang H J. 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[J]. Earth-Science Reviews, 2010, 99:162-172. doi: 10.1016/j.earscirev.2010.03.001
[3]	Liu Z H, Macpherson G L, Groves C, Martin J B, Yuan D X, Zeng S B. Large and active CO₂ uptake by coupled carbonate weathering[J]. Earth-Science Reviews, 2018, 182:42-49. doi: 10.1016/j.earscirev.2018.05.007
[4]	Cao J H, Wu X, Huang F, Hu B, Groves C, Yang H, Zhang C L. Global significance of the carbon cycle in the karst dynamic system: Evidence from geological and ecological processes[J]. China Geology, 2018, 1:17-27. doi: 10.31035/cg2018004
[5]	刘再华, 何师意, 袁道先, 赵景波. 土壤中的CO₂及其对岩溶作用的驱动[J]. 水文地质工程地质, 1998, 34(4):42-45. LIU Zaihua, HE Shiyi, YUAN Daoxian, ZHAO Jingbo. CO₂ in soil and its drive to karstification[J]. Hydrogeology & Engineering Geology, 1998, 34(4):42-45.
[6]	何师意, 徐胜友, 张美良. 岩溶土壤中CO₂浓度, 水化学观测及其与岩溶作用关系[J]. 中国岩溶, 1997, 16(4):319-324. HE Shiyi, XU Shengyou, ZHANG Meiliang. Observation on soil CO₂ concentration, hydrochemistry, and their relationship with karst processes[J]. Carsologica Sinica, 1997, 16(4):319-324.
[7]	徐胜友, 何师意. 碳酸盐岩土壤CO₂的动态特征及其对溶蚀作用的驱动[J]. 中国岩溶, 1996, 15(Supp.1):50-57. XU Shengyou, HE Shiyi. The CO₂ regime of soil profile and its drive to dissolution of carbonate rock[J]. Carsologica Sinica, 1996, 15(Supp.1):50-57.
[8]	邵明玉, 张连凯, 刘朋雨, 覃小群, 邵天杰, 曹建华, 张春来. 夏季黄土丘陵区不同土地利用方式土壤CO₂分布特征及影响因素[J]. 中国岩溶, 2019, 38(1):70-79. SHAO Mingyu, ZHANG Liankai, LIU Pengyu, QIN Xiaoqun, SHAO Tianjie, CAO Jianhua, ZHANG Chunlai. Distribution characteristics and influencing factors of soil CO₂ in different land use patterns in loess hilly region in summer[J]. Carsologica Sinica, 2019, 38(1):70-79.
[9]	赵瑞一, 吕现福, 蒋建建, 段逸凡. 土壤CO₂及岩溶碳循环影响因素综述[J]. 生态学报, 2015(13):4257-4264. ZHAO Ruiyi, LV Xianfu, JIANG Jianjian, DUAN Yifan. Factors affecting soil CO₂ and karst carbon cycle[J]. Acta Ecologica Sinica, 2015(13):4257-4264.
[10]	施晓, 杨琰, 李一冬, 田宁, 叶枝茂, 李建仓, 段军伟. 岩溶关键带土壤–洞穴系统CO₂运移的时空变化:以河南鸡冠洞为例[J]. 中国岩溶, 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.
[11]	蓝芙宁, 王文娟, 吴华英, 蒋忠诚, 覃小群, 安树青. 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. LAN Funing, WANG Wenjuan, WU Huaying, JIANG Zhongcheng, QIN Xiaoqun, AN Shuqing. Temporal and spatial distributions of CO₂ in soil and their influencing factors under different LUCC: A case study of the Dalongdong underground river drainage area[J]. Carsologica Sinica, 2017, 36(4):427-432.
[12]	Romero Mujalli G, Hartmann J, Börker J, Gaillardet J, Calmels D. Ecosystem controlled soil-rock pCO₂ and carbonate weathering–constraints by temperature and soil water content[J]. Chemical Geology, 2019, 527:118634. doi: 10.1016/j.chemgeo.2018.01.030
[13]	曹建华, 袁道先, 潘根兴, 姜光辉. 不同植被下土壤碳转移对岩溶动力系统中碳循环的影响[J]. 地球与环境, 2004, 32(1):90-96. doi: 10.3969/j.issn.1672-9250.2004.01.016 CAO Jianhua, YUAN Daoxian, PAN Genxing, JIANG Guanghui. Influence of soil carbon transfer under different vegetations on carbon cycle of karst dynamics system[J]. Earth and Environment, 2004, 32(1):90-96. doi: 10.3969/j.issn.1672-9250.2004.01.016
[14]	Berner R A. Weathering, plants, and the long-term carbon cycle[J]. Geochimica et Cosmochimica Acta, 1992, 56:3225-3231. doi: 10.1016/0016-7037(92)90300-8
[15]	李恩香, 蒋忠诚, 曹建华, 姜光辉, 邓艳. 广西弄拉岩溶植被不同演替阶段的主要土壤因子及溶蚀率对比研究[J]. 生态学报, 2004, 24(6):1131-1139. doi: 10.3321/j.issn:1000-0933.2004.06.006 LI Enxiang, JIANG Zhongcheng, CAO Jianhua, JIANG Guanghui, DENG Yan. The comparison of properties of karst soil and karst erosion ratio under different successional stages of karst vegetation in Nongla, Guangxi[J]. Acta Ecologica Sinica, 2004, 24(6):1131-1139. doi: 10.3321/j.issn:1000-0933.2004.06.006
[16]	章程. 不同土地利用下的岩溶作用强度及其碳汇效应[J]. 科学通报, 2011, 56(26):2174-2180.
[17]	王冬银, 章程, 谢世友, 杨平恒, 张文晖. 亚高山不同植被类型区的雨季岩溶溶蚀速率研究[J]. 地球学报, 2007, 28(5):488-495. doi: 10.3321/j.issn:1006-3021.2007.05.011 WANG Dongyin, ZHANG Cheng, XIE Shiyou, YANG Pingheng, ZHANG Wenhui. Karst dissolution rates of areas with different vegetation types in the sub-mountain region[J]. Acta Geoscientica Sinica, 2007, 28(5):488-495. doi: 10.3321/j.issn:1006-3021.2007.05.011
[18]	柯静, 邓艳, 岳祥飞, 梁锦桃, 李旭尧, 曹建华, 吴松. 典型岩溶断陷盆地溶蚀速率对海拔高度和土地利用方式的响应[J]. 地球学报, 2021, 42(3):407-416. KE Jing, DENG Yan, YUE Xiangfei, LIANG Jintao, LI Xuyao, CAO Jianhua, WU Song. The response of the karst dissolution rate to altitude and land use types in typical karst faulted basin[J]. Acta Geoscientica Sinica, 2021, 42(3):407-416.
[19]	章程, 李玉辉, 汪进良, 苗迎, 肖琼, 郭永丽. 云南石林地质公园土岩、土根界面过程和土下溶蚀速率[J]. 地质论评, 2020, 66(4):1019-1030. ZHANG Cheng, LI Yuhui, WANG Jinliang, MIAO Ying, XIAO Qiong, GUO Yongli. Interface processes at soil-rock, soil-root contacts and subsoil dissolution rate in Shilin Geopark, Yunnan[J]. Geological Review, 2020, 66(4):1019-1030.
[20]	刘文, 张强, 贾亚男. 气象要素及土壤理化性质对不同土地利用方式下冬夏岩溶作用的影响[J]. 生态学报, 2014, 34(6):1418-1428. LIU Wen, ZHANG Qiang, JIA Ya'nan. The influence of meteorological factors and soil physicochemical properties on karst processes in six land-use patterns in summer and winter in a typical karst valley[J]. Acta Ecologica Sinica, 2014, 34(6):1418-1428.
[21]	王冬银, 谢世友, 章程. 典型岩溶区不同土地利用方式下雨季、旱季岩溶作用研究[J]. 生态环境学报, 2009, 18(6):2366-2372. WANG Dongyin, XIE Shiyou, ZHANG Cheng. Impact of land-use patterns upon karst processes in typical karst regions of Jinfo Mountain[J]. Ecology and Environmental Sciences, 2009, 18(6):2366-2372.
[22]	侯满福, 覃小群, 黄奇波, 邓艳, 刘朋雨. 半干旱岩溶区油松林显著促进碳酸盐岩溶蚀[J]. 地球学报, 2022, 43(4):472-482. doi: 10.3975/cagsb.2022.030101 HOU Manfu, QIN Xiaoqun, HUANG Qibo, DENG Yan, LIU Pengyu. Pinus tabuliformis forests in semi-arid areas significantly enhance carbonate rock dissolution[J]. Acta Geoscientica Sinica, 2022, 43(4):472-482. doi: 10.3975/cagsb.2022.030101
[23]	方精云, 王襄平, 沈泽昊, 唐志尧, 贺金生, 于丹, 江源, 王志恒, 郑成洋, 朱江玲. 植物群落清查的主要内容, 方法和技术规范[J]. 生物多样性, 2009, 17(6):533-548. doi: 10.3724/SP.J.1003.2009.09253 FANG Jingyun, WANG Xiangping, SHEN Zehao, TANG Zhiyao, HE Jinsheng, YU Dan, JIANG Yuan, WANG Zhiheng, ZHENG Chengyang, ZHU Jiangling. Methods and protocols for plant community inventory[J]. Biodiversity Science, 2009, 17(6):533-548. doi: 10.3724/SP.J.1003.2009.09253
[24]	Krklec K, Domínguez-Villar D, Perica D. Use of rock tablet method to measure rock weathering and landscape denudation[J]. Earth-Science Reviews, 2021, 212:103449. doi: 10.1016/j.earscirev.2020.103449
[25]	黄奇波, 覃小群, 刘朋雨, 唐萍萍. 北方不同植被下土壤岩石试片的溶蚀速率及碳汇分析:以山西汾阳地区为例[J]. 中国岩溶, 2013, 32(3):258-265. HUANG Qibo, QIN Xiaoqun, LIU Pengyu, TANG Pingping. Analysis on tablets dissolution rate and carbon sink under different vegetation in North China karst area: A case study of Fenyang, Shanxi Province[J]. Carsologica Sinica, 2013, 32(3):258-265.
[26]	姜鑫, 黄先飞, 秦樊鑫, 张珍明. 不同土地利用方式下喀斯特地区岩石溶蚀速率及其驱动因素[J]. 云南农业大学学报(自然科学), 2020, 35(5):899-905. JIANG Xin, HUANG Xianfei, QIN Fanxin, ZHANG Zhenming. Rock dissolution rate and soil properties of karst soil under different land use ways[J]. Journal of Yunnan Agricultural University (Natural Science), 2020, 35(5):899-905.
[27]	Zhou Y C, Wang S J, Lu H M, Xie L P, Xiao D A. Forest soil heterogeneity and soil sampling protocols on limestone outctops: Example from SW China[J]. Acta Carsologica, 2010, 29:115-122.
[28]	周宁, 刘波. 鄂西南岩溶地区表层岩溶带发育强度变化规律研究[J]. 中国岩溶, 2009, 28(1):1-6. ZHOU Ning, LIU Bo. Varying regulation of epikarst developing intensity in southwest Hubei karst area[J]. Carsologica Sinica, 2009, 28(1):1-6.
[29]	Wang C W, Li W, Shen T M, Cheng W L, Yan Z, Yu L J. Influence of soil bacteria and carbonic anhydrase on karstification intensity and regulatory factors in a typical karst area[J]. Geoderma, 2018, 313:17-24. doi: 10.1016/j.geoderma.2017.10.016
[30]	黄其成, 马姜明. 桂林岩溶石山“风水林”植物群落数量分类与排序[J]. 西北植物学报, 2015, 35(11):2324-2330. doi: 10.7606/j.issn.1000-4025.2015.11.2324 HUANG Qicheng, MA Jiangming. Classification and ordination of Fengshui Woods on karst hills of Guilin[J]. Acta Botanica Boreali-Occidentalia Sinica, 2015, 35(11):2324-2330. doi: 10.7606/j.issn.1000-4025.2015.11.2324
[31]	巩书华, 朱丽芬. 湘西北地质地貌特征对岩溶石漠化影响研究:以张家界市为例[J]. 中国岩溶, 2021, 40(3):504-512. GONG Shuhua, ZHU Lifen. Influence of geological and geomorphologic features on karst rocky desertification in northwestern Hunan Province: A case study of Zhangjiajie City[J]. Carsologica Sinica, 2021, 40(3):504-512.
[32]	盘远方, 陈兴彬, 姜勇, 梁士楚, 陆志任, 黄宇欣, 倪鸣源, 覃彩丽, 刘润红. 桂林岩溶石山灌丛植物叶功能性状和土壤因子对坡向的响应[J]. 生态学报, 2018, 38(5):1581-1589. PAN Yuanfang, CHEN Xingbin, JIANG Yong, LIANG Shichu, LU Zhiren, HUANG Yuxin, NI Mingyuan, QIN Caili, LIU Runhong. Changes in leaf functional traits and soil environmental factors in response to slope gradient in karst hills of Guilin[J]. Acta Ecologica Sinica, 2018, 38(5):1581-1589.
[33]	王轶浩, 王彦辉, 谢双喜, 于澎涛, 熊伟, 郝佳. 六盘山小流域地形, 植被特征与土壤水文物理性质的关系[J]. 生态学杂志, 2012, 31(1):145-151. WANG Yihao, WANG Yanhui, XIE Shuangxi, YU Pengtao, XIONG Wei, HAO Jia. Relationships of landform and vegetation characters with soil hydrophysical properties in a small watershed of Liupan Mountains, Northwest China[J]. Chinese Journal of Ecology, 2012, 31(1):145-151.
[34]	闫伟, 曾成, 肖时珍, 蓝家程, 代林玉, 邰治钦, 何江湖, 何春, 狄永宁. 湿润亚热带典型白云岩流域不同土地利用下的试片溶蚀速率及岩溶碳汇[J]. 地球与环境, 2021, 49(5):529-538. YAN Wei, ZENG Cheng, XIAO Shizhen, LAN Jiacheng, DAI Linyu, TAI Zhiqin, HE Jianghu, HE Chun, DI Yongning. Dissolution rate and karst carbon sink of different land use in typical dolomite watershed with humid subtropical weather[J]. Earth and Environment, 2021, 49(5):529-538.
[35]	张鹏飞, 王融融, 戴燕燕, 李强, 马延东, 赵景波. 山西榆次不同植被土壤水分有效性与干燥化效应[J]. 水土保持研究, 2022, 29(5):192-198. doi: 10.3969/j.issn.1005-3409.2022.5.stbcyj202205027 ZHANG Pengfei, WANG Rongrong, DAI Yanyan, LI Qiang, MA Yandong, ZHAO Jingbo. Soil moisture availability and soil desiccation under different vegetation conditions in Yuci, Shanxi[J]. Research of Soil and Water Conservation, 2022, 29(5):192-198. doi: 10.3969/j.issn.1005-3409.2022.5.stbcyj202205027
[36]	孙平安, 肖琼, 郭永丽, 苗迎, 王奇岗, 章程. 混合岩溶流域碳酸盐岩溶蚀速率与岩溶碳汇:以漓江流域上游为例[J]. 中国岩溶, 2021, 40(5):825-834. SUN Ping'an, XIAO Qiong, GUO Yongli, MIAO Ying, WANG Qigang, ZHANG Cheng. Carbonate dissolution rate and karst carbon sink in mixed carbonate and silicate terrain: Take the upper reaches of the Lijiang river basin as an example[J]. Carsologica Sinica, 2021, 40(5):825-834.
[37]	李涛, 赵东兴, 张美良, 曹建华, 朱晓燕. 土壤CO₂、土壤水的动态特征及其对岩溶作用的驱动[J]. 热带地理, 2013, 33(5): 575-581. LI Tao, ZHAO Dongxing, ZHANG Meiliang, CAO Jianhua, ZHU Xiaoyan. Dynamic characteristics of the soil CO₂ and soil water chemistry, and their driving action on karstification[J]. Tropical Geography, 2013, 33(5): 575-581.
[38]	刘文, 张强, 贾亚男. 夏季不同土地利用方式下的溶蚀作用研究:以重庆青木关岩溶槽谷区为例[J]. 中国岩溶, 2012, 31(1):1-6. LIU Wen, ZHANG Qiang, JIA Ya'nan. Karstification under different land-use patterns in summer: A case study in the Qingmuguan karst velley, Chongqing[J]. Carsologica Sinica, 2012, 31(1):1-6.
[39]	Wu Z Y, Zhang C, Jiang Z C, Luo W Q, Xiao Q, Hu Z X, Wu H Y. Subsoil carbonate dissolution rates and their determining factors in a karst drainage basin, SW China[J]. Environmental Earth Sciences, 2020, 79(22):508. doi: 10.1007/s12665-020-09255-1
[40]	高宗军, 张洪英, 李伟, 刘新刚, 韩宝莹, 时孟杰, 牟林凯. 土壤CO₂浓度变化特征及其水文地质意义研究[J]. 地下水, 2017, 39(3):136-139. GAO Zongjun, ZHANG Hongying, LI Wei, LIU Xingang, HAN Baoying, SHI Mengjie, MOU Linkai. Analysis of vertical profiles of soil CO₂ with different depths and its hydro-geological significance[J]. Ground Water, 2017, 39(3):136-139.
[41]	王根绪, 夏军, 李小雁, 杨达, 胡兆永, 孙守琴, 孙向阳. 陆地植被生态水文过程前沿进展:从植物叶片到流域[J]. 科学通报, 2021, 66(28-29):3667-3683. doi: 10.1360/TB-2020-1339 WANG Genxu, XIA Jun, LI Xiaoyan, YANG Da, HU Zhaoyong, SUN Shouqin, SUN Xiangyang. Critical advances in understanding ecohydrological processes of terrestrial vegetation: From leaf to watershed scale[J]. Chinese Science Bulletin, 2021, 66(28-29):3667-3683. doi: 10.1360/TB-2020-1339
[42]	Wen H, Sullivan P L, Macpherson G L, Billings S A, Li L. Deepening roots can enhance carbonate weathering by amplifying CO₂-rich recharge[J]. Biogeosciences, 2021, 18(1):55-75. doi: 10.5194/bg-18-55-2021
[43]	邓艳, 蒋忠诚, 徐烨, 岳祥飞, 李旭尧, 梁锦桃. 典型表层岩溶泉域植被对降雨的再分配研究[J]. 中国岩溶, 2018, 37(5):714-721. DENG Yan, JIANG Zhongcheng, XU Ye, YUE Xiangfei, LI Xuyao, LIANG Jintao. Redistribution of precipitation by vegetation and its ecohydrological effects in a typical epikarst spring catchment[J]. Carsologica Sinica, 2018, 37(5):714-721.
[44]	王世杰, 刘再华, 倪健, 闫俊华, 刘秀明. 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. doi: 10.14050/j.cnki.1672-9250.2017.01.001 WANG Shijie, LIU Zaihua, NI Jian, YAN Junhua, LIU Xiuming. A review of research progress and future prospective of carbon cycle in karst area of South China[J]. Earth and Environment, 2017, 45(1):2-9. doi: 10.14050/j.cnki.1672-9250.2017.01.001
[45]	罗美, 周运超, 唐凤华. 不同植被下碳酸盐岩石发育形成土壤属性研究[J]. 中国岩溶, 2023, 42(2): 277-289. LUO Mei, ZHOU Yunchao, TANG Fenghua. Soil properties of carbonate rocks under different vegetation types[J]. Carsologica Sinica, 2023, 42(2): 277-289.
[46]	龙健, 吴求生, 李娟, 廖洪凯, 刘灵飞, 黄博聪, 张菊梅. 贵州茂兰喀斯特森林不同小生境类型对岩石溶蚀的影响[J]. 土壤学报, 2021, 58(1):151-161. doi: 10.11766/trxb201911040354 LONG Jian, WU Qiusheng, LI Juan, LIAO Hongkai, LIU Lingfei, HUANG Bocong, ZHANG Jumei. Effects of different microhabitat types on rock dissolution in Maolan karst forest, Southwest China[J]. Acta Pedologica Sinica, 2021, 58(1):151-161. doi: 10.11766/trxb201911040354
[47]	张川, 陈洪松, 张伟, 聂云鹏, 叶莹莹, 王克林. 喀斯特坡面表层土壤含水量、容重和饱和导水率的空间变异特征[J]. 应用生态学报, 2014, 25(6):1585-1591. ZHANG Chuan, CHEN Hongsong, ZHANG Wei, NIE Yunpeng, YE Yingying, WANG Kelin. Spatial variation characteristics of surface soil water content, bulk density and saturated hydraulic conductivity on karst slopes[J]. Chinese Journal of Applied Ecology, 2014, 25(6):1585-1591.

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF(1574.0KB)

XML

Article Metrics

Article views (1409) PDF downloads(61)

Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China

doi: 10.11932/karst2023y010

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Influence of forest types and slope positions on dissolution rates of carbonate rocks in the karst area in subtropical China

doi: 10.11932/karst2023y010

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Export File

Citation

Format

Content