详细信息
Mosses and cyanobacteria increased soil moisture and alleviated soil dehydration caused by dry-wet alternation in subtropical humid region ( SCI-EXPANDED收录)
文献类型:期刊文献
英文题名:Mosses and cyanobacteria increased soil moisture and alleviated soil dehydration caused by dry-wet alternation in subtropical humid region
作者:Zi, Ruyi[1] Han, Zhen[1,4] Fang, Qian[1] Yin, Xiaoai[1] Fang, Fayong[1] Qian, Xiaohe[1] Li, Sheng[3,4] Zhao, Longshan[1,2,4]
第一作者:Zi, Ruyi
通信作者:Zhao, LS[1]
机构:[1]Guizhou Univ, Coll Forestry, Guiyang 550025, Guizhou, Peoples R China;[2]Guizhou Univ, Key Lab Karst Georesources & Environm, Minist Educ, Guiyang 500025, Peoples R China;[3]Chinese Acad Forestry, Res Inst Subtrop Forestry, Fuyang 311400, Zhejiang, Peoples R China;[4]Guizhou Puding Rocky Desertificat Ecosyst Natl Obs, Puding 562100, Peoples R China
年份:2026
卷号:264
外文期刊名:CATENA
收录:;Scopus(收录号:2-s2.0-105028003627);WOS:【SCI-EXPANDED(收录号:WOS:001664925800001)】;
基金:This work was supported by the National Natural Science Foundation of China (42577378, 42367045) , the Guizhou Provincial High-level Innovative Talents Project (QKHPTRC-GCC [2023] 015) , and Basic research project of Guizhou University (GUI DA Foundation [2024] 23) .
语种:英文
外文关键词:Moss; Cyanobacteria; Eco-hydrological functions; Soil moisture; Dry-wet alternation; Subtropical humid region
摘要:Mosses and cyanobacteria are multifunctional communities that regulate the eco-hydrological functions of soil and are increasingly recognized as promising, sustainable resources for restoring degraded ecosystems. However, current knowledge regarding the effects of mosses and cyanobacteria on eco-hydrological processes in degraded karst environments remains limited. To provide more insight into this issue, a 14-month field monitoring experiment was conducted to explore the influence of mosses and cyanobacteria on soil moisture dynamics in the top layer under three treatments: Inoculated Hypnum cupressiforme, covered Nostoc commune and bare soil. The results showed that Hypnum cupressiforme and Nostoc commune treatments significantly increased shallow soil moisture by 6.09 %-14.6 % and 1.05 % -10.8 % in the 5 cm soil layer, by 0.34 % -9.6 % and 0.43 % -7.01 % in the 10 cm soil layer, respectively. Compared with bare soil, Hypnum cupressiforme treatment to slow down the rate of soil dehydration was superior to that of Nostoc commune treatment during the drying season; during the wetting season, Hypnum cupressiforme treatment significantly slowed down the loss rate of soil moisture, while Nostoc commune treatment only slowed down the loss rate of soil moisture in 10 cm soil layer, but accelerated the loss of soil moisture in 5 cm soil layer, which may be attributed to the high sensitivity of Nostoc commune to water. The runoff depth of bare soil were 1.55-9.14 times and 3.52-131.41 times than that of Hypnum cupressiforme and Nostoc commune, respectively, which indicated that Hypnum cupressiforme and Nostoc commune play a role in controlling runoff and increasing water infiltration. This study can contribute to the further understanding of the eco-hydrological processes and hydrological simulation of the humid ecosystem
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