[1]杨志强,孟 晨,王 兴,等.荒漠草原人工柠条引入后土壤大孔隙拓扑结构演变特征[J].水土保持研究,2024,31(02):92-100.
　Yang Zhiqiang,Meng Chen,Wang Xing,et al.Evolution of Soil Macropore Topological Structure After the Artificial Introduction of Caragana korshinskii in Desert Steppe[J].Research of Soil and Water Conservation,2024,31(02):92-100.
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荒漠草原人工柠条引入后土壤大孔隙拓扑结构演变特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 31 期数: 2024年02期 页码: 92-100 栏目: 出版日期: 2024-03-20
Title:
Evolution of Soil Macropore Topological Structure After the Artificial Introduction of Caragana korshinskii in Desert Steppe
文章编号:
1005-3409(2024)02-0092-09
作者:
杨志强1,2,3, 孟 晨2,3,4, 王 兴2,3,4, 朱志昊2,3,4, 宋乃平2,3,4, 杜灵通2,3,4
(1.宁夏大学 农学院, 银川 750021; 2.宁夏大学 西北土地退化与生态系统恢复国家重点实验室培养基地, 银川 750021; 3.西北退化生态系统恢复与重建教育部重点实验室, 银川 750021; 4.宁夏大学 生态环境学院, 银川 750021)
Author(s):
Yang Zhiqiang1,2,3, Meng Chen2,3,4, Wang Xing2,3,4, Zhu Zhihao2,3,4, Song Naiping2,3,4, Du Lingtong2,3,4
(1.College of Agriculture, Ningxia University, Yinchuan 750021, China; 2.State Key Laboratory of Land Degradation and Ecosystem Restoration in Northwest China, Ningxia University, Yinchuan 750021, China; 3.Key Laboratory of Restoration and Reconstruction of Degraded Ecosystem in Northwest China, Ministry of Education, Yinchuan 750021, China; 4.College of Ecology and Environment, Ningxia University, Yinchuan 750021, China)
关键词:
荒漠草原;  人工柠条;  土壤大孔隙;  拓扑结构;  CT扫描
Keywords:
desert steppe;  planted Caragana korshinskii;  soil macropore;  topological structure;  computed tomography(CT)scan
分类号:
S152.5
文献标志码:
A
摘要:
[目的]认识人工柠条种植对土壤生态过程的影响,从而为人工植被的管理提供科学依据。[方法]以宁夏盐池县典型荒漠草原区风沙土生境的草地(0 a)及9,14,24,35 a生人工柠条林为对象,分别进行原状土柱采集、CT扫描及图像处理分析,获取土壤大孔隙几何分布特征,量化大孔隙表面积、等效直径和连接度等拓扑结构参数,研究了柠条生长过程中土壤大孔隙演变特征。[结果]通过三维图像可以看出,和0 a样地相比,随着林龄增加,各样地在0—200 mm土层大孔隙数量明显增多且结构更加复杂。定量分析表明,和0 a样地相比,不同林龄柠条林地在同一土层,大孔隙数量密度、长度密度、等效直径、连接度之间差异显著(p<0.05),而表面积密度、体积密度无显著差异(p>0.05)。具体表现为在0—100 mm和100—200 mm土层大孔隙数量密度、长度密度均显著增加(p<0.05),且随着林龄增加,表层土壤(0—100 mm)增幅要大于深层土壤(100—200 mm); 等效直径在0—100 mm土层显著减小,在100—200 mm土层显著增加(p<0.05),而连接度变化规律恰好相反。进一步分析发现,林龄与大孔隙数量密度、长度密度、表面积密度呈显著正相关(p<0.05),与大孔隙等效直径呈显著负相关(p<0.01),与大孔隙体积密度差异不显著(p>0.05)。[结论]人工柠条林的引入会促进土壤大孔隙致密网络状结构形成,改善大孔隙表面积、连接度等拓扑结构,且随着林龄增加,对土壤改良效果越明显。
Abstract:
[Objective] The aims of this study are to understand the effects of planted Caragana korshinskii on soil ecological processes, and to provide a scientific basis for the management of artificial vegetation. [Methods] This study focused on the planted C. korshinskii forest with ages ranging from 9 years to 35 years in a typical desert grassland area of Yanchi County, Ningxia. The changes in the geometric distribution and topological structure of macropores in soil after the introduction of C. korshinskii were studied. Computed tomography(CT)scanning and image processing were applied to soil samples collected from the undisturbed soil column to identify the geometric distribution of soil macropores and their topological parameters. These parameters included macropore surface area, equivalent diameter, and connectivity. [Results] The three-dimensional(3D)CT images indicated a relatively small number of macropores in the 0—200 mm soil layer of plots 0 a, whereas those in the 0—200 mm layer of other plots were significantly higher and showed a more complex structure with stand age. Quantitative analysis showed the significant differences in the quantities, lengths, equivalent diameters, and connectivity of macropores of the same soil layers between different ages of C. korshinskii forest(p<0.05), although there were no significant differences in surface area density and volume density(p>0.05). The quantity density and length density of macropores in the 0—100 mm and 100—200 mm soil layers significantly increased(p<0.05)with the increase of forest age, with that in surface soil(0—100 mm)exceeding that in deep soil(100—200 mm). The equivalent macropore diameters for different ages of C. korshinskii forest decreased and increased significantly in 0—100 mm and 100—200 mm soil layers, respectively(p<0.05). In contrast, macropore connectivity increased and decreased significantly in the 0—100 mm and 100—200 mm soil layers, respectively(p<0.05). Further analysis showed positive correlations between stand age and the number density, length density, and surface area density of macropores(p<0.05), but a negative correlation with the equivalent diameter of macropores(p<0.01), whereas there was no significant relationship with the volume density of macropores(p>0.05). [Conclusion] The artificial introduction of C. korshinskii forest can promote a complex and compact macropore network structure, thereby improve the topological structure of macropores and increase soil connectivity. These effects on soil increase with increase of forest age. The results of this study can inform the use of artificial vegetation for restoration and management of aeolian soil in arid and semi-arid areas.

参考文献/References:

[1] 贾昂元,张勇勇,赵文智,等.干旱区绿洲农田土壤大孔隙与水分入渗特征[J].土壤学报,2022,59(2):486-497.
Jia A Y, Zhang Y Y, Zhao W Z, et al. Characteristics of Soil macropores and water infiltration in oasis croplands in an arid region[J]. Acta Pedologica Sinica, 2022,59(2):486-497.
[2] 祁子寒,王云琦,王玉杰,等.根系对浅表层土大孔隙分布特征及饱和渗透性的影响[J].水土保持学报,2021,35(5):94-100,107.
Qi Z H, Wang Y Q, Wang Y J, et al. Effect of root system on macropores distribution and saturated permeability of surface soil[J]. Journal of Soil and Water Conservation, 2021,35(5):94-100,107.
[3] Meng C, Niu J Z, Li X, et al. Quantifying soil macropore networks in different forest communities using industrial computed tomography in a mountainous area of North China[J]. Journal of Soils and Sediments, 2017,17(9):2357-2370.
[4] Li T C, Shao M A, Jia Y H, et al. Using the X-ray computed tomography method to predict the saturated hydraulic conductivity of the upper root zone in the Loess Plateau in China[J]. Soil Science Society of America Journal, 2018,82(5):1085-1092.
[5] Wendel A S, Bauke S L, Amelung W, et al. Root-rhizosphere-soil interactions in biopores[J]. Plant and Soil, 2022,475(1):253-277.
[6] Kochiieru M, Lamorski K, Feiza V, et al. The effect of soil macroporosity, temperature and water content on CO2 efflux in the soils of different genesis and land management[J]. Zemdirbyste, 2018,105(4):291-298.
[7] Yang Z G, Hu X, Li X Y, et al. Soil macropore networks derived from X-ray computed tomography in response to typical thaw slumps in Qinghai-Tibetan Plateau, China[J]. Journal of Soils and Sediments, 2021,21(8):2845-2854.
[8] Gao Z, Hu X, Li X Y, et al. Effects of freeze-thaw cycles on soil macropores and its implications on formation of hummocks in alpine meadows in the Qinghai Lake watershed, northeastern Qinghai-Tibet Plateau[J]. Journal of Soils and Sediments, 2021,21(1):245-256.
[9] Leuther F, Schlüter S. Impact of freeze-thaw cycles on soil structure and soil hydraulic properties[J]. Soil, 2021,7(1):179-191.
[10] Wang J, Zhao W W, Wang G, et al. Effects of long-term afforestation and natural grassland recovery on soil properties and quality in Loess Plateau(China)[J]. Science of the Total Environment, 2021,770:144833.
[11] Cui Z, Huang Z, Liu Y, et al. Natural compensation mechanism of soil water infiltration through decayed roots in semi-arid vegetation species[J]. Science of the Total Environment, 2022,819:151985.
[12] 华瑞.黄土丘陵区不同退耕年限林草地土壤结构及大孔隙研究[D].陕西杨凌:西北农林科技大学,2016.
Hua R. The Research of Soil Structure and Macro-pores of Forestlands and Grasslands Under Different Vegetation Restoration Years in Loess Hilly Area[D]. Yangling, Shaanxi: Northwest A&F University, 2016.
[13] 张玉萍,宋乃平,王兴.宁夏荒漠草原短花针茅丛“肥岛”效应研究[J].宁夏大学学报:自然科学版,2022,43(1):81-84.
Zhang Y P, Song N P, Wang X. Study on “Fertilizer Island” effect of Stipa breviflora in desert grassland in Ningxia[J]. Journal of Ningxia University: Natural Science Edition,2022,43(1):81-84.
[14] 张小菊,每杭,沈艳.平茬方式对宁夏荒漠草原人工柠条林土壤物理性质及持水能力的影响[J].草原与草坪,2020,40(4):73-79.
Zhang X J, Mei H, Shen Y. Effects of stubble on soil physical properties and water holding capacity of artificial Caragana in Ningxia Desert steppe[J]. Grassland and Turf, 2020,40(4):73-79.
[15] 王松伟,郭忠升.多年生人工柠条林生长对土壤水分的影响[J].水土保持研究,2020,27(3):70-75.
Wang S W, Guo Z S. Effects of perennial Caragana korshinskii kom on soil moisture[J]. Research of Soil and Water Conservation, 2020,27(3):70-75.
[16] 张茹,李建平,彭文栋,等.柠条枝条覆盖对宁夏荒漠草原土壤水热及补播牧草生物量的影响[J].草业学报,2021,30(4):58-67.
Zhang R, Li J P, Peng W D, et al. Effects of mulching with caragana(Caragana intermedia)branches on soil moisture content and temperature and reseeded forage biomass in desertified grassland in Ningxia Province, China[J]. Acta Prataculturae Sinica, 2021,30(4):58-67.
[17] 程静,王鹏,陈红翔,等.半干旱区生态风险时空演变及其影响因素的地理探测:以宁夏盐池县为例[J].干旱区地理,2022,45(5):1637-1648.
Cheng J, Wang P, Chen H X, et al. Geographical exploration of the spatial and temporal evolution of ecological risk and its influencing factors in semi-arid regions: A case of Yanchi County in Ningxia[J]. Arid Land Geography, 2022,45(5):1637-1648.
[18] 王乐,杜灵通,马龙龙,等.人工灌丛化对荒漠草原生态系统碳储量的影响[J].生态学报,2022,42(1):246-254.
Wang L, Du L T, Ma L L, et al. Effects of planted shrub encroachment on carbon storage of desert steppe ecosystem[J]. Acta Ecologica Sinica, 2022,42(1):246-254.
[19] 李同川.黄土高原土壤大孔隙特征及其对土壤水分的影响[D].陕西杨凌:西北农林科技大学,2017.
Li T C. Characteristics of Soil Macropore on the Loess Plateau and Their Effects on Soil Water[D]. Yangling, Shaanxi: Northwest A&F University, 2017.
[20] Luo L, Lin H, Li S. Quantification of 3-D soil macropore networks in different soil types and land uses using computed tomography[J]. Journal of Hydrology,2010,393(1/2):53-64.
[21] 石辉,陈凤琴,刘世荣.岷江上游森林土壤大孔隙特征及其对水分出流速率的影响[J].生态学报,2005,25(3):507-512.
Shi H, Chen F Q, Liu S R. Macropores properties of forest soil and its influence on water effluent in the upper reaches of Minjiang River[J]. Acta Ecologica Sinica, 2005,25(3):507-512.
[22] 吕刚,王洪禄,黄龙.辽西半干旱区森林土壤大孔隙特征研究[J].水土保持通报,2012,32(5):176-181.
Lü G, Wang H L, Huang L. A study on macropore properties of forest soil in semi-arid region of western Liaoning Province[J]. Bulletin of Soil and Water Conservation, 2012,32(5):176-181.
[23] Budhathoki S, Lamba J, Srivastava P, et al. Temporal and spatial variability in 3D soil macropore characteristics determined using X-ray computed tomography[J]. Journal of Soils and Sediments, 2022,22(4):1263-1277.
[24] 王卫华,张志鹏.基于土壤导气率的燥红土孔隙结构及弯曲连通性研究[J].土壤学报,2018,55(2):360-368.
Wang W H, Zhang Z P. Study on the dry red soil pore structure and pore tortuosity-connectivity based on soil air permeability[J]. Acta Pedologica Sinica, 2018,55(2):360-368.
[25] 张靖,陈琳,周虎,等.基于数字图像技术的土壤孔隙结构定量研究进展[J].土壤,2023,55(1):21-29.
Zhang J, Chen L, Zhou H, et al. Quantification of soil pore structure based on digital image technology: A review[J]. Soils,2023,55(1):21-29.
[26] 黄娟,邓羽松,马占龙,等.桂东南花岗岩丘陵区不同土地利用方式土壤大孔隙特征[J].水土保持学报,2021,35(2):80-86.
Huang J, Deng Y S, Ma Z L, et al. Characteristics of soil macropores in Granite Hilly Region Area with different land use types in southeast Guangxi[J]. Journal of Soil and Water Conservation, 2021,35(2):80-86.
[27] Yi J, Yang Y, Liu M X, et al. Characterising macropores and preferential flow of mountainous forest soils with contrasting human disturbances[J]. Soil Research, 2019,57(6):601-614.

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　LIU Hua,JIANG Qi,WANG Zhan-jun,et al.A Study on soil Seed Bank in Desert Steppe of Different Enclosing Years in Ningxia[J].Research of Soil and Water Conservation,2011,18(02):96.
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　LUO Xu,LI Jianping,ZHANG Yi,et al.Response of Spatial and Temporal Variation of Soil Moisture to Precipitation Change in Desert Steppe[J].Research of Soil and Water Conservation,2021,28(02):142.

备注/Memo

收稿日期:2023-01-19 修回日期:2023-04-11
资助项目:宁夏重点研发计划项目(2021BEB04012,2022BEG02003,2019BFG02010); 宁夏自然科学基金(2022AAC03012,2021AAC05005)
第一作者:杨志强(1996—),男,甘肃通渭人,硕士研究生,研究方向为水土保持与荒漠化防治。E-mail:17690618395@163.com
通信作者:孟晨(1990—),男,宁夏石嘴山人,博士,副研究员,主要从事水土保持与土壤水文研究。E-mail:mengchen@nxu.edu.cn

更新日期/Last Update: 2024-04-20