|
|
A review of researches on plant root channel architecture and soil preferential flow process |
DUAN Jian1, WANG Lingyun1, WANG Ling2, YANG Jie1, WANG Jian2, TANG Chongjun1, ZHENG Haijin1 |
1. Jiangxi Provincial Key Laboratory of Soil Erosion and Prevention, Jiangxi Academy of Water Science and Engineering, 330029, Nanchang, China; 2. College of Resources and Environment, Huazhong Agricultural University, 430070, Wuhan, China |
|
|
Abstract [Background] Root channels formed by the alive roots and rotten roots play an important role in increasing preferential flow and altering hydrological processes such as soil infiltration. The root channel architecture characteristics are very complex and difficult to describe accurately and quantitatively. The influence mechanisms of root channels on preferential flow infiltration process are theoretically beneficial to water resources management, groundwater pollution, landslides and mudslides prevention.[Methods] In view of this research hotspot, numerous literature retrieval were carried out with "root channels" "architecture characteristics" "preferential flow" "matrix infiltration" "soil infiltration" and "soil moisture" as keywords in the Web of Science and China National Knowledge Infrastructure (CNKI) databases. These keywords appeared very frequently in relevant fields. Representative literatures were selected for analysis and integration in the previous studies by the end of 2020. The influencing factors, quantitative measurement methods of plant root channel architecture were in detailed described, and the influences of root channel architecture on soil preferential flow infiltration process were discussed.[Results] 1) The biological and abiotic factors, such as plant species, planting time, soil properties, and management measures significantly influence root channel architecture and the mechanism of each influencing factor are still unclear. In the past, due to technical methods and other limitations, soil macropores from different sources were often studied together during the study of preferential flow, without separately considering the characteristics of plant root channels and their importance. 2) In recent years, it has become a trend to use CT scanning imaging technology to obtain three-dimensional parameters of root channel architecture, which can characterize the network structure of large pores from different sources (biopores and non-biopores) as a whole. 3) Preferential flow and soil matrix infiltration are the two forms of soil water infiltration. During soil infiltration process, preferential flow must be accompanied by soil matrix infiltration. Previous quantitative research methods of preferential flow cannot quantitatively partition the temporal preferential flow and matrix infiltration, resulting in very little quantitative research of preferential flow infiltration process. However, the macropore connectivity blocking method provide a practical solution for quantitatively partition the temporal preferential flow and soil matrix infiltration. 4) Plant root system may improve soil infiltration properties by forming root channels through its own decay and decomposition. The values of root channel numbers, area, volume, and diameter are significantly and positively correlated with the soil infiltration rates and preferential flow flux.[Conclusions] Therefore, in the future, the three-dimensional quantitative index system for root channel architecture should be established to reveal development mechanism and architecture characteristics of plant root channel. More efforts should be focused on the influence mechanisms of root channel architecture on soil preferential flow infiltration process. It will be an important research direction to deeply reveal the mechanism of soil preferential flow movement and its contribution to water infiltration.
|
Received: 30 September 2021
|
|
|
|
|
[1] |
朱钊岑, 刘冰, 刘婵, 等. 荒漠绿洲湿地土壤优先流与水分入渗特征[J]. 生态学报, 2020, 40(12):3979. ZHU Zhaocen, LIU Bing, LIU Chan, et al. Characteristics of preferential flow and water infiltration in desert oasis wetland[J]. Acta Ecologica Sinica, 2020, 40(12):3979.
|
[2] |
牛健植, 余新晓. 优先流问题研究及其科学意义[J]. 中国水土保持科学, 2005, 3(3):110. NIU Jianzhi, YU Xinxiao. Preferential flow and its scientific significance[J]. Science of Soil and Water Conservation, 2005, 3(3):110.
|
[3] |
FOX G, WILSON G. The role of subsurface flow in hillslope and stream bank erosion:A review[J]. Soil Science Society of America Journal, 2010, 74:717.
|
[4] |
刘芳, 李贵宝, 王殿武, 等. 植物根孔研究进展[J]. 水土保持学报, 2004, 18(2):178. LIU Fang, LI Guibao, WANG Dianwu, et al. Review of study on root channels[J]. Journal of Soil and Water Conservation, 2004, 18(2):178.
|
[5] |
张勇勇, 富利, 赵文智, 等. 荒漠绿洲土壤优先流研究进展[J]. 中国沙漠, 2017, 37(6):1189. ZHANG Yongyong, FU Li, ZHAO Wenzhi, et al. A review of researches on preferential flow in desert-oasis region[J]. Journal of Desert Research, 2017, 37(6):1189.
|
[6] |
ZHANG Zhongbin, LIU Kailou, ZHOU Hu, et al. Three dimensional characteristics of biopores and non-biopores in the subsoil respond differently to land use and fertilization[J]. Plant and Soil, 2018, 428:453.
|
[7] |
NAVEED M, MOLDRUP P, SCHAAP M, et al. Prediction of biopore-and matrix-dominated flow from X-ray CT-derived macropore network characteristics[J]. Hydrology and Earth System Science, 2016, 20:4017.
|
[8] |
KOSETEL J, LARSBO M. Imaging and quantification of preferential solute transport in soil macropores[J]. Water Resource and Research, 2014, 50:4357.
|
[9] |
BODNER G, LEITNER D, KAUL H. Coarse and fine root plants affect pore size distributions differently[J]. Plant and Soil, 2014, 380(1/2):133.
|
[10] |
WU Gaolin, LIU Yu, YANG Zheng, et al. Root channels to indicate the increase in soil matrix water inflltration capacity of arid reclaimed mine soils[J]. Journal of Hydrology, 2017, 546:133.
|
[11] |
LIU Yu, GUO Lei, HUANG Ze, et al.Root morphological characteristics and soil water inflltration capacity in semi-arid artiflcial grassland soils[J]. Agricultural Water Management, 2020, 235:106153.
|
[12] |
MATERECHERA S, ALSTON A, KIRBY J, et al. Influence of root diameter on the penetration of seminal roots into a compacted subsoil[J]. Plant Soil, 1992, 144:297.
|
[13] |
KAUTZ T, STUMM C, KOSTERS R, et al.Effects of perennial fodder crops on soil structure in agricultural headlands[J]. Journal of Plant Nutrition and Soil Science, 2010, 173:490.
|
[14] |
NESPOULOUS J, MERINO-MARTIN L, MONNIER Y, et al. Tropical forest structure and understorey determine subsurface flow through biopores formed by plant roots[J]. Catena, 2019, 181:104061.
|
[15] |
HUANG Ze, SUN Lei, LIU Yu, et al. Alfalfa planting significantly improved alpine soil water infiltrability in the Qinghai-Tibetan Plateau[J]. Agriculture, Ecosystems and Environment, 2019, 285:106606.
|
[16] |
HAN E, KAUTZ T, PERKONS U, et al. Quantification of soil biopore density after perennial fodder cropping[J]. Plant and Soil, 2015, 394:73.
|
[17] |
KAUTZ T. Research on subsoil biopores and their functions in organically managed soils:A review[J]. Renewable Agriculture and Food Systems, 2015, 30(4):318.
|
[18] |
王大力, 尹澄清. 植物根孔在土壤生态系统中的功能[J]. 生态学报, 2000, 20(5):869. WANG Dali, YIN Chengqing. Functions of root channels in the soil system[J]. Acta Ecologica Sinica, 2000, 20(5):869.
|
[19] |
VANNOPPEN W, VANMAERCKE M, DE BAETS S, et al. A review of the mechanical effects of plant roots on concentrated flow erosion rates[J]. Earth-Science Review, 2015, 150:666.
|
[20] |
CHEN Guihua, WEIL R R. Penetration of cover crop roots through compacted soils[J]. Plant and Soil, 2010, 331:31.
|
[21] |
陈晓冰, 严磊, 李振东, 等. 耕作方式对岩溶区甘蔗地土壤优先流特征的影响[J]. 土壤, 2019, 51(4):786. CHEN Xiaobing, YAN Lei, LI Zhendong, et al. Tillage pattern effects on characteristics of soil preferential flow in sugarcane fields in the karst region[J]. Soil, 2019, 51(4):786.
|
[22] |
ZHANG Zhongbin, PENG Xinhua. Bio-tillage:A new perspective for sustainable agriculture[J]. Soil and Tillage Research, 2021, 206:104884.
|
[23] |
QI Wei, ZHANG Zhanyu, WANG Ce, et al. Crack closure and flow regimes in cracked clay loam subjected to different irrigation methods[J]. Geoderma, 2020, 358:113978.
|
[24] |
MA Li, SHAO Ming'an, FAN Jun, et al. Effects of earthworm (Metaphire guillelmi) density on soil macropore and soil water content in typical Anthrosol soil[J]. Agriculture, Ecosystems and Environment, 2021, 311:107338.
|
[25] |
LEUE M, UTEAU-PUSCHMANN D, PETH S, et al. Separation of soil macropore types in three-dimensional x-ray computed tomography images based on pore geometry characteristics[J]. Vadose Zone Journal, 2019, 18:180170.
|
[26] |
PAGENKEMPER S, PETH S, PUSCHMANN D, et al. Effects of root-induced biopores on pore space architecture investigated with industrial X-ray computed tomography[M].Madison, Wisconsin, United States:SSSA Special Publication, 2013:67.
|
[27] |
STEWART R D, ABOU NAJM M R. Field measurements of soil cracks[J]. Soil Science Society of America, 2017, 2:1.
|
[28] |
BOTTINELLI N, ZHOU Hu, CAPOWIEZ Y, et al. Earthworm burrowing activity of two non-Lumbricidae earthworm species incubated in soils with contrasting organic carbon content (vertisol vs. Ultisol)[J]. Biology and Fertility of Soils, 2017, 53:951.
|
[29] |
ZHANG Jing, LEI Tingwu, QU Liqin, et al. Method to measure soil matrix inflltration in forest soil[J]. Journal of Hydrology, 2017, 552:241.
|
[30] |
GAO Man, LI Hongyi, LIU Dengfeng, et al. Identifying the dominant controls on macropore flow velocity in soils:A meta-analysis[J]. Journal of Hydrology, 2018, 567:590.
|
[31] |
ZHANG Jing, LEI Tingwu, QU Liqin, et al. Method to quantitatively partition the temporal preferential flow and matrix infiltration in forest soil[J]. Geoderma, 2019, 347:150.
|
[32] |
ALLAIRE S, ROULIER S, CESSNA A. Quantifying preferential flow in soils:A review of different techniques[J]. Journal of Hydrology, 2009, 378:179.
|
[33] |
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. SHI Hui, CHEN Fengqin, LIU Shirong. 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.
|
[34] |
刘目兴, 杜文正. 山地土壤优先流路径的染色示范研究[J]. 土壤学报, 2013, 50(5):871. LIU Muxing, DU Wenzheng. To investigate soil preferential flow paths in mountain area using dye tracer[J]. Acta Pedologica Sinica, 2013, 50(5):871.
|
[35] |
XU Xuexuan, KALHORO S, CHEN Wenyuan, et al. The evaluation/application of Hydrus-2D model for simulating macro-pores flow in loess soil[J]. International Soil and Water Conservation Research, 2017, 5(3):196.
|
[36] |
ALLAIRE-LEUNG S, GUPTA S, MONCRIEF J. Water and solute movement in soil as influenced by macropore characteristics 1. Macropore continuity[J]. Journal of Contaminant Hydrology, 2000, 41:283.
|
[37] |
ALLAIRE S, GUPTA S, NIEBER J, et al. Role of macropore continuity and tortuosity on solute transport in soils:1. Effects of initial and boundary conditions[J]. Journal of Contaminant Hydrology, 2002, 58:299.
|
[38] |
SANDERS E, NAJM M, MOHTAR R, et al. Field method for separating the contribution of surface-connected preferential flow pathways from flow through the soil matrix[J]. Water Resources Research, 2012, 48(4):1427.
|
[39] |
DAS GUPTA S, MOHANTY B, KOHNE J. Soil hydraulic conductivities and their spatial and temporal variations in a vertisol[J]. Soil Science Society of America Journal, 2006, 70(6):1872.
|
[40] |
陶婷婷, 陈晓燕, 黄永超, 等. 重庆沙溪庙组紫色土土壤基质和优先流入渗的定量测算[J]. 中国水土保持科学, 2019, 17(6):41. TAO Tingting, CHEN Xiaoyan, HUANG Yongchao, et al. Quantitative measurement and calculation of soil matrix and preferential infiltration in Shaximiao purple soil, Chongqing[J]. Science of Soil and Water Conservation, 2019, 17(6):41.
|
[41] |
BENEGAS L, ILSTEDT U, ROUPSARD O, et al.Effects of trees on infiltrability and preferential flow in two contrasting agroecosystems in central America[J]. Agriculture, Ecosystems & Environment, 2014, 183:185.
|
[42] |
LIU Yu, GUO Lei, HUANG Ze, et al. Root morphological characteristics and soil water inflltration capacity in semi-arid artiflcial grassland soils[J]. Agricultural Water Management, 2020, 235:106153.
|
[43] |
ARCHER N, QUINTON J, HESS T. Below-ground relationships of soil texture, roots and hydraulic conductivity in two-phase mosaic vegetation in Southeast Spain[J]. Journal of Arid Environment, 2002, 52:535.
|
[44] |
LARSBO M, KOESTEL J, JARVIS N. Relations between macropore network characteristics and the degree of preferential solute transport[J]. Hydrology and Earth System Science, 2014, 18:5255.
|
[45] |
WU Gaolin, CUI Zeng, HUANG Ze. Contribution of root decay process on soil infiltration capacity and soil water replenishment of planted forestland in semi-arid regions[J]. Geoderma, 2021, 404:115289.
|
[46] |
DEVITT D, SMITH S.Root channel macropores enhance downward movement of water in a Mojave Desert ecosystem[J]. Journal of Arid Environments, 2002, 50:99.
|
[1] |
YAO Lu, HOU Ruiping, WANG Yunqi, WANG Yujie, CUI Xinrui, ZHENG Yonglin, SHEN Hang, LAN Yue, LI Cheng, MA Lei, SI Hongtao. Short-term effects of burning on the soil moisture physical characteristics of typical stands in Jinyun Mountain[J]. SSWC, 2023, 21(3): 78-85. |
|
|
|
|