胡杨根系拓扑分形特征对水分梯度的响应规律OACHSSCD
Investigating the response dynamics of fractal-topological characteristics in Populus euphratica root systems to moisture gradient variations
在干旱区的荒漠生态系统之中,水资源极为匮乏.而根系作为植物极为关键的功能器官,其空间根系分形直接影响植物水分资源获取能力.根系发达的胡杨(Populus euphratica Oliv.)作为干旱区典型落叶乔木,研究其异型根系结构特征,对于了解荒漠植物环境适应具有重要价值.本研究选取新疆艾比湖湿地国家级自然保护区内自然生长、健康的胡杨作为对象,利用TRU树木雷达通过三维建模与统计学分析,探讨胡杨根系拓扑分形特征对水分有效性梯度的响应规律,揭示胡杨根系对于水分变化的变化规律.结果表明:(1)土壤含水量随距河岸距离增加呈显著递减趋势(18.36→4.58%),垂直剖面上则表现为表层(0-20 cm)低值区(3.78%)到深层(>200 cm)高值区(11.50%)的逐渐跃升.(2)胡杨根系密度随离河距离增加呈现逐渐增加在降低的一个趋势,最大值为2.58 g/cm3,最小值为1.75 g/cm3,且主要集中在距离河2-2.5 km的样地中,在土壤的垂直分层上.近岸区(0-0.5 km)与远岸区(4-4.5 km)根系密度呈单峰分布,峰值位于50-150 cm层;根系密度离河距离2-2.5 km时,过渡带(2-2.5 km)则表现为双波动态,深层(>200 cm)密度达最大值.(3)胡杨根系密度与土壤水分含量之间的关系存在显著差异,在近河岸(0-0.5km)和远河岸(4-4.5km)处,整体呈现出随着土壤含水量的增加,根系密度先增加后减少的趋势.而在距河2-2.5km处,根系密度与土壤水分含量之间呈现正相关,垂直剖面下的胡杨根系空间分布随土壤含水量变化呈线性分布.浅层(0-20 cm)呈正相关,深层(100-150 cm)负相关显著.
In desert ecosystems of arid regions,water availability is severely limited.Root systems,serving as critical functional organs of plants,exhibit spatial fractal architectures that directly influence plant water acquisition capacity.Populus euphratica Oliv.,a typical deciduous tree species in arid zones characterized by well-developed root systems,presents a valuable model for investigating dimorphic root architectural features.Such research provides crucial insights into the adaptive strategies employed by desert vegetation in response to environmental constraints.This study selected naturally occurring,healthy Populus euphratica specimens within the Xinjiang Ebinur Lake Wetland National Nature Reserve as research subjects.Employing TRU tree radar technology integrated with three-dimensional modeling and statistical analyses,we investigated the response patterns of topological fractal characteristics in P.euphratica root systems along water availability gradients,thereby elucidating the adaptive mechanisms governing root system plasticity in response to hydrological variability.Results revealed that:(1)Soil moisture content exhibited a significant decreasing gradient with increasing distance from the riparian zone(declining from 18.36%to 4.58%),while the vertical soil profile demonstrated a contrasting stratification pattern,characterized by a progressive increase from moisture-depleted surface horizons(0-20 cm;3.78%)to water-enriched deeper soil layers(>200 cm;11.50%).(2)P.euphratica root density exhibited a non-linear response pattern with increasing distance from the riverbank,initially increasing before subsequently declining across the lateral gradient,with values ranging from a minimum of 1.75 g/cm3 to a maximum of 2.58 g/cm3.Peak root densities were predominantly concentrated in sampling plots located 2-2.5 km from the river.Vertical distribution patterns varied systematically across the riparian-upland gradient:both proximal riparian zones(0-0.5 km)and distal zones(4-4.5 km)displayed unimodal root density distributions,with maximum concentrations occurring in the intermediate soil horizon(50-150 cm).In contrast,the intermediate transition zone(2-2.5 km)exhibited a distinct bimodal distribution pattern,characterized by maximum root density values in the deeper soil strata(>200 cm).(3)The relationship between P.euphratica root density and soil moisture content exhibited significant spatial variation.In both riparian(0-0.5 km)and distal zones(4-4.5 km),root density displayed a unimodal response to increasing soil moisture,initially increasing before subsequently declining.Conversely,in the intermediate zone(2-2.5 km from the river),root density showed a positive correlation with soil moisture content.Vertical analysis revealed that the spatial distribution of P.euphratica root systems exhibited a linear relationship with soil moisture gradients.Specifically,shallow soil horizons(0-20 cm)demonstrated a significant positive correlation,while deeper horizons(100-150 cm)exhibited a significant negative correlation.
刘晶;何学敏;冯海鹏;巴合别勒德;杨欢;党子颜;松哈尔
新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300新疆大学生态与环境学院,乌鲁木齐 830017||新疆大学绿洲生态教育部重点实验室,乌鲁木齐 830017||新疆精河温带荒漠生态系统教育部野外科学观测研究站,乌鲁木齐 833300
胡杨根系水分梯度树木雷达根系密度艾比湖
Populus euphratica root systemmoisture gradienttree radarroot densityEbinur Lake
《生态学报》 2026 (6)
3001-3012,12
中央引导地方科技发展专项(ZYYD2023A03)国家自然科学基金(31760168)
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