• <tr id="yyy80"></tr>
  • <sup id="yyy80"></sup>
  • <tfoot id="yyy80"><noscript id="yyy80"></noscript></tfoot>
  • 99热精品在线国产_美女午夜性视频免费_国产精品国产高清国产av_av欧美777_自拍偷自拍亚洲精品老妇_亚洲熟女精品中文字幕_www日本黄色视频网_国产精品野战在线观看 ?

    Response of density-related fine root production to soil and leaf traits in coniferous and broad-leaved plantations in the semiarid loess hilly region of China

    2022-06-04 11:43:46MeimeiSunBoChaoZhaiQiuWenChenGuoqingLiShengDu
    Journal of Forestry Research 2022年3期

    Meimei Sun·Bo-Chao Zhai·Qiu-Wen Chen·Guoqing Li·Sheng Du

    Abstract Fine roots are the most active and functional component of root systems and play a significant role in the acquisition of soil resources.Density is an important structural factor in forest plantations but information on changes in fine roots along a density gradient is limited.In this study,plantations of black locust (Robinia pseudoacacia L.) and Chinese pine (Pinus tabuliformis Carr.) with four density classes were analyzed for the influence of soil and leaf traits on fine root growth.Fine root biomass increased with stand density.High fine root biomass was achieved through increases in the fine root production and turnover rate in the high-density black locust plantations and through an increase in fine root production in the pine plantations.In the high-density Chinese pine stand,there was a high fine root turnover which,coupled with high fine root production,contributed to a high fine root biomass.Overall,fine root production and turnover rate were closely related to soil volumetric water content in both kinds of plantations,while fine root biomass,especially the component of necromass,was related to soil nutrient status,which refers to phosphorous content in black locust plantations and nitrogen content in Chinese pine plantations.There was a close linkage between leaf area index and fine root dynamics in the black locust plantations but not in the pine plantations.

    Keywords Fine roots·Black locust·Chinese pine·Semiarid·Soil moisture·Leaf area index

    Introduction

    In forest plantations,stand density is a major index representing resource use conditions and interactions among and between trees and environments;thus,it is of major consideration in management practices.Stand density determines stand spatial structure and directly affects the distribution of light,heat,moisture,and other ecological factors affecting the growth of individual trees and of the plantation (Cai et al.2016;Hakkenberg et al.2016;Bo et al.2018).The effect of stand density on fine root dynamics has been studied in natural forests coupled with species richness (He et al.2005;Marquard et al.2 009;Zeng et al.2020).In plantations,the effects of stand density on fine root biomass,production,and turnover rate have been reported less frequently.

    Fine roots,generally defined as ≤ 2 mm in diameter,are one of the most physiologically active organs of the tree,owing to their short lifespan and large absorption capacity(Liu et al.2014;Wells and Eissenstat 2001).Although fine roots account for less than 10% of the total forest biomass(Olesinski et al.2012),they account for approximately a third of the annual net primary production in forest ecosystems (Finer et al.2019;Wang et al.2019).Because of their crucial role in energy and matter fluxes and the essential function of soil resource acquisition in the biosphere (Stewart and Frank 2008),fine root dynamics have been widely studied.However,most studies have focused on the upper soil layers no more than 30 cm deep where fine roots are believed to be the most abundant (Yuan and Chen 2010;Pickles and Pither 2014).Fine roots in deeper soil profiles have been reported to have a disproportionate impact on soil resource acquisition when trees cope with stress such as seasonal drought (Binkley 2015;Yang et al.2017;Wasyliw and Karst 2020).Due to the heterogeneous spatiotemporal distribution of fine roots (Wang et al.2013b),and the difficulty of directly observing underground processes (Finer et al.2011),knowledge about fine root dynamics remains limited.

    The effects of soil factors on fine root growth have been extensively studied.Soil nutrients and water have been reported to affect age-related fine root biomass but not fine root production in plantations on the Loess Plateau (Chen et al.2016).Zhou and Shangguan (2007) reported that soil water is a key factor in fine root vertical distribution,whereas the effect of inorganic nitrogen (N) is relatively limited.Soil surface layers are believed to have higher nutrient concentrations,low soil strength,and high water availability,which would promote the proliferation of roots with a more acquisitive strategy (Prieto et al.2015).However,a contrasting hypothesis suggested that fine roots might grow rapidly in order to more efficiently exploit soil resources in poor soil (Weemstra et al.2017).Given that both theories have been corroborated and refuted with empirical data (Leuschner et al.2004;Hertel et al.2013;Wang et al.2013a),more field data are needed from semiarid regions.

    Just as fine roots do belowground,leaves serve as absorption and interface organs aboveground (Jia et al.2015).Fine roots provide nutrients and water for photosynthesis in the leaves and in return,leaves provide carbohydrate products for fine roots (Jackson et al.1997).The two active organ systems are closely linked through material exchange and their activities and biomass are interdependent as predicted by the functional balance theory (Vanninen and Makela 1999;Albaugh et al.2006).Leaves and roots show similar resource acquisition strategies based on previous evidence (Diaz et al.2004;Liu et al.2010),and leaf functional traits may be partially extrapolated to corresponding root traits (Fort et al.2013;Li and Bao 2015).Fine root traits,such as biomass,morphology,and physiology,were found to be associated with leaf traits within and among species (Withington et al.2006;Hajek et al.2013;Meng et al.2018).Leaf nutrients are considered plastic traits that change with plant response to environmental variability (Pugnaire 2001).For example,carbon (C) contents reflect the adaptation strategy,to some extent,of plants to the environment (Zhao et al.2018),nitrogen (N) contents reflect the ability of plants to capture resources through enzymatic processes,and phosphorus(P) contents determine the energy available for metabolism(Agren 2008;Li and Bao 2015).Cote et al.(2003) reported that fine root production was negatively correlated with leaf N and P concentrations.The sensitivity of the shoot-to-root ratio to foliage N decreased with increasing root biomass in Japanese red pine seedlings (Chiwa et al.2012).Moreover,carbon allocation to roots was found to be mediated by foliar N in black spruce seedlings (Campagna and Margolis 1989).

    The Loess Plateau is a vast ecologically fragile area in China (Fu et al.2017).Since the launch of the Grain-for-Green Program in 1999,16,000 km2of rain-fed cropland has been converted to planted vegetation,resulting in an increase of 25% in vegetation cover in the region (Feng et al.2016).Plantation forests are the main contributors to ecological restoration in this area.Black locust (Robinia pseudoacaciaL.) and Chinese pine (Pinus tabuliformisCarr.) are the major plantation species in this area and have high environmental adaptability and stress resistance (Zhou and Shangguan 2007;Chen et al.2016).In this study,we investigated fine root biomass,fine root production,fine root turnover rate,and fine root necromass of four stand density classes in black locust and Chinese pine plantations in the loess hilly region.It was hypothesized that:(1) the effect of stand density on soil and leaf characteristics is inconsistent in the two plantation species due to different nutrient utilization strategies;and,(2) broad-leaved and coniferous plantations differ in their root-leaf linkages and responses of fine root production to soil properties.

    Materials and methods

    Site characteristics

    This study was conducted in southern Yan’an,Shaanxi Province,China.This area is characterized by a temperate semi-arid climate in the“forest to forest-steppe”ecosystem transition zone (Yamanaka et al.2014).The landforms are mainly loess hills and gullies.Mean annual precipitation is 537.9 mm,mostly occurring in July and August,and the annual mean temperature is 10.0 °C based on the Yan’an city meteorological station data for 1956–2015 (Cheng et al.2020).The growing season is from April to October.The main soil type is calcic Cambisols according to the FAO classification system (Yamamoto and Endo 2014).The study area comprised black locust and Chinese pine plantations established in large areas during the past decades (Yamanaka et al.2014).Shrubs and grasses are sparse in the understory layer of both plantations.

    Experimental design and vegetation survey

    Two types of plantations (black locust and Chinese pine)were selected along a stand density gradient.Stand density was classified into four classes (Table 1).All plots were converted from croplands with similar history and management.In the early spring of 2017,the study plots were established 0.5–5 km apart.The plots were 400 m2(20 m×20 m),except for a few at 100 m2(10 m×10 m) because of terrain conditions.Only two replicates were established in each density class due to few classes sharing similar age and site conditions.The vegetation survey was conducted yearly at the end of the growing season.Stand age was determined from tree rings of core samples.Details of the sampling plots are presented in Table 1.

    Table 1 Information on the plots of the plantations

    Soil sampling and measurements

    In 2017,soil samples from depths of 0–20,20–40,40–60 and 60–80 cm were collected in each plot using a cylindrical soil core sampler (4 cm in diameter).Six sites were chosen for sampling within each plot and were divided into two groups,on the left and on the right,each including upper,middle,and lower locations along the slope.For each group,samples from the same soil layer were thoroughly mixed to form a representative sample.Two soil samples were collected as replicates for each depth in each plot.The samples were cleaned of rocks and plant fragments,air-dried,ground and sieved through a 0.25 mm mesh.Organic C content was measured by wet combustion with K2C r2O7(Chinese standard GB 7857–87),total N content was determined by the Kjeldahl acid-digestion method,and total P content quantified using molybdenum-blue colorimetry (National Agricultural Technology Extension Service Center 2006).The nutrient concentrations in the horizon (0–80 cm) were calculated by averaging those of the four layers.

    In each plot,two representative sites at the upper and lower positions were chosen as replicates,and 3-m Tecanat?plastic tubes with an internal diameter of 42 mm were placed for repetitive measurements of soil moisture.Volumetric soil water content was measured using a time-domain reflectometry system (TRIME;IMKO Micromodultechnik,Ettlingen,Germany).Measurements began one year after installation.Soil water content was measured at 20-cm intervals along the profile,and the average for each layer obtained from the replicated tubes.During the growing season,three measurements were carried out:before the rainy season (May),during the rainy season (August),and after the rainy season(October).The average of the three measurements was taken as the plot soil water content used in the analysis.

    Leaf sample collection and measurement

    To collect leaf samples,representative trees were selected in each plot and healthy,mature leaves were collected from the upper and middle crowns.Three groups of leaf samples were collected from each plot and brought to the laboratory for nutrient content analysis.To determine the specific leaf area (SLA,m2kg?1),10–20 mature leaves without disease symptoms and insect pests were scanned to full size images.Samples were oven-dried at 105 °C for 30 min and then at 65 °C to a consistent weight.Leaf surface area was determined from the leaf images using Image J (National Institute of Health,Washington DC,USA).The specific leaf area was calculated as the ratio of leaf area to dry leaf weight.

    Oven-dried leaves were ground to powder and sieved through a 0.15 mm sieve.Organic C content was measured using the same method as used for soil samples.The powdered samples were initially digested with H2S O4and H2O2,and leaf N and P contents were determined using the semimicro Kjeldahl method and colorimetry assays,respectively.

    Leaf area index (LAI,m2m?2) was calculated from litterfall data from three litter traps (50 cm×50 cm) in each plot.Leaf litter was sorted by species,dried at 65 °C for approximately 48 h to a constant weight,and weighed to the nearest 0.01 g.Leaf area index was estimated by the treeleaf litter biomass and mean specific leaf area for the two plantations (Henderson and Jose 2005).

    Estimates of fine root biomass,production,and turnover rate

    Fine root biomass and necromass were measured using soil cores.Seven soil cores at representative locations were collected from each plot in July 2017.A soil auger was used to collect soil cores at 20-cm intervals to a depth of 80 cm.Fine root production was estimated using ingrowth cores established at seven representative points in each plot in August 2017.Ingrowth cores made of nylon net bags (6.5 cm diameter) were set up after soil columns were removed and filled with root-free original soil at the same depth.All ingrowth cores were extracted after one year (August 2018) by carefully removing the soil around the cylinder and separated into four layers at 20-cm intervals to collect roots that had grown into the core during the year.Soil cores were placed in plastic bags and transported to the laboratory to separate the roots.Fine roots were removed from the soil using forceps,and the remaining root segments in the soil were gently washed in a 0.1 mm sieve.All fine roots were washed to remove affixed soil residue and divided into living and dead roots.Fine roots that were brown or black in color,rigid and inelastic,and in some cases had decaying tissue were regarded as dead roots,whereas those that were white or light brown in color,were elastic and flexible were classifeid as live (Yuan and Chen 2012;Ding et al.2019).After classification,fine roots were oven-dried at 70 °C to a constant mass and weighed to the nearest 0.001 g.

    Fine root production (t ha?1a?1) was estimated from root biomass growing into the ingrowth cores–both live and dead roots were counted because of the short root longevity–divided by the growth time (one year).Fine root turnover rate (a?1) was defined as the ratio of fine root production to fine root biomass (Aber et al.1985;Yuan and Chen 2012).

    Data analysis

    Individual soil and leaf samples from each plot were treated as subsamples and used for statistical analysis.Averaged values were used in diagrams created with Sigmaplot 14.0.One-way analysis of variance (ANOVA) tested the differences in soil,leaf,and fine root characteristics.Two-way ANOVA analyzed the effect of stand density and species on fine root traits.The association between fine root characteristics and soil and leaf properties was assessed by Pearson correlation analysis.Statistical analyses were performed using SPSS 21.0 for Windows (version 21.0;SPSS Inc.,Chicago,IL,USA).Stepwise regression analysis was conducted using RStudio (version 3.6.2;R Core Team 2019,https://www.r-proje ct.org/).Significant differences were evaluated at the 0.05 probability level.

    Results

    Soil properties and leaf traits

    In black locust plantations,soil C and N contents were higher in density class II than in class I and the differences among classes II,III,and IV were not statistically significant (Fig.1 a,b).Soil P content and volumetric water content decreased with increasing stand density (Fig.1 c,d).In Chinese pine plantations,soil C,N,and P contents were significantly higher in stand density class III than in other density classes (Fig.1 a–c).Soil volumetric water content decreased as stand density increased (Fig.1 d).

    Fig.1 Soil properties of the two plantations along a stand density gradient.I,II,III,and IV represent four stand density classes;data bars are means and standard deviations.Different lowercase letters are statistically different (P <0.05) among density classes within the same plantation

    Leaf C content did not change significantly with stand density in either plantation (Fig.2a).In black locust plantations,leaf N content was maximized in density class III and minimized in class II (Fig.2 b).P contents in the leaves increased with stand density (Fig.2 c).There was no apparent change in leaf N and P contents with stand density in Chinese pine plantations (Fig.2 b,c).Leaf N content was highest in density class II and lowest in class III,while leaf P content was highest in density class IV and lowest in class I.Specific leaf area and leaf area index increased with stand density and maximized in density class III in black locust plantations (Fig.2 d,e).A similar trend was found in leaf area index,while specific leaf area was the lowest in density class II and highest in class IV in Chinese pine plantations.

    Fig.2 Leaf properties of the two plantations along a stand density gradient.I,II,III,and IV represent four stand density classes;data bars are means and standard deviations;different lowercase letters are statistically different (P <0.05) among stand density classes within the same plantation

    Fine root biomass,production,turnover rate,and necromass

    Greater fine root biomass,production,turnover rate,and necormass were found in higher stand density classes in both types of plantations,but differences between the adjacent classes were not statistically significant,particularly between class III and class IV (Fig.3).Overall,more significant differences were found among density classes in black locust plantations than in pine plantations,especially for fine root turnover rate (Fig.3 d).

    Fine roots were influenced by stand density and species(Table 2).The interaction between species and stand density had no effect on fine root production and biomass,but did have a significant effect on fine root turnover rate.Fine root production and biomass of Chinese pine were higher than those of black locust in each stand density class (Fig.3 a,c),while the fine root turnover rate of Chinese pine was lower than that of black locust along the stand density class spectrum.

    Fig.3 Fine root characteristics in the two plantations along a stand density gradient.I,II,III,and IV represent four stand density classes;bars are means and standard deviations,different lowercase letters are statistically different (P <0.05)

    Effects of soil properties on fine roots

    Pearson correlation analysis on fine root characteristics and soil properties in black locust plantations showed that fine root biomass and necromass were significantly related to soil N and P contents,whereas fine root production and turnover rate were related to soil P and volumetric water content.In Chinese pine plantations,fine root biomass and necromass were significantly related to soil N and volumetric water content,while fine root production and turnover rate were significantly related only to soil volumetric water content(Table 3).

    Relationships between leaves and fine roots

    In black locust plantations,fine root biomass,production,and turnover rate were correlated with leaf area index.In addition,fine root production and turnover rate were also correlated with leaf P contents (Table 4).In Chinese pine plantations,fine root biomass was correlated with specific leaf area and leaf area index,fine root production was correlated with leaf C and P contents and specific leaf area,and fine root turnover rate was correlated with leaf C and P contents.We did not find any relationships between necromass and leaf traits in the two plantations.

    Influence of multiple factors on fine roots

    The relationships between fine roots and multiple factors(including soil and leaf properties) were further analyzed by stepwise regressions (Table 5).The results showed that fine root biomass in black locust could be explained by soil P and leaf area index,and fine root production and turnover rate was closely related to soil volumetric water and leaf area index.Fine root necromass was related to soil P.In Chinese pine plantations,fnie root biomass could be explained by soil N and volumetric water contents.Fine root production and turnover rate were related to soil volumetric water and leaf C contents,and fine root necromass to soil N.In the two plantations,fine root biomass and necromass were closely related to soil nutrient contents (N or P),while fine root production and turnover rate shared similar major explanatory variables.

    Table 2 Two-way ANOVA summary of the effects of stand density and tree species on fine root variables

    Table 3 Pearson correlation coefficients between fine root characteristics and soil properties in the two plantations

    Table 4 Pearson correlation coefficients between fine root characteristics and leaf properties in the two plantations

    Table 5 Stepwise regressions for the effects of soil and leaf properties on fine root characteristics in the two plantations

    Discussion

    Changes in soil and leaf traits along the stand density gradient

    Stand density influences soil environments by affecting the availability of nutrients (Bo et al.2018),and is regarded as one of the most significant factors influencing nutrient fluctuations (Zheng et al.2020).In black locust plantations,soil C and N contents showed a cumulative trend in low stand densities,peaked at density class III,then decreased slightly with increasing density.Organic C and N content were closely related on a small scale to stand density (Chen 2006).A possible reason may be that more sunlight and throughfall are available in relatively lower density stands,which would result in greater litterfall decomposition rates.In forests with N-fixing species,such as black locust,rapid litterfall decomposition often results in the accumulation of organic matter and N in the soil (Tateno et al.2007).The results of this study suggest that this promotional effect was weakened with increasing stand density.Soil P content decreased with increasing density,which is consistent with results reported previously (He et al.2005;Zeng et al.2020).This may be because N-fixation is accompanied by high energy costs and increases the P demand required to synthesize the energy product ATP,a molecule that carries energy within cells(Reed et al.2011;Schleuss et al.2020).High consumption and insufficient sources caused a decline in soil P content with increasing stand density.In Chinese pine plantations,there were no clear trends in changes of soil nutrients with stand density.The ectomycorrhizal mycobiont of the root system of Pinaceae,which is involved in nutrient uptake and circulation (Chu et al.2016),may counteract the effect of stand density on soil nutrients,although stands planted at higher densities are believed to have a larger demand for soil resources (Will et al.2005).Compared with deciduous leaves,the poor decomposition of needle litter slows down the recycling of nutrients (Yuste et al.2005).In high density stands,this is often accompanied by a higher interception of precipitation in crowns and interception of throughfall in thicker litterfall layers on the soil surface.The lack of water replenishment in the soil,coupled with the high consumption in high density stands,caused the decline in soil volumetric water content with increasing density.

    In this study,leaf nutrient contents did not show a clear trend with stand density.Forest nutrient cycling is governed by numerous inter-related processes and factors (Paluch andGruba 2010).Leaf nutrient content is a result of complex processes combined with nutrient uptake,allocation,and resorption (Wright and Westoby 2003;Tsujii et al.2020).However,tree species have specific physiological and biological processes,and coupled with environmental conditions,influence nutrient content in leaves that vary with adaptation and resilience (Cao et al.2018).Therefore,standdensity may be a relatively weak factor affecting leaf nutrient content.Specific leaf area and leaf area index showed clear,similar trends with stand density in the two plantations.Individual trees may adapt to decreasing light levels caused by high stand density by increasing single leaf area and leaf quantity.Higher specific leaf area is in line with the poorer conservation of the acquired resources and stronger nutrient return,thus leading to faster nutrient cycling (Wright et al.2002).The forest canopy has sufficient sunlight,competition between individuals is weak,and the demand for photosynthetic carbohydrates is lower in low density stands,so leaf area is relatively small.As stand density increases,sunlight in the forest weakens and competition between individuals increases.A larger leaf area is required to increase the interception of sunlight.When the stand density is excessive,leaves may divert more energy and nutrients toward the synthesis of defense compounds to resist and adapt to the stress caused by weak sunlight and neighbor competition,which explains the decrease in both leaf area index and specific leaf area.

    Effect of stand density on fine roots

    Along the density gradient,the increasing tendencies of fine root biomass,necromass and production were similar in both plantations.This could be attributed to the stands were in early stage of development (Table 1).At this stage,low competition promotes production,leading to higher fine root production in higher density stands (He et al.2005;Li et al.2011).However,this effect would be negligible when the stand density exceeds a threshold value (He et al.2005).This might explain the insignificance in fine root biomass and production between density classes III and IV.

    The vertical distribution of fine roots followed similar patterns in these plantations.Both fine root production and biomass gradually decreased along the soil profile (0–80 cm)in each density class (Appendix Figs.S1,2).In both plantations,there were larger significant differences among the density classes in the upper soil layers than in the deeper layers.Allocation percentage of fine roots in deeper soil layers increased with increasing stand density,suggesting that intensified competition by increased stand density would result in more roots being forced into the deeper soil to acquire resources (Prieto et al.2015).

    Unlike biomass and production,the response of fine root turnover rate to stand density showed subtle differences.In Chinese pine plantations,fine root turnover rate did not increase significantly (classes I to III,stand density <3500 ind.ha?1) until the density was excessive (class IV,>6500 ind.ha?1).However,there were larger significant differences among density classes in fine root turnover rate in black locust plantations,which may have been caused by differences in genetics and/or adaptation to environmental changes between species (Eissenstat and Yanai 2002;Wang et al.2020).Black locust is considered a fast-growing species (Campagnaro et al.2018;He et al.2020),and therefore has a higher turnover rate.However,Chinese pine is a species which has a relatively conservative growth strategy (Yan et al.2006).These results suggest that black locust ensures high fine root biomass by increasing fine root production and turnover rate with increasing stand density,whereas Chinese pine does so by increasing fine root production;only when stand density increases significantly,does the fine root turnover rate increase significantly.

    Response of fine roots to soil properties

    The availability of soil resources is a key driver of production and ecosystem processes (van der Sande et al.2018).There were significant correlations between fine root biomass,fine root production,and soil resources in the two plantations.Fine root biomass and necromass were affected by soil N and P content,especially N according to the results of stepwise regressions (Tables 3 and 5) in black locust plantations.The weak relationships between soil N,fine root production,and fine root turnover rate may be attributable to specific N fixation characteristics,resulting in less N limitation (Tateno et al.2007).In addition,fine root production and turnover rate were negatively related to soil P content.These results support the hypothesis that plants preferentially allocate more resources to roots on sites with low soil moisture and poor nutrients (Garnier 1991;Gao et al.2020).In Chinese pine plantations,the positive relationship between soil N and fine root biomass could be explained by the conservation nutrient use strategies employed by Chinese pine.As Chinese pine has lower leaf N and P contents,longer leaf life,and slower litter decomposition than those of black locust,the nutrient-use strategy by Chinese pine is more conservative than black locust (Yan et al.2006;Chen et al.2018).Lower N utilization and leaf N content,and slower nutrient cycling allow Chinese pine to be beneficial in infertile habitats.In the two plantations,there were negative relationships between both fine root production and turnover rate and soil volumetric water content.A more likely explanation might be that plants resisting drought stress would allocate more biomass to roots (Davis et al.2004) by promoting the proliferation of fine roots to effi-ciently exploit the soil resources.Our results are consistent with the optimal resource partitioning theory (Hertel et al.2013).Nevertheless,these relationships between fine root biomass,production,and turnover rate and soil properties are not constant because fine roots grow and turnover rapidly as available nutrients increase,which would result in a decline in net fine root biomass (Yuan and Chen 2010).

    Correlation between fine roots and leaf traits

    Leaves and fine roots share attributes that suggest they may have similar trait syndromes:a relatively short life span,a primary function of resource acquisition,and typical determinate growth (Eissenstat and Yanai 1997;Withington et al.2006).In the black locust plantations,fine root biomass and production were positively related to stand leaf area index.In forests,leaf area is the trade-offinterface between photosynthetically active organs of the vegetation and the atmosphere,and affects the light,thermal,and hydric conditions within the canopy (Wright et al.2004;Kalacska et al.2005).Therefore,larger leaf area had greater light interception,resulting in more energy for root activity.However,fine root turnover rate was not only related to leaf area index,but was also explained by leaf P content.Black locust is known for its N-fixation properties which may result in P being a limiting factor for photosynthesis (Reed et al.2011).The production of photosynthesis,however,drives fine root activity (Du and Fang 2014;Meng et al.2018),which seems to be a more likely explanation.In contrast to black locust plantations,fine root production and turnover rate were closely related to leaf C content in Chinese pine plantations.Leaves are the main organ for C assimilation,and their C content reflects their adaptability to the external environment (Wright et al.2004).Evergreen needles are believed to sequester carbon concurrently with needles of the previous year,directly providing C to maintain growth (Cao et al.2018).Therefore,leaf C content is an important factor in the physiological processes of Chinese pine.This might explain the close correlation between fine root dynamics (fine root production and turnover rate) and C content in needles.In addition,a feedback loop has been proposed between leaf nutrient contents,fine root production,and soil nutrient conditions(Cote et al.2003);more relevant information is needed to complement this loop.

    On the other hand,the spatio-temporal heterogeneity of fine roots in the plantations and the relatively small number of plots might result in some limitations in this study.Although the relationships between density-based fine roots and soil and leaf characteristics were analyzed,we were unable to analyze these along the stand density gradients.In consideration of this limitation,the number of plots in each stand density class should be increased in future investigations,and the relationships between fine roots,soil and leaves with density gradients analyzed more comprehensively.

    Conclusions

    In the black locust plantations,soil carbon and nitrogen accumulated with stand density at relatively lower densities,while soil phosphorous and volumetric water contents constantly decreased.In the Chinese pine plantations,carbon,nitrogen and phosphorous contents did not show a clear trend with stand density.The changing trend of soil volumetric water contents was similar to that in the black locust plantations.In the black locust plantations,high fine root biomass in the higher density stand was maintained by increasing fine root production and turnover rate with increasing stand density.In the Chinese pine plantations,fine root biomass increased with stand density was achieved by increasing the fine root production.When stand density was excessive,fine root turnover rate increased significantly to ensure higher biomass.Fine root biomass,especially necromass,was related to soil phosphorous content in the black locust plantations and nitrogen content in the Chinese pine plantations,and fine root production and turnover rate were related to soil moisture in the two plantations.Fine root biomass,production and turnover rate were closely correlated to leaf area index in the black locust stands.In the Chinese pine plantations,fine root production and turnover rate were related to leaf carbon contents.

    AcknowledgementsWe gratefully acknowledge our group members,mainly graduate students from Northwest A &F University and the University of Chinese Academy of Sciences for their contributions to the field investigations.

    Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License,which permits use,sharing,adaptation,distribution and reproduction in any medium or format,as long as you give appropriate credit to the original author(s) and the source,provide a link to the Creative Commons licence,and indicate if changes were made.The images or other third party material in this article are included in the article’s Creative Commons licence,unless indicated otherwise in a credit line to the material.If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use,you will need to obtain permission directly from the copyright holder.To view a copy of this licence,visit http:// creat iveco mmons.org/l icen ses/ by/4.0/.

    中文字幕久久专区| 欧美成人a在线观看| 在线免费观看的www视频| 国产男人的电影天堂91| 亚洲欧洲日产国产| 日本爱情动作片www.在线观看| 久久精品综合一区二区三区| 日日撸夜夜添| 26uuu在线亚洲综合色| 汤姆久久久久久久影院中文字幕 | 亚洲精品一二三| av在线老鸭窝| 成人亚洲精品av一区二区| 午夜精品国产一区二区电影 | 夫妻午夜视频| a级毛片免费高清观看在线播放| 美女黄网站色视频| 国产成人福利小说| 亚洲自偷自拍三级| 免费观看a级毛片全部| 男女边摸边吃奶| 男女啪啪激烈高潮av片| 国产高潮美女av| 免费观看av网站的网址| 久久久久久久久久久免费av| 午夜免费观看性视频| 蜜桃亚洲精品一区二区三区| 国产美女午夜福利| 久久国内精品自在自线图片| 麻豆成人午夜福利视频| 丰满少妇做爰视频| 国产精品女同一区二区软件| 成人特级av手机在线观看| 国产精品三级大全| 国产一区亚洲一区在线观看| 高清日韩中文字幕在线| 国产乱人视频| 精品熟女少妇av免费看| 国产老妇女一区| 99视频精品全部免费 在线| 人人妻人人澡人人爽人人夜夜 | 九九在线视频观看精品| .国产精品久久| av.在线天堂| h日本视频在线播放| 波多野结衣巨乳人妻| 日日啪夜夜爽| 极品教师在线视频| 日韩欧美国产在线观看| 亚洲国产精品国产精品| 色尼玛亚洲综合影院| 色视频www国产| 在现免费观看毛片| 最近2019中文字幕mv第一页| 蜜桃亚洲精品一区二区三区| 国产免费又黄又爽又色| 中文在线观看免费www的网站| 欧美成人午夜免费资源| 免费人成在线观看视频色| 大又大粗又爽又黄少妇毛片口| 久久久a久久爽久久v久久| 精品久久久久久成人av| 日日啪夜夜爽| 午夜视频国产福利| 又爽又黄a免费视频| 欧美日韩亚洲高清精品| 久久草成人影院| 女人被狂操c到高潮| 国产69精品久久久久777片| 秋霞在线观看毛片| 狂野欧美白嫩少妇大欣赏| 又爽又黄无遮挡网站| 久久97久久精品| 国内精品宾馆在线| 成人性生交大片免费视频hd| 老司机影院成人| 好男人在线观看高清免费视频| 精品一区在线观看国产| 日本免费a在线| 欧美xxxx黑人xx丫x性爽| 能在线免费观看的黄片| 成人亚洲精品av一区二区| 国产色爽女视频免费观看| 观看免费一级毛片| 亚洲精品成人av观看孕妇| 在现免费观看毛片| 美女高潮的动态| 麻豆乱淫一区二区| 五月天丁香电影| 91久久精品国产一区二区成人| 国产黄色小视频在线观看| 欧美zozozo另类| 男人和女人高潮做爰伦理| 婷婷色av中文字幕| 午夜精品国产一区二区电影 | 搡老妇女老女人老熟妇| 日本一二三区视频观看| 少妇熟女欧美另类| 女人被狂操c到高潮| 免费黄色在线免费观看| 最近2019中文字幕mv第一页| 国产精品美女特级片免费视频播放器| 51国产日韩欧美| 能在线免费观看的黄片| 男女视频在线观看网站免费| 亚洲av男天堂| 亚洲欧美精品专区久久| 日本免费在线观看一区| 日本-黄色视频高清免费观看| 色网站视频免费| 男女啪啪激烈高潮av片| 免费观看av网站的网址| 中文字幕av成人在线电影| 精品少妇黑人巨大在线播放| 亚洲精品一二三| 高清午夜精品一区二区三区| 22中文网久久字幕| 国产午夜福利久久久久久| 大话2 男鬼变身卡| 少妇高潮的动态图| 可以在线观看毛片的网站| 韩国av在线不卡| 中文乱码字字幕精品一区二区三区 | 亚洲欧美清纯卡通| 能在线免费观看的黄片| 国产精品嫩草影院av在线观看| 插阴视频在线观看视频| 在线免费十八禁| 水蜜桃什么品种好| 日韩一区二区三区影片| 成年免费大片在线观看| 蜜桃亚洲精品一区二区三区| 乱码一卡2卡4卡精品| 欧美潮喷喷水| 亚洲av中文字字幕乱码综合| 国产高清三级在线| 国产激情偷乱视频一区二区| 成人午夜精彩视频在线观看| 成人高潮视频无遮挡免费网站| 国产乱人视频| 少妇被粗大猛烈的视频| 欧美区成人在线视频| 国产精品一区二区在线观看99 | 国产av不卡久久| 97超视频在线观看视频| av在线播放精品| 国产淫片久久久久久久久| 麻豆精品久久久久久蜜桃| 在线观看人妻少妇| 日日摸夜夜添夜夜添av毛片| 国产白丝娇喘喷水9色精品| 亚洲精品一二三| 欧美激情久久久久久爽电影| 国产在线男女| 成年版毛片免费区| 一个人看的www免费观看视频| 国产精品国产三级专区第一集| 男人舔女人下体高潮全视频| 2018国产大陆天天弄谢| 一级毛片我不卡| 欧美 日韩 精品 国产| 国产探花在线观看一区二区| 久久精品熟女亚洲av麻豆精品 | 少妇人妻一区二区三区视频| 九色成人免费人妻av| 天美传媒精品一区二区| 秋霞在线观看毛片| 亚洲av不卡在线观看| 成年女人在线观看亚洲视频 | 国内精品美女久久久久久| 免费电影在线观看免费观看| 国精品久久久久久国模美| 久热久热在线精品观看| 久久亚洲国产成人精品v| 亚洲精品aⅴ在线观看| 日韩精品有码人妻一区| 在线观看美女被高潮喷水网站| 免费黄色在线免费观看| 精品久久久噜噜| 人体艺术视频欧美日本| 26uuu在线亚洲综合色| 青春草亚洲视频在线观看| 亚洲av免费高清在线观看| 蜜桃亚洲精品一区二区三区| 国产高清三级在线| 99re6热这里在线精品视频| 亚洲国产高清在线一区二区三| 22中文网久久字幕| 最新中文字幕久久久久| 亚洲av成人av| 久久久久久久午夜电影| 国产精品久久视频播放| av女优亚洲男人天堂| av女优亚洲男人天堂| 女的被弄到高潮叫床怎么办| 亚洲天堂国产精品一区在线| 国产淫语在线视频| 搞女人的毛片| av网站免费在线观看视频 | 激情五月婷婷亚洲| 一级毛片我不卡| 少妇熟女欧美另类| 日产精品乱码卡一卡2卡三| 自拍偷自拍亚洲精品老妇| 亚洲美女视频黄频| 亚洲av免费在线观看| 91精品伊人久久大香线蕉| 男人爽女人下面视频在线观看| 国产精品久久久久久久久免| 美女被艹到高潮喷水动态| 大陆偷拍与自拍| 欧美区成人在线视频| 精品国产三级普通话版| 美女xxoo啪啪120秒动态图| 在线免费十八禁| 亚洲人成网站在线播| 在线播放无遮挡| 午夜福利在线观看免费完整高清在| 男的添女的下面高潮视频| 亚洲精品乱码久久久久久按摩| 精品国产三级普通话版| 日本免费a在线| 日韩亚洲欧美综合| 精品久久久久久成人av| 91狼人影院| 三级男女做爰猛烈吃奶摸视频| 日本与韩国留学比较| 国产男人的电影天堂91| 日本欧美国产在线视频| 久久精品国产鲁丝片午夜精品| 天天一区二区日本电影三级| 中文天堂在线官网| 久久久精品94久久精品| 国产黄色视频一区二区在线观看| 天堂网av新在线| 日本免费在线观看一区| 国产 一区精品| 中文精品一卡2卡3卡4更新| 最近中文字幕高清免费大全6| 在线免费观看不下载黄p国产| 国产成人精品一,二区| av福利片在线观看| 国产精品久久久久久精品电影| 嫩草影院入口| 午夜激情福利司机影院| 色尼玛亚洲综合影院| 欧美区成人在线视频| 最近最新中文字幕免费大全7| 男女视频在线观看网站免费| 国产一级毛片在线| 日日摸夜夜添夜夜添av毛片| 男人舔奶头视频| 一级毛片电影观看| 最近2019中文字幕mv第一页| 可以在线观看毛片的网站| 成人毛片a级毛片在线播放| 国产精品三级大全| 亚洲国产精品成人久久小说| 国产欧美日韩精品一区二区| 天天躁夜夜躁狠狠久久av| 国产精品三级大全| 麻豆乱淫一区二区| 白带黄色成豆腐渣| 黑人高潮一二区| 最近的中文字幕免费完整| 精品国内亚洲2022精品成人| 国产免费一级a男人的天堂| 亚洲内射少妇av| 日韩一区二区三区影片| 欧美+日韩+精品| 日韩av在线免费看完整版不卡| 一级a做视频免费观看| 中文乱码字字幕精品一区二区三区 | 丝瓜视频免费看黄片| 国产在线男女| 婷婷色麻豆天堂久久| 一级二级三级毛片免费看| 国产人妻一区二区三区在| 亚洲av在线观看美女高潮| 九草在线视频观看| 美女主播在线视频| av国产久精品久网站免费入址| 精品久久久久久久久久久久久| 精品熟女少妇av免费看| 国产黄a三级三级三级人| 麻豆精品久久久久久蜜桃| 亚洲最大成人中文| 国产精品久久久久久精品电影| 亚洲精品日本国产第一区| 国产在线男女| 国产 一区精品| 久久午夜福利片| 亚洲三级黄色毛片| 久久99蜜桃精品久久| av卡一久久| 夜夜爽夜夜爽视频| 精品人妻视频免费看| 亚洲国产最新在线播放| 免费观看精品视频网站| 午夜日本视频在线| 日日摸夜夜添夜夜爱| 国产一级毛片在线| 三级毛片av免费| 国产伦一二天堂av在线观看| 五月伊人婷婷丁香| 日韩成人av中文字幕在线观看| 亚洲美女搞黄在线观看| 一个人看的www免费观看视频| 国产 亚洲一区二区三区 | 国产男人的电影天堂91| 亚洲国产精品成人久久小说| 日韩成人伦理影院| 菩萨蛮人人尽说江南好唐韦庄| 在线观看免费高清a一片| 99久久人妻综合| 国产高潮美女av| 欧美日韩视频高清一区二区三区二| 亚洲精品乱码久久久v下载方式| 三级国产精品欧美在线观看| 搡老乐熟女国产| 欧美高清性xxxxhd video| 1000部很黄的大片| 国产黄色小视频在线观看| 午夜久久久久精精品| 日韩人妻高清精品专区| 校园人妻丝袜中文字幕| 久久久久久久久久久丰满| 91久久精品电影网| 日本爱情动作片www.在线观看| 免费少妇av软件| 日本色播在线视频| 亚洲四区av| 欧美日本视频| 久久99热这里只有精品18| 亚洲av.av天堂| 久久久亚洲精品成人影院| 精品国产一区二区三区久久久樱花 | www.色视频.com| 日韩一区二区三区影片| 欧美最新免费一区二区三区| 色综合亚洲欧美另类图片| 日本黄色片子视频| 22中文网久久字幕| 能在线免费看毛片的网站| 亚洲精华国产精华液的使用体验| 免费av毛片视频| 99热全是精品| 九九在线视频观看精品| 在线观看美女被高潮喷水网站| 成人美女网站在线观看视频| 亚洲成人中文字幕在线播放| 男人爽女人下面视频在线观看| 国产成人精品福利久久| 色综合站精品国产| 中文字幕人妻熟人妻熟丝袜美| 中文欧美无线码| 男人和女人高潮做爰伦理| www.av在线官网国产| 国产视频首页在线观看| 国产高清三级在线| 又大又黄又爽视频免费| 禁无遮挡网站| 99re6热这里在线精品视频| 亚洲欧洲国产日韩| 高清午夜精品一区二区三区| 日本猛色少妇xxxxx猛交久久| 国产精品一二三区在线看| 久久久久久久久久久免费av| 亚洲精品国产成人久久av| 亚洲人成网站高清观看| 91av网一区二区| 大香蕉97超碰在线| 精品少妇黑人巨大在线播放| 日本猛色少妇xxxxx猛交久久| 国产亚洲av片在线观看秒播厂 | 国内揄拍国产精品人妻在线| 国语对白做爰xxxⅹ性视频网站| 精品亚洲乱码少妇综合久久| 汤姆久久久久久久影院中文字幕 | 久久久久网色| 精品酒店卫生间| 男女国产视频网站| 免费人成在线观看视频色| 热99在线观看视频| 大香蕉97超碰在线| 亚洲性久久影院| 国产精品一及| 国产乱来视频区| 日本黄大片高清| 丝袜美腿在线中文| 赤兔流量卡办理| 99久久中文字幕三级久久日本| 亚洲精品456在线播放app| 麻豆久久精品国产亚洲av| 国产精品一及| 噜噜噜噜噜久久久久久91| 国产色爽女视频免费观看| 26uuu在线亚洲综合色| 一级av片app| 国产精品国产三级专区第一集| 春色校园在线视频观看| 人妻一区二区av| 亚洲av免费在线观看| 国产麻豆成人av免费视频| 欧美+日韩+精品| 国国产精品蜜臀av免费| 99热这里只有精品一区| 成人毛片60女人毛片免费| 最近中文字幕高清免费大全6| 国产伦精品一区二区三区四那| 色综合亚洲欧美另类图片| 又爽又黄无遮挡网站| 国内少妇人妻偷人精品xxx网站| av国产久精品久网站免费入址| 亚洲,欧美,日韩| 色哟哟·www| 中文在线观看免费www的网站| av免费观看日本| 国产精品一二三区在线看| 边亲边吃奶的免费视频| 久久午夜福利片| 国产成人freesex在线| 精品一区在线观看国产| 久久久久久久亚洲中文字幕| 草草在线视频免费看| 男人狂女人下面高潮的视频| 久久久午夜欧美精品| 精品一区二区三区视频在线| 精品国产一区二区三区久久久樱花 | 国产亚洲最大av| 成人美女网站在线观看视频| 又大又黄又爽视频免费| 超碰97精品在线观看| 久久热精品热| 精品久久久久久久末码| 人妻一区二区av| 日韩强制内射视频| 天堂影院成人在线观看| 亚洲精品,欧美精品| 简卡轻食公司| 精品熟女少妇av免费看| 一二三四中文在线观看免费高清| 一级毛片aaaaaa免费看小| 亚洲综合色惰| 欧美成人精品欧美一级黄| 亚洲激情五月婷婷啪啪| 国产亚洲精品久久久com| 看免费成人av毛片| a级毛片免费高清观看在线播放| 日本一本二区三区精品| 亚洲国产av新网站| 特大巨黑吊av在线直播| 国产黄频视频在线观看| 简卡轻食公司| 寂寞人妻少妇视频99o| 97热精品久久久久久| 国产成人精品福利久久| 青青草视频在线视频观看| 99久久精品一区二区三区| 日韩欧美三级三区| 国产精品一区www在线观看| 日本熟妇午夜| 一级毛片久久久久久久久女| 国产精品人妻久久久影院| 久久热精品热| 国内精品宾馆在线| 高清午夜精品一区二区三区| 国产成人a∨麻豆精品| 成人高潮视频无遮挡免费网站| 美女xxoo啪啪120秒动态图| 少妇的逼水好多| 国国产精品蜜臀av免费| 免费观看精品视频网站| 日韩三级伦理在线观看| 天堂影院成人在线观看| 99久久精品热视频| 国产久久久一区二区三区| 91av网一区二区| 麻豆av噜噜一区二区三区| 男女边摸边吃奶| 日本黄色片子视频| 亚洲av.av天堂| 精品久久久久久久人妻蜜臀av| 嫩草影院新地址| 大陆偷拍与自拍| 成人av在线播放网站| 天天躁夜夜躁狠狠久久av| 蜜桃亚洲精品一区二区三区| 97超视频在线观看视频| 91精品一卡2卡3卡4卡| 91精品伊人久久大香线蕉| 精品一区二区三区人妻视频| 国产69精品久久久久777片| 久久久成人免费电影| 日韩一区二区视频免费看| 日本免费a在线| 99视频精品全部免费 在线| 久久精品夜色国产| 国产精品av视频在线免费观看| 大又大粗又爽又黄少妇毛片口| 美女xxoo啪啪120秒动态图| 三级男女做爰猛烈吃奶摸视频| 熟女人妻精品中文字幕| 看非洲黑人一级黄片| 精品久久久噜噜| 综合色丁香网| 成年女人看的毛片在线观看| 免费看av在线观看网站| 爱豆传媒免费全集在线观看| 麻豆成人av视频| 久久久久九九精品影院| 久久久久久九九精品二区国产| 特大巨黑吊av在线直播| 一级片'在线观看视频| 国产探花极品一区二区| 禁无遮挡网站| 亚洲自拍偷在线| 丝袜喷水一区| 少妇裸体淫交视频免费看高清| 在线天堂最新版资源| 一级黄片播放器| 成人国产麻豆网| 国产伦精品一区二区三区四那| 成人午夜高清在线视频| 中文天堂在线官网| 99热这里只有精品一区| 国国产精品蜜臀av免费| 人人妻人人澡人人爽人人夜夜 | 99久久精品一区二区三区| 成人午夜高清在线视频| 一区二区三区高清视频在线| 亚洲国产成人一精品久久久| 国产精品一区二区三区四区久久| 日本熟妇午夜| 亚洲国产精品成人久久小说| 又大又黄又爽视频免费| 精品久久久久久久人妻蜜臀av| 毛片一级片免费看久久久久| 男女边摸边吃奶| 直男gayav资源| 国产视频首页在线观看| 欧美区成人在线视频| 青春草国产在线视频| 免费电影在线观看免费观看| 高清视频免费观看一区二区 | 2021天堂中文幕一二区在线观| av黄色大香蕉| 一级二级三级毛片免费看| 一级毛片黄色毛片免费观看视频| 干丝袜人妻中文字幕| 亚洲精品乱久久久久久| 日本熟妇午夜| 国产精品一区www在线观看| 日韩不卡一区二区三区视频在线| 看黄色毛片网站| 亚洲婷婷狠狠爱综合网| 亚洲精品日韩在线中文字幕| videos熟女内射| 少妇裸体淫交视频免费看高清| 日本黄大片高清| 欧美极品一区二区三区四区| 久久久久久久午夜电影| 精品国产一区二区三区久久久樱花 | av播播在线观看一区| 亚洲av成人精品一区久久| 视频中文字幕在线观看| 边亲边吃奶的免费视频| 亚洲图色成人| 青春草亚洲视频在线观看| 精品熟女少妇av免费看| 亚洲国产成人一精品久久久| 成人特级av手机在线观看| 国内精品一区二区在线观看| 国产麻豆成人av免费视频| 久久久成人免费电影| 人妻一区二区av| 久久久久网色| 亚洲国产av新网站| 国产伦在线观看视频一区| 老司机影院成人| 亚洲av成人精品一二三区| 亚洲国产日韩欧美精品在线观看| 国内精品宾馆在线| 久久久久精品久久久久真实原创| 人人妻人人看人人澡| 高清欧美精品videossex| 少妇被粗大猛烈的视频| 久久久久久久久中文| 春色校园在线视频观看| 日韩中字成人| 国产成人午夜福利电影在线观看| 最后的刺客免费高清国语| 久久国产乱子免费精品| 日韩欧美一区视频在线观看 | 久久精品人妻少妇| 免费黄频网站在线观看国产| 久久97久久精品| 婷婷色麻豆天堂久久| 99热这里只有是精品50| 色播亚洲综合网| 国产三级在线视频| 国产淫语在线视频| 好男人视频免费观看在线| 国产一区二区三区av在线| 国产伦精品一区二区三区四那| 一区二区三区乱码不卡18| 亚洲成人中文字幕在线播放| 波多野结衣巨乳人妻| 99久久精品国产国产毛片| 免费播放大片免费观看视频在线观看| 久久亚洲国产成人精品v| 麻豆成人午夜福利视频| 99热网站在线观看| 看免费成人av毛片| 99热全是精品|