伪潜育土季节性滞水条件下大冷杉毫根动态的研究(Abies grandis Lindl.)

本文对一个25年生大冷杉林在伪潜育土至45cm矿质土壤里,从1987年晚秋滞水期至1988年生长旺盛期的毫根量动态及化学组成变化进行了研究。 滞水期土壤中死根量(5558kg DS/ha)显著高于活根量(3594kg DS/ha)。生长旺盛期初,活根量增加约50％,死根量降低约27％。经过夏季至生长旺盛期末,活根量仍略有增加,死根量继续降低。毫根化学组成分析显示,滞水期活根中K、Mg及Zn离子含量显著低于生长旺盛期,Mn离子含量则明显高于生长旺盛期。这一结果表明,除了与季节性相关的生长节奏因素外,大冷杉毫根生物量的变化主要是由滞水状况所致。     

Biomass, morphology and nutrient contents of fine roots in four Norway spruce stands

Fine root systems may respond to soil chemical conditions, but contrasting results have been obtained from field studies in non-manipulated forests with distinct soil chemical properties. We investigated biomass, necromass, live/dead ratios, morphology and nutrient concentrations of fine roots (<2 mm) in four mature Norway spruce (Picea abies [L.] Karst.) stands of south-east Germany, encompassing variations in soil chemical properties and climate. All stands were established on acidic soils (pH (CaCl₂) range 2.8–3.8 in the humus layer), two of the four stands had molar ratios in soil solution below 1 and one of the four stands had received a liming treatment 22 years before the study. Soil cores down to 40 cm mineral soil depth were taken in autumn and separated into four fractions: humus layer, 0–10 cm, 10–20 cm and 20–40 cm. We found no indications of negative effects of N availability on fine root properties despite large variations in inorganic N seepage fluxes (4–34 kg N ha⁻¹ yr⁻¹), suggesting that the variation in N deposition between 17 and 26 kg N ha⁻¹ yr⁻¹ does not affect the fine root system of Norway spruce. Fine root biomass was largest in the humus layer and increased with the amount of organic matter stored in the humus layer, indicating that the vertical pattern of fine roots is largely affected by the thickness of this horizon. Only two stands showed significant differences in fine root biomass of the mineral soil which can be explained by differences in soil chemical conditions. The stand with the lowest total biomass had the lowest Ca/Al ratio of 0.1 in seepage, however, Al, Ca, Mg and K concentrations of fine roots were not different among the stands. The Ca/Al ratio in seepage might be a less reliable stress parameter because another stand also had Ca/Al ratios in seepage far below the critical value of 1.0 without any signs of fine root damages. Large differences in the live/dead ratio were positively correlated with the Mn concentration of live fine roots from the mineral soil. This relationship was attributed to faster decay of dead fine roots because Mn is known as an essential element of lignin degrading enzymes. It is questionable if the live/dead ratio can be used as a vitality parameter of fine roots since both longevity of fine roots and decay of root litter may affect this parameter. Morphological properties were different in the humus layer of one stand that was limed in 1983, indicating that a single lime dose of 3–4 Mg ha⁻¹ has a long-lasting effect on fine root architecture of Norway spruce. Almost no differences were found in morphological properties in the mineral soil among the stands, but vertical patterns were apparently different. Two stands with high base saturation in the subsoil showed a vertical decrease in specific root length and specific root tip density whereas the other two stands showed an opposite pattern or no effect. Our results suggest that proliferation of fine roots increased with decreasing base saturation in the subsoil of Norway spruce stands.     

岷江上游干旱河谷地区油松和岷江柏细根生物量和根长密度

了解岷江上游干旱河谷地区12年生油松（Pinus tabulaeformis）和岷江柏（Cupressus chengiana）人工林细根（直径≤2 mm）生物量和根长密度在土层中的垂直分布状况,分析不同土层中细根系统的碳分配策略,为岷江上游干旱河谷地区植被恢复提供理论依据。以岷江上游干旱河谷地区的油松和岷江柏人工林为研究对象,采用土钻法进行取样,测定2种林分不同土层深度（h）（0 cm<h≤15 cm和15 cm<h≤30 cm）中吸收根（1~3级）和运输根（≥4级的细根）生物量和根长密度,以及吸收根占总细根生物量和根长密度比例。结果显示：油松和岷江柏吸收根生物量和根长密度在0 cm<h≤15 cm土层均显著高于15 cm<h≤30 cm土层,而运输根生物量和根长密度在土层间差异均不显著;油松和岷江柏吸收根占总细根生物量和根长密度比例在0 cm<h≤15 cm土层均显著高于15 cm<h≤30 cm土层（P<0.05）;岷江柏吸收根占总细根生物量和根长密度比例在2个土层中均显著高于油松 （P<0.05）。研究结果表明,在养分有效性最高的土壤表层,油松和岷江柏细根系统内将更多的碳分配到吸收根。     

Comparison of biomass allocation in ectomycorrhizal and nonmycorrhizal Douglas fir seedlings of similar nutrition and overall size

Biomass allocation in 6-month-old ectomycorrhizal Douglas fir seedlings was compared to that in nonmycorrhizal seedlings of the same age, nutrient status and total biomass. Seedlings colonized by Rhizopogon vinicolor had the same distribution of biomass between roots, stems and needles, but only 56% of the total length of roots (including mycorrhizal branches) compared to nonmycorrhizal seedlings. Laccaria laccata had no effect on distribution of biomass or root length of seedlings. The results for Rhizopogon provide direct evidence that the process of ectomycorrhizal colonization can significantly affect plant biomass allocation by one or more mechanisms not directly related to altered nutrition or overall plant size.     

Response of fine roots to precipitation change: A meta-analysis北大核心CSCD

Aims The response of fine roots to soil moisture is very sensitive. Climate change scenarios predict changes in precipitation which influence soil moisture directly. Plants optimize resource acquisition by fine root morphological plasticity and biomass redistribution when soil moisture changes. Therefore, it is important to study the effect of precipitation increase and decrease on fine roots and reveal the response of ecosystem carbon cycling to global climate change. Methods We collected 202 sets of data from 48 published domestic and foreign articles, and analized the responses of fine root biomass, production, turnover, root length density, specific root length and soil microbial biomass carbon which reflects fine root decomposition dynamic to precipitation change by the meta-analysis. RR++ (weighted response ratio) was used to quantify the effect size of the response of fine roots to precipitation change. Important findings (1) The significance and magnitude of the precipitation effects on fine roots varied among plant types. Shrub fine roots had stronger response than tree fine roots. (2) The response of fine roots differed across soil depth. Fine root had most significant responses when the precipitation increased or decreased 50%. A 50% increase in precipitation had a significant positive impact on both fine root biomass in 20–40 cm soil and specific root length in 0–10 cm soil depth. A 50% decreased in precipitation had a significant negative impact on fine root production in 20–40 cm soil but positive impact on root length density in 0–10 cm soil. (3) The duration of experiment affected the response of fine roots, fine roots responded to precipitation changes (increase and decrease) by morphological plasticity in short-term experiments, and by biomass redistribution in long-term experiments. (4) Increasing precipitation contributed to the nutrient release of fine roots, because soil microbes accelerated the decomposability of fine roots due to sufficient substrate resources stimulated their own activity. © 2018 Editorial Office of Chinese Journal of Plant Ecology. All rights reserved.     

秦岭大巴山地啮齿类的生态分布

秦岭大巴山地位于陕西省南部,秦岭山脉是我国东部的第一高山,是这一段地区我国南北方的分界线。秦巴山地是一个农林业发达,自然资源富饶的地区。本文仅就啮齿类在这一地区的生态分布规律和数量状况进行初步探讨,为今后开展对秦巴山地群落生态和生态系统的研究提供一些基础资料。本工作始于1955年,文内所用数据主要是1959至1964年和1978年在周至、户县、眉县、太白县、留坝、阳平关、汉中及南郑等地进行的数量统计。秦巴山地的啮齿类共有31种,隶于2目6科,其区系部分另有专题报道。     

杉木,火力楠纯林及混交林细根周转的研究

系统研究了杉木、火力楠纯林及混交林细根生物量、生产力及年周转率。结果表明,杉木、火力楠纯林及混交林活细根生物量分别为８８０、３０３５和１５６０ｋｇ．ｈａ＾－１;死细根生物量为２３５、３９８和５６５ｋｇ．ｈａ＾－１;细根年周转率为１．２９、１．４２和１．４０;年生产量为１１３７、４３１８和２１７９ｋｇ．ｈａ＾－１;年死亡量为４９７．５９５和１１４９ｋｇ．ｈａ＾－１,分别相当于林分枯枝落叶年凋落量为３     

杨树细根及草根的生产力与周转的研究

对北方杨树人工林0－40cm土层中杨树细根和草根（≤2mm）年生物量、分解量、死亡量、生长量和周转率进行观察研究。结果表明,杨树细根的年生物量为2．062t.hm^-2,死根生物量为0．746t.hm^-2,分解量为0．158t.hm^2,生长量为2．351t.hm^－2,周转率为每年1．14次,活草根的年生物量、死根生物量、分解量、生长量和周转率分别0．501、0．035、0．023、0．691t.hm^-2和1．38,同时给出了杨树细根干重损失随分解时间变化的方程：1nx/x0=0.9515e^-0.0014t。     

Fine root biomass under light gap openings in an Amazon rain forest

Summary Belowground processes in light gap openings are poorly understood, particularly in tropical forests. Fine roots in three zones of light gap openings and adjacent intact forest were regularly measured in buried bags and surface litter envelopes for 2 years. Fine root biomass does not vary significantly within gaps for either buried bags or for surface litter envelopes. When entire gaps are compared without regard for within gap zones, root growth into both surface litter and buried bags is significantly different between gaps, with highest rates of fine root biomass accumulation in the smallest gap. These results suggest that the aboveground within-gap zones do not result in a congruent pattern of below-ground zonation. Gap size, decomposition of the fallen tree, and pre-gap fine root growth rates should be considered to determine fine root growth patterns following the formation of light gap openings.