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101.
土壤活性有机碳的表征及其生态效应 总被引:147,自引:10,他引:147
土壤活性有机碳指在一定的时空条件下,受植物、微生物影响强烈、具有一定溶解性、在土壤中移动比较快、不稳定、易氧化、分解、易矿化,其形态,空间位置对植物、微生物来说活性比较高的那一部分土壤碳素。国外描述这一部分碳素的术语为有效碳、水溶性碳、易氧化碳、可矿... 相似文献
102.
103.
By Martin A. Smith William A. Loneragan Carl D. Grant John M. Koch 《Ecological Management & Restoration》2000,1(1):50-60
Summary Germinable seed stores of 5- and 8-year-old rehabilitated bauxite mine pits in south-west Western Australia were assessed before and after burning. These seed stores were compared to those of adjacent unmined Jarrah ( Eucalyptus marginata ) forest, to identify at what age fire can be reintroduced, in order to measure restoration success and reduce fire hazard. Soils were sampled in early summer (before fire) and late autumn (after fire). Before fire, the mean topsoil seed bank of 5-year-old sites was 2121 seeds per m2 while 8-year-old sites had a mean of 1520 seeds per m2 . Only the 5-year-old sites were significantly different from the forest mean of 1478 seeds per m2 for the same season. After summer burns (and possibly due to seasonal effects) topsoil seed banks of rehabilitated areas (sampled in autumn) decreased by an average of 53 per cent. Topsoil seed banks of 5–8-year-old sites were resistant to lower intensity burns, with 362 seeds per m2 of native species surviving mild burns and 108 seeds per m2 of native species surviving after an intense summer fire. The topsoil seed reserve of 5–8-year-old rehabilitated areas had a high proportion of annual weed species while the forest sites had high levels of subshrubs and native annuals. Low-intensity burns did not alter the composition of life-forms in the soil seed bank, while intense burns favoured annual weed and shrub species. The results indicate that it is not appropriate to introduce fire to rehabilitated areas before 8 years, due to limited fuel reduction benefits and possible adverse effects on obligate seeding species. The large proportion of weed species in the soil seed bank of young rehabilitated areas is a concern, and remains a major consideration for future disturbance of these areas. 相似文献
104.
105.
不同群落类型柔毛淫羊藿总黄酮和淫羊藿苷含量及其与土壤因子的关系 总被引:3,自引:0,他引:3
2009年8月,采用高效液相色谱法和紫外分光光度法测定了唐家河自然保护区次生落叶阔叶林红桦群落(群落Ⅰ)、常绿落叶阔叶混交林细叶青冈群落(群落Ⅱ)和常绿阔叶林油樟群落(群落Ⅲ)下生长的柔毛淫羊藿各器官的总黄酮和淫羊藿苷含量,分析其与土壤因子的关系结果表明:柔毛淫羊藿叶片中总黄酮和淫羊藿苷含量最高、茎中最低;群落Ⅰ的柔毛淫羊藿总黄酮和淫羊藿苷含量[(5.32±0.23)%和(0.47±0.05)%]均显著高于群落Ⅱ[(4.06±0.03)%和(0.32±0.01)%]和群落Ⅲ[(4.15±0.07)%和(0.28±0.09)%];土壤氮含量和pH值对柔毛淫羊藿的总黄酮和淫羊藿苷含量影响较大,柔毛淫羊藿总黄酮和淫羊藿苷含量与土壤全氮和碱解氮呈显著负相关(P<0.05),与土壤pH值呈极显著正相关(P<0.01).土壤较低的氮供应水平和较高的土壤酸度可能使群落Ⅰ柔毛淫羊藿的总黄酮和淫羊藿苷含量增加. 相似文献
106.
黄土高原子午岭油松林的种子雨和土壤种子库动态 总被引:7,自引:1,他引:7
对黄土高原区子午岭不同林龄(18a、29a、40a、54a)油松(Pinus tabulaeformis carr.)人工林及天然林(约75a)的种子雨和土壤种子库进行了研究.结果表明,该区油松种子雨一般从每年9月初开始,一直到11月底结束,种子雨降落历程与林龄大小有关,种子雨发生时间和降落高峰期有所不同.不同林龄的油松种子雨强度不同,种子雨总量大小顺序为:40a人工林((489 9±8.64)粒· m-2)>29a人工林((346.8±7.45)粒· m-2)>54a人工林((327.1±8.13)粒· m-2)>天然林((146.9±5.25)粒· m-2)>18a人工林((78.1±2.72)粒· m-2).种子雨总量随林龄的增加而增加,约40a时达到高峰,种子雨活力也以40a时最高.不同林龄油松林土壤种子库存在显著差异,其中18a人工林种子库最小,40a人工林种子库最大.从种子雨降落到次年4月,5种林分土壤种子库总量下降了42.34%~53.59%,空粒种子增加了26.72%~48.69%;从4月到8月份种子腐烂率由10.28%~13 62%增加到57.25%~63.28%.动物的搬运、取食和种子腐烂死亡是种子库损耗的主要因素.土壤种子库中的油松种子主要集中在枯枝落叶层,其次为0~2cm层,2~10cm层种子最少.到8月中旬,土壤中98.26%的油松种子都已丧失活性.不同林分下油松幼苗的密度差异较大,40a人工林下幼苗最多,其余依次为29a人工林、54a人工林和天然林,18a人工林下的实生苗极少,幼苗死亡率极高.在一定龄级范围内,人工林结实能力和更新潜力随林龄增加而增加,40a时更新潜力最大.虽然有大量种子下落,但由于种子大量损耗和幼苗死亡,通过环境筛作用而最终可以成熟的个体数量十分有限. 相似文献
107.
Mercury (Hg) is a persistent soil pollutant that affects soil microbial activity. We monitored the changes in soil microbial
biomass and activity of enzymes, including alkaline phosphatase, arylsulfatase, fluorescein diacetate (FDA) hydrolytic activity,
and o-diphenol oxidase (o-DPO) in three soils contaminated with different concentrations of Hg. Increasing levels of Hg, from 0.5 to 10 μmol/g of dried
soil, generally depressed microbial activity; however, the effects of Hg on soil microbial activity depended on soil type
and composition, particularly organic matter content. o-DPO was less affected by Hg than the other three enzymes tested. Our results indicate that the analysis of microbial biomass
content and soil-enzyme activities may be used to predict the soil quality contaminated with Hg. 相似文献
108.
109.
Varunendra Singh Rawat Jasleen Kaur Sakshi Bhagwat Manisha Arora Pandit Charu Dogra Rawat 《Restoration Ecology》2023,31(1):e13688
Ecosystem degradation is a major environmental threat. Beyond conservation, restoration of degraded ecosystems is a prerequisite to reinstate their ability to provide essential services and benefits. Most of the restoration efforts focus on aboveground restoration, that is, plants, under the assumption that establishment of plant species will reestablish the faunal and microbial species. While this may be true for some cases, it is not a general rule. Reestablishment of microbial communities by dedicated efforts is also necessary for successful restoration, as cycling of essential nutrients for plant growth and decomposition of organic matter is dependent on them. The role of microbial fertilizers and efficient organisms used in agriculture needs to be explored in restoration. Testing of symbiotic interactions between potential plant growth-promoting Rhizobacteria and plants native to a degraded ecosystem can be conducted and utilized for successful establishment of plant species. However, utmost care must be taken while introducing new microbial species or non-native plant species to an area, as they can adversely affect the resident microbial community. Techniques like phospholipid fatty-acid analysis can be used for taxonomic identification of large microbial groups in non-degraded reference ecosystems before introducing microbial species into a degraded ecosystem. For use of microbes in restoration, more studies on microbe-plant interactions need to be conducted. For use of Soil Microbial Community (SMC) as indicators of restoration, their role and function in the ecology of the area need to be elucidated by employing all the available techniques. 相似文献
110.
Napthalene- and decane-contaminated soils were treated with Triton X-100 (a nonionic surfactant) to characterize the soil-water partitioning behavior of the surfactant in soils with different organic content. Soil samples with different organic content were prepared by mixing sand-mulch mixtures at different proportions. The experimental results indicated that the amount of surfactant sorbed onto soil increased with increasing soil organic content and increasing surfactant concentration. The effective critical micelle concentration (CMC) also increased with increasing organic content in soil. The CMC of Triton X-100 in aqueous systems without soil was about 0.3 mM and the effective CMC values measured for soil-water-surfactant systems (approximately 1:19 soil/water ratio) with 25%, 50%, and 75% mulch content were 0.9, 1.0, and 1.7 mM, respectively. Sub-CMC surfactant sorption was modeled accurately with both the Freundlich and the linear isotherm. The maximum surfactant sorption onto soil varied from 66% to 82% of added surfactant in the absence of contaminant. The effective CMC values for Triton X-100 increased to some extent in the presence of contaminants, as did the maximum surfactant sorption. The maximum surfactant sorbed onto the soil with 75% mulch content increased from 82% for clean soils, to 95% and 96% for soils samples contaminated with naphthalene and decane, respectively. 相似文献