暖温带地区主要树种叶片凋落物分解过程中主要元素释放的比较

应用分解网袋法对暖温带落叶阔叶林内分布较为优势的辽东栎（Quercus liaotungensis)、五角枫（Acermono)、蒙椴（Tilia mongolica)、糠椴（T.mandshurica)等4种植物叶片凋落物第一年的分解速率损失过程基本符合Olson的指数降解模型。4种凋落物的分解速率（凋落物的年重量损失）依次为五角枫＞糠椴＞蒙椴＞辽乐栎。N、P、Na、Fe、Cu、Mn在几种凋落物残留物中各自有不同程度的富集。C、K含量显著单调下降,其它几种元素含量变化不太规律。可以看出,元素的初始含量对其释放速率有很大影响,当微生物固持作用使C与其它元素比升高到某一阈值时,元素开始释放;初始含量较高的元素则从最初开始释放。高含量的木质素对元素的净释放有一定抑制作用,而在凋落物分解初期影响不大。     

辽东栎叶片凋落物在不同气候带下的分解及其主要元素释放的比较

应用分解网袋法对辽东栎（Quercus liaotungensis Koize)叶片凋落物分别在暖温带的东灵山,亚热带的神农架,热带的西双版纳为期1-2年的分解和K,Ca,Mg,Fe,P,Cu,Mn等营养元素释放动态进行比较研究。三个气候带下辽东栎叶片凋落物质量损失基本符合Olson的指数模型。但降解速率有很大的差别。气候条件对凋落物的分解和营养元素的释放影响很大,降水量增多,年均温增高,凋落物分解速率相应加快,研究还发现影响营养元素释放的因素除公认的土壤生物（土壤动物和土壤微生物）作用外。对于Fe,Mn等元素遵循的是“化学因素主导”模式。特征在于由于化学螯合作用。其释放过程和凋落物本身失重呈显著负相关。另外,对不同因素占主导的各种分解模式进行了归纳总结。     

不同培养基对杜氏藻（DunaliellaSalina）生长和无机离子含量的影响

培养在Ｊｏｈｎｓｏｎ培养液、Ｊｏｈｎｓｏｎ＋０．３％ＮａＣｌ培养液、海水和卤水中的杜氏藻,其生长速度有区别,在Ｊｏｈｎｓｏｎ＋０．３％ＮａＣｌ培养液中生长较好,Ｊｏｈｎｓｏｎ培养液和卤水次之,海水中生长较差。杜氏藻生沃的盐度范围为０～１２％,当培养基中ＮａＣｌ浓度超过１２％时,细胞数几乎不增加,甚至略有降低。在不同培养基中藻细胞Ｈ￣＋含量较稳定,而积累ｃａ￣（２＋）,在Ｊｏｈｎｓｏｎ＋０．３％ＮａＣｌ培养液中,杜氏藻细胞Ｎａ￣＋含量增加;而在含高浓度Ｎａ￣＋的海水和卤水中杜氏藻细胞中Ｎａ￣＋的含量低于培养液。     

几种常微量元素在辽东栎枝条分解过程中的变化特征

应用分解网袋法 ,对暖温带落叶阔叶林主要优势树种辽东栎小枝进行连续 5a的分解研究 ,测定了 Ca、Mg、Cu、Zn和 Mn5种元素在凋落物分解过程中的含量和剩余百分率的变化 ,发现这两个指标在这几种元素之间既有一定的相似性 ,又有一定的差异。相似性表现在这几种元素在分解开始时 ,其含量都有一个不断上升的过程。但有的表现为不断上升( Ca和 Zn) ,而有的则在分解阶段的中期 ,已开始明显下降 ( Mg,Cu和 Mn)。从丢失速率常数上看 (根据 Olson的失重率常数 k) ,由于 Ca和 Cu在分解过程中的大量增加 ,因而用 Olson指数方程的拟合效果较差 ,而其它 3种元素用 Olson指数方程拟合结果相比较 ,发现 Mn的失重率略高于 Mg,而超过 Zn的 2倍。但这些元素的失重率都明显低于一些大量营养元素如 N、P、K的失重率     

北京山区辽东栎林土壤释放CO_2的模拟实验研究

模拟北京山区辽东栎林群落,对该类型土壤释放ＣＯ２过程进行了连续３ａ的实验研究,结果表明：辽东栎林土壤呼吸强度平均为５．９２±１．３２μｍｏｌＣＯ２ｍ－２ｓ－１,在不同月份中,以８月份最高,１０月最低,依次为８月＞７月＞６月＞９月＞１０月（Ｐ＜０．０５）;１３：００为土壤日呼吸的最高峰。温度为影响土壤呼吸的主要因子,二者存在极显著相关关系（ｒ＝０．５６６８,ｐ＜０．００１,ｎ＝９４）。据３ａ观测的土壤呼吸日平均值计算得出,模拟辽东栎林土壤释放ＣＯ２的通量估计范围为１７１．５～２７５．１ｋｇＣＯ２ｈｍ－２ｄ－１,平均为２２３．３ｋｇＣＯ２ｈｍ－２ｄ－１。     

蚯蚓体内一种纤溶酶原激活剂(e-PA)对ATEE的降解

赤子爱胜蚓（Ｅｉｓｅｎｉａｆｅｔｉｄａ）体内的一种纤溶酶原激活剂（ｅ－ＰＡ）能够降解人工合成底物Ｎ－乙酰－Ｌ－酪氨酸乙酯（ＡＴＥＥ）,该降解反应的最适ｐＨ为８．５,而且在０．２ｍｏｌ／ＬＮａ２ＨＰＯ４中的活性要强于在０．０５ｍｏｌ／ＬＴｒｉｓ－ＨＣｌ（ｐＨ８．５）中．分别测定了ｅ－ＰＡ的大小亚基及全酶在０．２ｍｏｌ／ＬＮａ２ＨＰＯ４与０．０５ｍｏｌ／ＬＴｒｉｓ－ＨＣｌ（ｐＨ８．５）两种体系中的Ｋｍ和Ｋｃａｔ．结果表明,在０．２ｍｏｌ／ＬＮａ２ＨＰＯ４中,全酶的ＡＴＥＥ活性远远高于大小亚基单独的ＡＴＥＥ活性,而在０．０５ｍｏｌ／ＬＴｒｉｓ－ＨＣｌ（ｐＨ８．５）中则没有这种现象．从蛋白质结构的角度对这一结果作了解释．用不同抑制剂和ｅ－ＰＡ作用,结果表明,ｐｅｐｓｔａｔｉｎ,Ｅ－６４和ＥＤＴＡ对ｅ－ＰＡ的ＡＴＥＥ活性都有不同程度的抑制,这一点与ｅ－ＰＡ的ＢＡＥＥ活性不同．     

几种常微量元素的辽东栎枝条分解过程中的变化特征

应用分解网袋法,对暖温带落叶阔叶林主要优势树种辽东栎小枝进行连续５ａ的分解研究,测定了Ｃａ、Ｍｇ、Ｃｕ、Ｚｎ和Ｍｎ５种元素的凋落物分解过程中的含量和剩余百分率的变化,发现这两个指标在这几种元素之间既有一定的相似性,又有一定的差异。相似性表现在这几种元素在分解开始蝗,其含量都有一个不断上升的过程。但有的表现为不断上升（Ｃａ和Ｚｎ）,而有的则在分解阶段的中期,已开始明显下降（Ｍｇ、Ｃｕ和Ｍｎ）。从丢失     

北京东灵山辽东栎种群DNA多样性的研究

在同工酶研究基础上,利用随机扩增多态性ＤＮＡ（ＲＡＰＤ）及ＤＮＡ扩增指纹（ＤＡＦ）方法,从生态学观点分析了北京东灵山区辽东栎（ＱｕｅｒｃｕｓｌｉａｏｔｕｎｇｅｎｓｉｓＫｏｉｄｚ．）种群的遗传结构和多样性。对１２个引物扩增产生的２０５个产物（部分）,经Ｓｈａｎｎｏｎ信息指数分析,结果表明：辽东栎种群内部存在丰富的遗传变异,中央种群的遗传多样性高于边缘种群的遗传多样性。总遗传多样性的９５％发生在种群内,只有５％发生在种群间。两种群在个别位点上存在差异。不同年龄组辽东栎的分析结果表明：人为干扰对辽东栎的遗传结构有一定影响。     

白腐菌产锰过氧化物酶条件的研究

白腐菌ＰｈａｎｅｒｏｃｈａｅｔｅｃｈｒｙｓｏｓｐｏｒｉｕｍＭＩＧ．３８３降解桉木时具有显著的选择性,３０天内降解３７．２３％Ｋｌａｓｏｎ木素,７．２９％综纤维素。该菌株产胞外锰过氧化物酶,并在高碳低氧培养基中显示较高酶活,静置液体培养的优化培养条件是（Ｌ＾－１）：１０ｇ葡萄糖,２ｍｍｏｌ酒石酸铵,１０ｍｍｏｌｐＨ４．５醋酸钠缓冲液;１ｇ吐温８０,２ｇＫＨ２ＰＯ４,０．５ｇＭｇＳＯ４．７Ｈ２Ｏ,０．     

羊草草原分解者亚系统的特性及作用

在内蒙古羊草（Ｌｅｙｍｕｓｃｈｉｎｅｎｓｉｓ）草原,对其分解者亚系统的特性及作用开展研究,采用网袋法对不同物候期羊草植株和凋落物的分解作用进行了测定。结果如下：１．植株分解的最初２－３ａ中,其残体表面的微生物生物量及转化酶、蛋白酶的活性均呈现返青期植株＞结实期植株＞果后营养期植株＞凋落物。植株分解的速度亦为上述规律。２．羊草植株被分解后,可提高临近土壤的微生物活性。各植株分解均引起土壤的Ｃ／Ｎ值下降,老熟植株分解使土壤的ＨＡ／ＦＡ值升高。３．幼嫩植株分解时,其体内营养元素会较快释放;凋落物分解则导致氮和磷元素的积累,但钾不会。４．通过指数衰减模型估算,羊草凋落物的分解常数为０．１５３ｇ／ｇ·ａ,９５％被分解掉约需１９ａ时间。５．羊草草原凋落物的最大积累量为年输入量的６．５４倍,即１１７５．６ｇ／ｍ￣２。６．分用凋落物的微生物其生物量平均为４．４×１０￣（－３）ｇ／ｇ·ＤＷ,微生物所含能量仅占凋落物贮存能量的０．５％左右。     

Change of Organic Matter in the Decomposing Oak Twigs in the Temperate Forest Ecosystems

Litter bag method was used in this study on the twig decomposition of an oak ( Quercus liaotungensis Koidz. ) which is dominant in the warm temperate deciduous forests. A consecutive five-year investigation was carded out to measure the changes of organic components in the twig litter. The decomposition of oak twigs based on rates of the mass loss during the first five years was simulated using the Olson exponential equation. The simulated data fit well with the observed values. Oak twigs were predicted to reach 95% decomposition within 21 years. During the first five years, the concentration of protein in the remaining litter increased from 3.5 % to 5.5 %, while the concentration of semicellulose decreased from 16.0% to 8.0%. However, there was no obvious change in the concentrations of lignin and cellulose. The loss of lignin, crude-cellulose, cellulose and semicellulose could be well simulated using the Olson exponential equation. However, this was not so effective for protein.     

Studies on litter decomposition processes in a temperate forest ecosystem. I. Change of organic matter in oak (Quercus liaotungensis Koidz.) twigs

The litter bag method was used in this study on the decomposition of twigs of an oak (Quercus liaotungensis Koidz.) which is dominant in the warm temperate deciduous forests. This continual 5-year investigation was to measure the changes of organic compounds in twig litter. The decomposition of oak twigs based on rates of the mass loss during the first 5 years was simulated using the Olson exponential equation. The simulated data fitted well with the observed values. Oak twigs were predicted to reach 95% mass loss within 21 years. During the first 5 years, the concentration of protein in the remaining litter increased from 3.5% to 5.5%, while the concentration of hemicellulose decreased from 16.0% to 8.0%. However, there was no obvious change in the concentrations of lignin and cellulose. The losses of lignin, crude-cellulose and hemicellulose could be well simulated using the Olson exponential equation. However, this was not true for cellulose and protein.     

滇中亚高山人工林凋落物分解对模拟氮沉降的响应

2018年2月至2019年1月,利用尼龙网袋法对滇中亚高山华山松和云南松两种人工林开展模拟氮(N)沉降下凋落叶和凋落枝原位分解试验,N沉降水平分别为对照(CK, 0 g N·m^-2·a^-1)、低N(LN, 5 g N·m^-2·a^-1)、中N(MN, 15 g N·m^-2·a^-1)和高N(HN, 30 g N·m^-2·a^-1)。结果表明: 华山松凋落叶和凋落枝年分解率分别为34.8%和18.0%,分别高于云南松凋落叶的32.2%和凋落枝的16.1%。模拟N沉降下,LN处理使华山松凋落叶、枝分解95%所需时间较对照分别减少0.202和1.624年,MN处理分别减少0.045和1.437年,HN处理则分别增加0.840和2.112年;LN处理使云南松凋落叶、枝分解95%所需时间较对照分别减少0.766和4.053年,MN处理分别增加0.366和0.455年,HN处理分别增加0.826和0.906年。经过1年的分解,低N处理促进了华山松和云南松凋落物(叶、枝)的分解,而高N处理表现为抑制作用;N沉降对两种林型凋落物分解的影响与凋落物中纤维素和木质素含量密切相关。可见,凋落物基质质量在一定程度上决定了凋落物分解对N沉降的响应情况,尤其是纤维素和木质素含量。     

辽东栎枝条分解过程中几种主要营养元素的变化

 应用分解网袋法,对暖温带落叶阔叶林主要优势树种辽东栎小枝进行连续5年的分解研究,测定了C、N、K、P和Na5种元素在凋落物分解过程中的含量和剩余百分率的变化,发现这两个指标在这几种元素之间有很大的差异。从丢失速率上看(根据Olson的失重率常数k),K元素的丢失速率明显高于其它4种元素;而从这几种元素含量变化的格局上看,K的含量在整个5年的分解过程中是不断降低的,C也有这样的趋势,N的含量有不断上升的趋势,而P和Na则表现为先升高后降低的趋势。     

滇中亚高山地带性植被凋落物分解对模拟氮沉降的响应

模拟氮(N)沉降对凋落物分解特征的影响对研究森林生态系统物质循环响应大气N沉降的内在机理和应对N沉降全球化具有重要意义。从2018年2月至2019年1月,对滇中亚高山常绿阔叶林(Evergreen broad-leaf forest)和高山栎林(Quercus semecarpifolia forest)两种地带性植被进行模拟N沉降试验,利用尼龙网袋法对两种林型凋落叶和凋落枝进行原位分解试验,N沉降处理水平分别为对照CK(Control check, 0 g N m^-2 a^-1)、低氮LN(Low nitrogen, 5 g N m^-2 a^-1)、中氮MN(Medium nitrogen, 15 g N m^-2 a^-1)和高氮HN(High nitrogen, 30 g N m^-2 a^-1)。结果表明:常绿阔叶林凋落叶和凋落枝分解率分别为44.84%和21.96%,均高于高山栎林的35.97%(凋落叶)和17.5...     

模拟氮沉降对华西雨屏区苦竹林凋落物基质质量的影响

凋凋落物基质质量是影响凋落物分解速率的决定性因子之一,本研究旨在探究模拟氮沉降对苦竹林凋落物基质质量的影响。2007年11月至2010年12月每月一次连续对华西雨屏区苦竹人工林进行了模拟氮沉降试验,施氮水平分别为：低氮（5 g N?m–2?a–1）,中氮（15 g N?m–2?a–1）和高氮（30 g N?m–2?a–1）。在施氮2 a后,于2010年1月开始收集各样方的凋落物样品,连续收集12个月,分析测定凋落物基质质量。结果表明：施氮显著增加了凋落叶中N、P元素含量,中氮处理显著增加了凋落枝中N元素含量,中氮和高氮处理均显著增加了凋落枝中P元素含量;施氮对凋落物中C元素含量影响很微弱,显著降低了凋落叶中的C/N,中氮处理显著降低了凋落枝中的C/N,对木质素和纤维素含量均未造成显著影响。由于模拟氮沉降增加了苦竹凋落物的N、P含量,降低了其C/N,因此氮沉降可能会促进苦竹凋落物的初期分解速率。     

Mass loss and nitrogen dynamics in decomposing acid forest litter in the Netherlands at increased nitrogen deposition

Litterbag experiments were carried out in five forest ecosystems in the Netherlands to study weight loss and nitrogen dynamics during the first two years of decomposition of leaf and needle litter. All forests were characterized by a relatively high atmospheric nitrogen input by throughfall, ranging from 22–55 kg N ha^–1 yr^–1.Correlation analysis of all seven leaf and needle litters revealed no significant relation between the measured litter quality indices (nitrogen and lignin concentration, lignin-to-nitrogen ratio) and the decomposition rate. A significant linear relation was found between initial lignin-to-nitrogen ratio and critical nitrogen concentration, suggesting an effect of litter quality on nitrogen dynamics.Comparison of the decomposition of oak leaves in a nitrogen-limited and a nitrogen-saturated forest suggested an increased nitrogen availability. The differences in capacities to retain atmospheric nitrogen inputs between these two sites could be explained by differences in net nitrogen immobilization in first year decomposing oak leaves: in the nitrogen-limited oak forest a major part (55%) of the nitrogen input by throughfall was immobilized in the first year oak leaf litter.The three coniferous forests consisted of two monocultures of Douglas fir and a mixed stand of Douglas fir and Scots pine. Despite comparable litter quality in the Douglas fir needles in all sites, completely different nitrogen dynamics were found.     

Decomposition of [C]Lignocelluloses of Spartina alterniflora and a Comparison with Field Experiments

Decomposition of lignocelluloses from Spartina alterniflora in salt-marsh sediments was measured by using C-labeled compounds. Rates of decomposition were fastest in the first 4 days of incubation and declined later. Lignins labeled in side chains were mineralized slightly faster than uniformly labeled lignins; 12% of the [side chain-C]lignin-labeled lignocellulose was mineralized after 816 h of incubation, whereas only 8% of the [U-C]lignin-labeled lignocelluloses were degraded during this period. The carbohydrate moiety within the lignocellulose complex was degraded about four times faster than the lignin moiety; after 816 h of incubation, 29 to 37% of the carbohydrate moiety had been mineralized. Changes in concentration of lignin and cellulose in litter of S. alterniflora were followed over 2 years of decay. Cellulose disappeared from litter more rapidly than lignin; 50% of the initial content of cellulose was lost after 130 days, whereas lignin required 330 to 380 days for 50% loss. The slow loss of lignin compared with other litter components resulted in a progressive enrichment of litter in lignin content. The rates of mineralization of [C]lignocelluloses in marsh sediments were similar to the rates of lignocellulose decomposition in litter on the marsh.     

降水量变化对蒙古栎落叶分解过程的间接影响

分析了在4种不同降水量条件下蒙古栎叶凋落物基质质量的变化,并应用分解袋法研究其凋落物在蒙古栎次生林内的分解过程.结果表明：与对照相比,降水量减少条件下,蒙古栎叶凋落物的初始N、P、K浓度显著升高,初始木质素浓度显著降低,凋落物分解速率大,N、P、K矿化率高,N和P固持时间缩短;降水量增加情况下,其凋落物初始N浓度显著降低、木质素浓度显著升高,N、P、K矿化率低,N和P固持时间延长.4种类型叶片凋落物的质量损失过程均符合指数降解模型,分解速率可以由凋落物木质素/N来预测.相关性分析显示,木质素浓度高、N浓度低的两种凋落物的分解速率与N浓度相关性最大;而木质素浓度低、N浓度高的两种凋落物的分解速率与木质素浓度相关性最大.说明降水量的变化显著地改变了蒙古栎叶凋落物的基质质量,进而间接地改变了凋落物的分解过程.