Biocycle of nitrogen in a Cyclobalanopsis glauca-dominated evergreen broad-leaved forest in East China

The nitrogen (N) cycling was elucidated in a 40-year-old subtropical evergreen broad-leaved forest dominated by Cyclobalanopsis glauca growing on red soil in Zhejiang Province, East China. The concentrations of N in the representative species ranged from 0.49% to 1.64%, the order of which in various layers was liana and herb layers > understory layer > tree and subtree layers; in various organs was leaf > branch > root > trunk; and aboveground parts > underground parts. The sequence of the concentrations of N in C. glauca was understory > tree > subtree layer; young and high-growing > old organs; reproductive > vegetative organs. Seasonal dynamics of the concentrations of N in C. glauca in the tree and subtree layers was comparatively stable. It was lower in autumn (October) in root, branch, and leaf in the tree layer, and low in January in the understory. There was no evident change in regularity of the concentrations of N in varying diameter classes. The concentrations of N in the litterfall, precipitation, throughfall, litter layer, and soil were 0.74%–2.30%, 0.000,038%, 0.000,09%, 1.94%, and 0.59%, respectively. The standing crop of N in the plant community was 1,025.28 kg/hm², accumulation in the litter layer was 224.88 kg/hm², and reserve in the soil was 55,151 kg/hm². Annual retention of N was 119.47 kg/hm², return was about 84.13 kg/hm², among which litterfall was 78.49 kg/hm² and throughfall, 5.64 kg/hm². Annual absorption of N was 203.60 kg/hm². Annual input of N through incident precipitation was 4.88 kg/hm². Compared with other forest types, cycling rate of N in the community was lower than in deciduous broad-leaved forests, rain forests, and mangroves, and was moderate in evergreen broad-leaved forests. N use efficiency of this forest was moderate among the forest types cited. According to the characteristics of the biocycle of phosphorous, it was concluded that N availability in the soil of this forest was not lower, and phosphorous not N was the limiting factor in the growth of plants in this community. __________ Translated from Acta Ecologica Sinica, 2005, 25(4): 740–748 [译自: 生态学报, 2005, 25(4): 740–748]     

Carbon and nitrogen dynamics under windrowed residues during the establishment phase of a second-rotation hoop pine plantation in subtropical Australia

The dynamics of carbon (C) and nitrogen (N), derived from the decomposition of windrowed harvest residues, was examined in the establishment phase of a second rotation (2R) hoop pine (Araucaria cunninghamii Aiton ex A. Cunn) plantation in subtropical Queensland, Australia. Following harvesting and site preparation, when residues were formed into windrows, in situ N mineralisation was measured in positions along the three tree-planting rows formed between the windrows. The position above the windrow had a higher nitrification rate than the other positions, averaging about 18 kg N ha⁻¹/month compared with 12 and 9 Kg N ha⁻¹ for the positions between and below the windrow positions, respectively. This position also had consistently greater soil moisture.

Macroplots were formed extending 5 m above and 10 m below a windrow. Windrowed residues within the macroplots were replaced by ¹⁵N-labelled material comprising hoop pine foliage, branch and stem. Hoop pine trees were planted within each macroplot with foliar samples taken at 12 and 24 months. Differences in foliar ¹⁵N enrichment between positions within macroplots were <1‰. Soil samples were taken from positions along the macroplots at 6-monthly intervals. Samples revealed an initial release of labile C and N but soil δ¹⁵N showed that residue-derived N was largely immobilised within the windrows for the 30-month sampling period. Whilst the use of windrows may act as a barrier to the down-slope movement of water, the residue N within the windrows may not be available to the trees of the following rotation for a considerable period following planting. Trees closest to the windrows may be able to introduce roots under the windrows thereby gaining access to the available N, but trees in the central tree planting row are unlikely to derive any significant benefit from the decomposition of windrowed residues.     

常绿和落叶阔叶树叶中N和P的变化及转移

从叶完全展开到生长季结束对常绿阔叶树种铁冬青、红楠和海桐及落叶阔叶树种日本朴、银杏和木叶的N和P浓度进行了定期测定。结果表明,常绿阔叶树种新叶的N和P浓度从5—7月急剧下降,然后小幅波动,而老叶的N和P浓度变化缓慢。落叶阔叶树种的N和P浓度随着季节的推移而明显下降。大多数树种的P转移率大于N转移率。常绿阔叶树种的N和P的转移率大于落叶阔叶树种。     

外生菌根真菌彩色豆马勃优良菌株营养源的研究*

通过Ｐ．ｔ．优良菌株９１０９在不同培养基上生长速度、培养特性及其生长规律的研究，筛选出生长最佳培养基作为基础培养基，进行Ｃ、Ｎ营养研究，试验结果表明：Ｐ．ｔ．９１０９不仅能利用单糖、低聚糖和无机Ｎ等速效Ｃ、Ｎ源，而且能利用多糖、多元醇和有机Ｎ等长效Ｃ、Ｎ源。其菌丝生长最适Ｃ源是玉米粉和甘露糖；最适Ｎ源是蛋白胨和氯化铵。在无机Ｎ利用中，对硝态Ｎ和铵态Ｎ的利用无显著差异。应用Ｌ１６（４５）正交设计确定了Ｐ．ｔ．９１０９菌丝生长的最佳营养配方，菌丝增殖高达８６０倍，不但提高菌丝生物产量，而且节省了原料，降低了成本，为改进Ｐ．ｔ．菌剂生产配方和研制新型菌剂提供了最佳营养条件。     

沼液施肥对杨树林地土壤微生物量碳氮的影响

沼液是沼气发酵过后的液体残留物,是一种优质的有机肥料。研究了不同沼液施肥对杨树林地土壤微生物量碳氮的影响。结果表明:施用沼液可以提高土壤微生物量碳、氮的含量,微生物量碳、氮含量增加范围分别为4.29%~61.62%和6.08%~76.10%,土壤微生物量碳氮含量随沼液施用量增加逐渐提高。土壤微生物量碳氮呈正相关。土壤微生物量碳氮比随沼液施用量增加逐渐下降,其变化范围为9.92~10.81,土壤微生物量碳氮比与微生物量碳、氮含量负相关。     

甲醛交联碱木质素-聚乙烯醇-尿素薄膜氮元素缓释性能研究

采用交联法制备了碱木质素-聚乙烯醇-尿素-甲醛(AL-PVA-U-F)交联薄膜,分析碱木质素(AL)和交联剂甲醛(F)的加入量对氮元素缓释的影响,研究薄膜对氮元素的缓释机理,并采用XRD和FT-IR-ATR方法分析薄膜的结晶度和化学结构,结果显示碱木质素的加入可降低薄膜中氮元素的缓释速率,使氮元素达到释放平衡的时间增大,碱木质素和聚乙烯醇质量比5∶5时复合薄膜192 h时达到释放平衡,释放平衡时间最长,氮元素累积释放率最大为77.73%。加入适量的甲醛交联剂使碱木质素、聚乙烯醇、尿素、甲醛之间发生化学反应,线性和网状结构交互从而使薄膜中氮元素缓释减慢。与共混薄膜(ALPVA-U)相比,甲醛的交联作用使薄膜的结晶度降低。薄膜的氮元素累积释放率曲线呈"S"型趋势,Ritger-Peppas模型和2次多项式模型拟合较好,相关系数(R2)分别为0.976 3和0.950 9,Ritger-Peppas模型中n为0.816 7,说明氮元素释放规律是扩散和溶蚀综合作用的结果。     

低蛋白质氨基酸平衡饲粮对生长猪生长性能和氮素减排的影响研究

试验旨在研究饲喂低蛋白质氨基酸平衡饲粮对生长猪生长性能和氮排泄量的影响,采用单因子完全随机设计,将144头平均体重30 kg左右的杜长大三元杂种生长母猪分成3组,每组设6个重复,每个重复8头猪,对照组饲喂实测粗蛋白质含量为18.10%的普通饲粮,试验1组、试验2组分别饲喂实测粗蛋白质含量为16.08%和14.12%的氨基酸平衡饲粮。试验期37 d,前7 d为预试期,正试期30 d。结果显示,3组日采食量、日增重、料重比指标均没有显著差异(P0.05),而日氮素总排泄量试验1组、试验2组分别比对照组减少18.69%、38.68%,3组之间差异均显著(P0.05),且试验1组、试验2组猪每增重1 kg所需要的饲料成本分别较对照组节省0.11和0.23元。综合考虑,生长猪饲喂低蛋白质氨基酸平衡饲粮,可以作为实现养殖效益与环保双赢的主要技术措施予以推广。     

豆秸、花生秧和青贮玉米秸间的组合效应研究

本试验旨在研究豆秸、花生秧和青贮玉米秸间的组合效应。试验将豆秸、花生秧和青贮玉米秸分别以0∶100、20∶80、40∶60、60∶40、80∶20、100∶0比例进行两两组合,利用体外瘤胃发酵技术,分析不同组合对产气量及产气参数、pH、氨态氮、菌体蛋白的影响,计算各组合的单项组合效应值和综合组合效应值,进而筛选各饲料组合的适宜比例。结果表明：豆秸-花生秧、豆秸-青贮玉米秸、花生秧-青贮玉米秸组合在产气参数上差异显著(P<0.05),豆秸-花生秧和豆秸-青贮玉米秸均以20∶80时各产气参数最优,花生秧-青贮玉米秸以60∶40时各产气参数为最优;各组合对体外瘤胃液pH影响差异不显著(P>0.05);不同组合的氨态氮浓度差异显著(P<0.05),在39~64 mg/dL变化;豆秸-花生秧和花生秧-青贮玉米秸的菌体蛋白浓度随花生秧比例增多而增多,豆秸-青贮玉米秸的菌体蛋白浓度在两者比例为20∶80时最高。以多项组合效应评定指数评定各组合效应,豆秸与花生秧、青贮玉米秸均以20∶80的比例较为适宜,花生秧与青贮玉米秸比例以60∶40时较为适宜,综合组合效应指数均达到最大。     

绿洲灌溉区与旱作区多龄苜蓿地土壤有机碳、氮及物理特性分析

以甘肃灌区和旱作区苜蓿(Medicago sativa)地土壤为研究对象,对不同地域的苜蓿地土壤全氮(TSN)、有机碳(SOC)、容重、含水量进行测定,结果表明:灌区SOC含量均高于旱作区,在90~100cm土层其含量与旱作区差值最大,达3.41g/kg。在0~100cm灌区SOC含量为6.81~12.49g/kg,均值为9.25g/kg,比旱作区高22%。旱作区TSN含量随土壤深度的增加而减小,含量在(1.03±0.01)~(0.44±0.04)g/kg。在0~30cm灌区TSN含量相对较稳定,差异不显著(P0.05),在30~60cm剖面全氮含量急剧下降,70~100cm含量变化较为稳定,TSN含量维持在(0.66±0.01)g/kg。旱作苜蓿地土壤含水量在0~60cm变化不显著(P0.05),0~100cm土壤含水量均值为(14.437±1.124)%,灌区苜蓿地土壤含水量均值为(16.025±2.029)%。随着土壤深度的增加,旱作区和灌区苜蓿地土壤容重均呈现依次增大的分布规律,旱作区最大值为(1.421±0.034)g/cm,比最小值高出17.5%,灌区最大值(1.332±0.017)g/cm,比最小值高出11.3%.     

外源氮素形态及水平对紫花苜蓿幼苗各部位氮含量的影响

在完全营养液条件下,采用砂培法,研究了2种氮素形态(NO-3-N,NH+4-N)和5个氮素水平(0、105、210、315、420mg/L)对紫花苜蓿品种"甘农3号"和"陇东苜蓿"幼苗各部位氮含量的影响。结果表明:施氮处理下各部位NO-3-N含量、NH+4-N含量和全氮含量均显著高于CK(P0.05)。"甘农3号"和"陇东苜蓿"2个品种的各部位氮含量变化一致,均随施氮水平的升高呈先增加后降低的趋势,但峰值表现不一。同一氮素形态及水平下,不同部位NO-3-N、NH+4-N及全氮含量表现为:叶根茎。"甘农3号"在NO-3-210处理下叶、茎、根中NO-3-N含量最优,分别为490,385和463μg/g;"陇东苜蓿"分别为473,355和447μg/g。"甘农3号"在NH+4-210处理下叶、茎、根中NH+4-N含量最优,分别为212,182和194μg/g;"陇东苜蓿"茎和根中含量分别为177μg/g、178μg/g,叶却在NH+4-315处理最大,为189μg/g。"甘农3号"在NH+4-315处理下叶、茎、根中全氮含量最优,分别为4.25%,1.7%和3.47%;"陇东苜蓿"叶和根中含量分别为4.01%、3.08%,茎却在NH+4-210处理最大,为2.33%。对于同一部位除"陇东苜蓿"茎全氮含量高于"甘农3号"外,其他部位的NO-3-N、NH+4-N和全氮含量均表现为"甘农3号"优于"陇东苜蓿"。