农业生态系统养分循环再利用作物产量增益的地理分异

通过４个地点中长期田间试验联网比较获得以下结果,农业生态系统养分循环再利用的作物产量增益受气候的热量因素、化肥施用和养分循环再利用持续时间的长短等因素影响．在不施化肥情况下,保持０．８循环率养分循环再利用的平均粮食增产量自北向南分别是：温带黑龙江海伦２５３ｋｇ·ｈｍ－２（１０年平均）、暖温带辽宁沈阳１１２２ｋｇ·ｈｍ－２（６年）和喀左１３３２ｋｇ·ｈｍ－２（８年）、亚热带湖南桃源２８８４ｋｇ·ｈｍ－２（７年）;在施用ＮＰ化肥基础上保持养分循环再利用则分别为海伦２２５、沈阳６９４、喀左７８６、桃源１３２１ｋｇ·ｈｍ－２．循环回田的农家肥养分对作物增产有着明显的残效叠加作用,在施用ＮＰＫ化肥基础上保持养分循环再利用的作物增产率在试验期间的前３年平均为５％,后３年平均可上升至１４％．     

稻鱼鸭复合生态经济效益的初步研究

试验表明．稻鱼鸭种养共生,水稻增产 １０％以上,同时增收鲜鱼 １０３６．５ ｋｇ· ｈｍ－２,成鸭２３８．９～４８９．３ ｋｇ·ｈｍ－２;水稻土壤全Ｎ、Ｐ、Ｋ和有机质含量分别增加２７．９、 ４４． ３、６． ５和 ２８． ２％,提高了土壤肥力;水稻植株虫口量最少．稻鱼鸭共生大大提高了稻田 的产出和效益．属良性循环的高效复合生态农业．     

玉米植株对大田温室气体N2O排放的影响

利用封闭式箱法对玉米田Ｎ２Ｏ排放通量的观测表明,大田种植玉米后,对Ｎ２Ｏ排放产生了很大影响,玉米土壤系统的Ｎ２Ｏ排放通量大于不种玉米的土壤．此外,植物根系能明显促进土壤中Ｎ２Ｏ的排放,特别是在玉米生长后期尤为明显．从播种开始到年底,施尿素导致Ｎ２Ｏ排放为３．３ｋｇ·ｈｍ－２,玉米植株为０．６９ｋｇ·ｈｍ－２,占总排放量的１７．３％．     

长喙田菁-Azorhizobium caulinodans共生固氮体系在华南地区的生长、结瘤、固氮和种子生产

研究了长喙田菁－Ａｚｏｒｈｉｚｏｂｉｕｍｃａｕｌｉｎｏｄａｎｓ共生固氮体系在华南地区的生长、结瘤、固氮和种子生产．结果表明,长喙田菁－Ａ．ｃａｕｌｉｎｏｄａｎｓ共生固氮体系在华南地区生长正常,并具旺盛的茎根瘤结瘤作用．经６５天的生长,其在湛江地区的单位面积生物量（干物质）和单位面积Ｎ产量分别为２８７５２和６８１ｋｇ·ｈｍ－２,远优于普通田菁的１６５２０和３５２ｋｇ·ｈｍ－２;茎瘤菌Ａ．ｃａｕｌｉｎｏｄａｎｓ品系ＡＲ１１１和ＡＲ５６在华南地区混合接种效果良好,植株茎瘤结瘤率达到１００％,平均单株茎瘤个数为１８２个,单株茎瘤鲜重约为１．２ｇ,茎瘤生物量在茎根瘤总生物量中所占比重为７０％,而其根瘤生物量略高于普通田菁;长喙田菁在华南地区能够正常开花结实,在栽植密度为４×１０４株·ｈｍ－２的条件下,其种子产量达３２００ｋｇ·ｈｍ－２．     

高寒草甸生态系统氮素循环

应用分室模型,研究了高寒草甸（矮嵩草草甸）生态系统中氮素的分布与循环。结果表明：系统中,土壤库氮素总储量为 １０６３ｔ／ｈｍ ２,主要以有机态存在,土壤氮素全量养分丰富,而有效养分贫乏,仅能满足较低水平生产的供求关系;植物氮素主要储存于植物活根中,根系氮素储量为 １９０１１±４９６２ｋｇ／ｈｍ ２·ａ,活根内氮素占 ７９２６％ 。通过对该系统氮素收支平衡计算结果表明,氮素输出为 １５９３５ｋｇ／ｈｍ ２·ａ,大于系统的输入 ８４７３ｋｇ／ｈｍ ２·ａ,系统中氮素亏缺,成为限制草场生产力提高的限制因子。     

不同质地土壤的水热状况及其对冬小麦产量形成的影响

对豫东平原３种质地土壤的水热状况和冬小麦籽粒生长特征进行了研究．结果表明,冬小麦籽粒生长阶段,粘壤土５ｃｍ处的日平均温度最低,为１８．３℃,砂壤土最高,为１９．５℃,中壤居中,为１９．１℃．３种土壤的含水量大小顺序为粘壤＞中壤＞砂壤,粘壤土上小麦籽粒灌浆时间最长,千粒重最高,分别为３８ｄ和４５．５ｇ,砂壤土小麦籽粒灌浆时间最短,千粒重最低,分别为３３ｄ和４２．４ｇ,中壤土小麦２项指标居中,分别为３６ｄ和４３．１ｇ．高产栽培条件下,粘壤土冬小麦产量最高,为８２５３ｋｇ·ｈｍ－２,中壤次之,为７９８０ｋｇ·ｈｍ－２,砂壤最低,为７６１７ｋｇ·ｈｍ－２     

麦-稻两熟集约生产土壤养分平衡与调控研究

以兴化市钓鱼乡为例,研究了麦－稻两熟集约生产的土壤有机质、养分的动态平衡以及调控途径。结果表明,在不同的管理模式下,高产农田有机物归还量比一般产量条件下高１４．２２％￣１８．６９％,氮、磷盈余量、钾亏缺量分别为３８０．０￣４３２ｋｇ／ｈｍ＾２、１９．１５￣３２．７８ｋｇ／ｈｍ＾２、９９．１￣１７４．０ｋｇ／ｈｍ＾２,与一般产量条件下比较,氮、磷盈余量提高,而钾的亏缺量相近,提出了改善高产农田土壤肥     

北方稻田生态系统研究Ⅱ．稻萍结合系统细绿萍共生固N量研究

对稻萍结合系统细绿萍共生固Ｎ量研究表明,萍的固Ｎ力在整个生长季不同时期有所变化．最高固Ｎ率出现在６月初,萍固Ｎ量随其接种量和水稻行距增加而增加．５０～１０ｃｍ宽窄行交替的水稻行距和１５００ｋｇ·ｈｍ－２的萍接种量的稻萍结合系统的总固Ｎ量为１０７．１ｋｇ·ｈｍ－２,而３０ｃｍ等行距的３２５ｋｇ·ｈｍ－２的萍接种量的稻－萍结合系统的总固Ｎ量仅为３６．０ｋｇ·ｈｍ－２     

草原土壤N2O释放及全球变暖影响下土壤养分变化的反馈效应

对草原土壤Ｎ２Ｏ释放及其受全球变暖土壤养分变化的影响研究表明,以沼泽泥炭土Ｎ２Ｏ释放量最大,生长季节为１３～１２．２ｋｇＮ·ｈｍ－２·ａ－１,其次灰壤土,为１．５～２．４ｋｇＮ·ｈｍ－２·ａ－１,酸性棕壤最小,为０～３．２ｋｇＮ·ｈｍ－２·ａ－１;Ｎ２Ｏ的释放层灰壤土在０～５ｃｍ,其它２种土壤为０～１０ｃｍ;施肥试验表明,Ｎ、Ｐ肥在生长季节对土壤Ｎ２Ｏ释放量影响不显著,但在生长季末期,Ｎ肥对酸性棕壤及灰壤土Ｎ２Ｏ影响显著,施肥后第３天酸性棕壤由对照的１．３提高到４４．２ｋｇＮ·ｈｍ－２·ａ－１,灰壤土则由对照的１．９提高到３１．１ｋｇＮ·ｈｍ－２·ａ－１,说明全球变暖对土壤有机质分解的影响不会诱发Ｎ２Ｏ释放量的大幅度增加．     

武夷山甜槠群落钙,镁的累积和循环

对５１年生甜槠群落Ｃａ、Ｍｇ含量及其生物循环研究表明,甜槠群落现存量中,Ｃａ、Ｍｇ总量分别为１０２９．９６和２３１．３４ｋｇ·ｈｍ－２;其中地上部分分别为８０１．４０和１５９．６８ｋｇ·ｈｍ－２,地下部分分别为２２８．５６和７１．６６ｋｇ·ｈｍ－２．该群落Ｃａ、Ｍｇ生物循环中,年吸收量分别为６３．１７和１８．６８ｋｇ·ｈｍ－２,年存留量分别为３１．７７和１１．４１ｋｇ·ｈｍ－２,年归还量分别为３１．４０和７．２７ｋｇ·ｈｍ－２;Ｃａ、Ｍｇ的富集率分别为１．６６和２．１４．     

植物、土壤及土壤管理对土壤微生物群落结构的影响

土壤微生物是土壤生态系统的重要组成部分,对土壤微生物群落结构多样性的研究是近年来土壤生态学研究的热点。本文综述了有关植物、土壤类型以及土壤管理措施对土壤微生物群落结构影响的最新研究结果,指出植物的作用因植物群落结构多样性、植物种类、同种植物不同的基因型,甚至同一植物不同根的区域而异;而土壤的作用与土壤质地和有机质含量等因素有关;植物和土壤类型在对土壤微生物群落结构影响上的作用存在互作关系。不同的土壤管理措施对土壤微生物群落结构影响较大,长期连作、大量的外援化学物质的应用降低了土壤微生物的多样性;而施用有机肥、免耕可以增加土壤微生物群落结构多样性,有利于维持土壤生态系统的功能。     

Estimating respiration of roots in soil: Interactions with soil CO2, soil temperature and soil water content

Little information is available on the variability of the dynamics of the actual and observed root respiration rate in relation to abiotic factors. In this study, we describe I) interactions between soil CO₂ concentration, temperature, soil water content and root respiration, and II) the effect of short-term fluctuations of these three environmental factors on the relation between actual and observed root respiration rates. We designed an automated, open, gas-exchange system that allows continuous measurements on 12 chambers with intact roots in soil. By using three distinct chamber designs with each a different path for the air flow, we were able to measure root respiration over a 50-fold range of soil CO₂ concentrations (400 to 25000 ppm) and to separate the effect of irrigation on observed vs. actual root respiration rate. All respiration measurements were made on one-year-old citrus seedlings in sterilized sandy soil with minimal organic material.Root respiration was strongly affected by diurnal fluctuations in temperature (Q₁₀ = 2), which agrees well with the literature. In contrast to earlier findings for Douglas-fir (Qi et al., 1994), root respiration rates of citrus were not affected by soil CO₂ concentrations (400 to 25000 ppm CO₂; pH around 6). Soil CO₂ was strongly affected by soil water content but not by respiration measurements, unless the air flow for root respiration measurements was directed through the soil. The latter method of measuring root respiration reduced soil CO₂ concentration to that of incoming air. Irrigation caused a temporary reduction in CO₂ diffusion, decreasing the observed respiration rates obtained by techniques that depended on diffusion. This apparent drop in respiration rate did not occur if the air flow was directed through the soil. Our dynamic data are used to indicate the optimal method of measuring root respiration in soil, in relation to the objectives and limitations of the experimental conditions.     

Available soil nitrogen in relation to fractions of soil nitrogen and other soil properties

The available N of 27 soils from England and Wales was assessed from the amounts of N taken up over a 6-month period by perennial ryegrass grown in pots under uniform environmental conditions. Relationships between availability and the distribution of soil N amongst various fractions were then examined using multiple regression. The relationship: available soil N (mg kg^–1 dry soil)=(N_min×0.672)+(N_inc×0.840)+(N_mom×0.227)–5.12 was found to account for 91% of the variance in available soil N, where N_min=mineral N, N_inc=N mineralized on incubation and N_mom=N in macro-organic matter. The N mineralized on incubation appeared to be derived largely from sources other than the macro-organic matter because these two fractions were poorly correlated. When availability was expressed in terms of available organic N as % of soil organic N (N_ao) the closest relationship with other soil characteristics was: N_ao=[N_inc×(1.395–0.0347×CN_mom]+[N_mom×0.1416], where CN_mom=CN ratio of the macro-organic matter. This relationship accounted for 81% of the variance in the availability of the soil organic N.The conclusion that the macro-organic matter may contribute substantially to the available N was confirmed by a subsidiary experiment in which the macro-organic fraction was separated from about 20 kg of a grassland soil. The uptake of N by ryegrass was then assessed on two subsamples of this soil, one without the macro-organic matter and the other with this fraction returned: uptake was appreciably increased by the macro-organic matter.     

Effect of soil moisture on bioremediation of chlorophenol-contaminated soil

A chlorophenol-contaminated soil was tested for the biodegradability in a semi-pilot scale microcosm using indigenous microorganisms. More than 90% of 4-chlorophenol and 2,4,6-trichlorophenol, initially at 30 mg kg^–1, were removed within 60 days and 30 mg pentachlorophenol kg^–1 was completely degraded within 140 days. The chlorophenols were degraded more effectively under aerobic condition than under anaerobic condition. Soil moisture had a significant effect with the slowest degradation rate of chlorophenols at 25% in the range of 10–40% moisture content. At 25–40%, the rate of chlorophenol degradation was directly related to the soil moisture content, whereas at 10–25%, it was inversely related. Limited oxygen availability through soil agglomeration at 25% moisture content might decrease the degradation rate of chlorophenols.     

耕作方式对潮土土壤团聚体微生物群落结构的影响

为探究不同耕作方式对潮土土壤团聚体微生物群落结构和多样性的影响,采用磷脂脂肪酸(PLFA)法测定了土壤团聚体中微生物群落。试验设置4个耕作处理,分别为旋耕+秸秆还田(RT)、深耕+秸秆还田(DP)、深松+秸秆还田(SS)和免耕+秸秆还田(NT)。结果表明:与RT相比,DP处理显著提高了原状土壤和>5 mm粒级土壤团聚体中真菌PLFAs量和真菌/细菌,为真菌的繁殖提供了有利条件,有助于土壤有机质的贮存,提高了土壤生态系统的缓冲能力;提高了5～2 mm粒级土壤团聚体中细菌PLFAs量,降低了土壤革兰氏阳性菌/革兰氏阴性菌,改善了土壤营养状况;提高了<0.25 mm粒级土壤团聚体中微生物丰富度指数。总的来说,深耕+秸秆还田(DP)对土壤团聚体细菌和真菌生物量有一定的提高作用,并且在一定程度上改善了土壤团聚体微生物群落结构,有利于增加土壤固碳能力和保持土壤微生物多样性。冗余分析结果表明,土壤团聚体总PLFAs量、细菌、革兰氏阴性菌和放线菌PLFAs量与土壤有机碳相关性较强,革兰氏阳性菌PLFAs量与总氮相关性较强。各处理较大粒级土壤团聚体微生物群落主要受碳氮比、含水量、pH值和团聚体质量分数的影响,较小粒级土壤团聚体微生物群落则主要受土壤有机碳和总氮的影响。     

The porosity of soil aggregates from bulk soil and from soil adhering to roots

Summary Total porosity and pore-size distribution (p.s.d.) were determined in soil aggregates taken in plots planted with maize and treated with farmyard manure and three rates of compost. Soil aggregates were collected from the soil adherent to the maize roots (root soil aggregates) and from bulk soil (bulk soil aggregates). Mercury intrusion porosimetry was used to evaluate the total porosity and the p.s.d. Treatments did not affect the total porosity of the bulk soil aggregates. The same was observed for the root soil aggregates. However the total porosity of the root soil aggregates was always lower than that of the bulk soil aggregates. The loss of total porosity was found to be due to a decrease in the percentage of larger pores with respect to the total.     

生物质炭对水稻土团聚体微生物多样性的影响

生物质炭施用对土壤微生物群落结构的影响已有报道,但土壤团聚体粒组中微生物群落对生物质炭施用的响应的研究还相对不足。以施用玉米秸秆生物质炭两年后的水稻土为对象,采用团聚体湿筛法,通过高通量测序对土壤团聚体的微生物群落结构与多样性进行分析,结果表明:(1)与对照相比,生物质炭施用显著促进了大团聚体(2000—250μm)的形成,并提高了团聚体的稳定性。(2)不同粒径团聚体间微生物相对丰度存在显著差异。在未施生物质炭的处理(C0)中,随着团聚体粒径增大,变形菌门、子囊菌门、β-变形杆菌目、格孢腔菌目的相对丰度逐渐降低,而酸杆菌门、担子菌门、粘球菌目、类球囊霉目的相对丰度逐渐升高。(3)生物质炭施用显著改变了团聚体间的微生物群落结构。与C0处理相比,生物质炭施用处理的大团聚体中变形菌门、鞭毛菌门和β-变形杆菌目的相对丰度分别显著提高了14.37%、33.28%和33.82%;微团聚体(250—53μm)中酸杆菌门、子囊菌门和粘球菌目的相对丰度分别显著降低了20.15%、19.93%和17.66%;粉、黏粒组分(53μm)中担子菌门的相对丰度升高90.25%,而子囊菌门和鞭毛菌门的相对丰度分别降低12.15%和12.58%。由此可见,生物质炭不仅改变土壤团聚体组成和分布,同时伴随着土壤微生物群落结构的改变。     

酸性硫酸盐土水改旱后土壤化学性状的变异初报

探讨了酸性硫酸盐水稻土改为旱作后土壤化学性状的变异以及比较不同利用方式之间的经济效益．结果表明,酸性硫酸盐水稻土改种甜玉米和蔬菜后,土壤化学性状发生显著变化．耕层土壤酸度、水溶性硫酸根含量、土壤活性铝和活性铁含量均显著降低．经济效益得到显著提高．建议对水改旱后的环境效应进行深入研究以及进行定位观测,以便合理利用这一特殊的土壤资源     

Bioremediation of pentachlorophenol-contaminated soil by bioaugmentation using activated soil

The use of an indigenous microbial consortium, pollutant-acclimated and attached to soil particles (activated soil), was studied as a bioaugmentation method for the aerobic biodegradation of pentachlorophenol (PCP) in a contaminated soil. A 125-l completely mixed soil slurry (10% soil) bioreactor was used to produce the activated soil biomass. Results showed that the bioreactor was very effective in producing a PCP-acclimated biomass. Within 30 days, PCP-degrading bacteria increased from 10⁵ cfu/g to 10⁸ cfu/g soil. Mineralization of the PCP added to the reactor was demonstrated by chloride accumulation in solution. The soil-attached consortium produced in the reactor was inhibited by PCP concentrations exceeding 250 mg/l. This high level of tolerance was attributed to the beneficial effect of the soil particles. Once produced, the activated soil biomass remained active for 5 weeks at 20 °C and for up to 3 months when kept at 4 °C. The activated attached soil biomass produced in the completely mixed soil slurry bioreactor, as well as a PCP-acclimated flocculent biomass obtained from an air-lift immobilized-soil bioreactor, were used to stimulate the bioremediation of a PCP-impacted sandy soil, which had no indigenous PCP-degrading microorganisms. Bioaugmentation of this soil by the acclimated biomass resulted in a 99% reduction (from 400 mg/kg to 5 mg/kg in 130 days) in PCP concentration. The PCP degradation rates obtained with the activated soil biomass, produced either as a biomass attached to soil particles or as a flocculent biomass, were similar. Received: 31 March 1997 / Received revision: 22 July 1997 / Accepted: 25 August 1997