不同腐解期玉米秸秆对Lou土胡敏酸基本性质及级分变异的影响

采用田间腐解试验,在研究不同腐解期玉米秸秆对土壤胡敏酸性质影响的基础上,利用分级沉淀法对土壤胡酶酸进行分级,研究了不同腐解期土壤胡敏酸级分组成及性质变化。结果表明：在整个腐解过程中土壤胡敏酸由A型转化为P型又转化为A型,呈现由复杂到简单又到复杂的变化趋势。不同腐解期土壤胡敏酸的级分组成不同。玉米秸秆更新土壤胡敏酸过程是一个双向过程,一方面使胡敏酸中结构复杂成分（级分1、2、3）向简单化发展,另一方面一些小分子胡敏酸（级分6、7）随时间推移按Rp→P→A途径逐渐综合。     

不同肥力条件下黑土及其有机无机复合体的腐殖质组成

采用Kumada法研究了不同肥力黑土及其复合体的腐殖质组成.结果表明,黑土培肥后,粉粒和细砂复合体含量增多;土壤及各级复合体游离态和结合态腐殖质含量得到不同程度提高,但游离态腐殖质的腐殖化度降低.这种作用在粉粒和细砂复合体中表现得更为明显.随复合体粒径增大,复合体有机碳含量、腐殖质提取率、游离态腐殖质含量及游离态胡敏酸的腐殖化度等均有降低趋势.胡敏酸分类结果表明,高肥土壤游离态胡敏酸均为R_p型,低肥则为R_p型和B型.随复合体粒径增大,游离态胡敏酸类型变化序列主要为:A型(粘粒)→B型(粉粒)→R_p型(细砂);无论粒径大小,结合态胡敏酸大多为A型.土壤培肥后,可使全土及各级复合体的游离态腐殖质的腐殖化度降低,进而会发生型变.在黑土中,游离态胡敏酸的型变主要体现在粉粒复合体中,结合态胡敏酸的型变主要体现在细砂复合体中.     

不同促腐条件下秸秆还田对土壤微生物量碳氮磷动态变化的影响

通过2年田间定位试验,研究了冀东地区小麦 玉米轮作制度下,不同促腐条件下玉米秸秆配施化肥直接还田对土壤微生物量C、N、P动态变化的影响,并讨论了其与土壤养分和酶活性的关系.结果表明,秸秆配施化肥并调节其C/N条件下,施用促腐剂处理作物各生育期土壤微生物量C、N、P均表现出高于未施用处理的趋势,并使微生物量N、P达到高峰期的时间提前,对土壤养分调控效果较好.土壤微生物量C、N、P与土壤酶活性在作物各生育期均表现为显著和极显著正相关关系,但与土壤碱解氮、有效磷的相关性受到施肥制度和作物生长的强烈影响.     

Research and Analysis of Microorganisms in Returning the Corn Straw to Field

以玉米秸秆中木质纤维素的基本结构与组成和降解木质纤维素的微生物与酶类为依据,以解决秸秆还田过程定向快速腐熟关键技术为主,通过对微生物腐熟剂在秸秆腐解过程中定殖能力和腐解率的研究,确立了微生物腐熟剂在玉米秸秆还田中的作用,观察测试了人工加入的微生物菌群对土壤微生物种群数量及土壤酶活性的影响,对其研究测试结果进行了分析。     

施氮对关中还田玉米秸秆腐解和养分释放特征的影响

在陕西关中平原的冬小麦-夏玉米轮作区,采用尼龙网袋田间填埋与¹⁵N同位素标记玉米秸秆相结合的方法,设置不施氮和施氮200 kg·hm^-2两个处理,研究施氮对小麦生长期内还田玉米秸秆腐解的影响以及腐解过程中秸秆碳、氮、磷、钾的养分释放.结果表明: 从小麦播种到越冬期,施用氮肥对秸秆碳和干物质分解无显著影响,但可促进秸秆中磷的释放,抑制氮和钾的释放.灌浆到成熟期,氮肥对秸秆腐解及其N、P、K养分的释放无显著影响,但秸秆碳的释放显著增加.不同生育期,玉米秸秆碳的释放与干物质分解变化趋势一致,C/N逐渐下降.种植一季小麦后,秸秆干物质累计腐解率不足50%;秸秆碳释放率为47.9%～51.1%,不施氮和施氮处理的秸秆C/N分别由32.2降低到20.2和17.9.小麦收获时,秸秆氮、磷、钾均为净释放,氮释放量为7.2～9.4 kg·hm^-2,占秸秆氮的12.7%～16.6%;磷释放量为1.29～1.44 kg·hm^-2,占29.0%～32.4%;钾的释放量大、释放快,越冬前超过80%,成熟时释放量为51.8～52.5 kg·hm^-2,占90.5%～91.7%.在秸秆还田条件下,应考虑秸秆归还的钾,减少小麦钾肥用量,适量补充氮、磷.     

微生物在玉米秸秆还田中的作用研究与分析

以玉米秸秆中木质纤维素的基本结构与组成和降解木质纤维素的微生物与酶类为依据,以解决秸秆还田过程定向快速腐熟关键技术为主,通过对微生物腐熟剂在秸秆腐解过程中定殖能力和腐解率的研究,确立了微生物腐熟剂在玉米秸秆还田中的作用,观察测试了人工加入的微生物菌群对土壤微生物种群数量及土壤酶活性的影响,对其研究测试结果进行了分析。     

Bt玉米秸秆分解对土壤酶活性和土壤肥力的影响

通过室内实验,研究了Bt玉米34B24和同源常规品种34B23、Bt玉米农大61和常规品种农大3138秸秆分解对土壤酶活性和土壤肥力的影响.结果表明,与34B23处理相比,34B24处理的土壤蛋白酶和酸性磷酸酶活性在观测期没有显著差异;7d时土壤脱氢酶活性显著提高,1、4、60和7d土壤蔗糖酶活性显著提高;30d时土壤脲酶活性显著提高,4d和7d时则土壤脲酶活性显著降低.2个Bt玉米处理和2个常规玉米处理的土壤酶活性也在某些时间有显著差异.秸秆分解90d后,34B24处理比34B23处理.显著降低了土壤速效磷和速效钾含量.以上差异与不同秸秆的化学构成有关,Bt基因的转化过程可能会影响受体作物秸秆的化学成分.应建立不同土壤类型土壤酶活性的标准分级体系,以便科学评价Bt玉米秸秆分解对土壤质量的影响.     

低温复配菌系对玉米秸秆的降解特性及稳定性

针对我国北方地区冬季还田秸秆腐解慢导致的出苗率降低及病虫害加重等问题,探究外源促腐微生物在低温条件下对玉米秸秆的降解特性,为低温秸秆降解复配菌系的大田应用提供数据支持.本研究利用单菌株 Achromobacter deleyi(A3)、Pseudomonas plecoglossicida(A4)、Aspergillu...     

秸秆还田配施中微量元素对农田土壤有机碳固持的影响

为研究秸秆还田配施中量元素(S)和微量元素(Fe和Zn)对粮田土壤有机碳固持的影响,进行了为期52 d的室内玉米秸秆腐解培养试验. 结果表明:秸秆腐解过程中分别添加S、Fe和Zn元素,均提高了微生物生物量碳(MBC)及土壤CO₂-C矿化速率,52 d腐解培养结束后,CO₂-C的累积矿化量显著提高,但土壤有机碳含量并未显著降低;3种元素中,添加Fe或Zn的处理提高了土壤惰性碳库、惰性碳库比例及土壤有机碳表观平衡,有利于土壤有机碳固持,而添加S的处理却降低了惰性有机碳比例及土壤有机碳表观平衡,不利于有机碳固持. 因此,在施N、P肥基础上,秸秆还田添加S、Fe或Zn均能促进土壤有机碳的矿化进程,但添加Fe或Zn可使更多有机碳固持于土壤中,添加S不利于土壤有机碳的固持.     

不同作物秸秆对辣椒的化感效应

采用室内生物测定、室外盆栽的实验方法,研究了不同大田作物秸秆浸提液、腐解液及腐解物对辣椒的化感效应。结果表明:秸秆浸提液和腐解液对辣椒种子萌发的化感效应不同,浸提液抑制辣椒种子萌发,且随着浸提液浓度的增加,辣椒发芽指数、胚根长显著或极显著受到抑制,其中以大豆秸秆浸提液的抑制作用最强;秸秆腐解液对辣椒种子的萌发总体上表现为促进效应,腐解物对辣椒的株高、茎粗、鲜质量及根系活力均具有促进作用,且与腐解 物的添加量呈正比;不同秸秆腐解物的化感效应大小依次为玉米秸秆>水稻秸秆>大豆秸秆。     

玉米秸秆还田培肥土壤的效果

辽北地区玉米根茬还田、秸秆直接还田或间接还田的3年微区培肥试验研究结果表明,无机肥的增产效果特别明显,而施有机物料,更主要的作用是改善土壤的物理、化学性质、培肥地力,与无肥对照相比,有机无机肥料配合施用可使土壤有机质提高3．06％－27．78％,各有机物料对土壤有机质提高的顺序依次为100％秸秆＞50％秸秆＞土粪＞牛粪＞33％秸秆＞根茬。在含C量相等的条件下,秸秆对土壤有机质的保持和提高好于土粪,土粪好于牛粪。同时,与单施化肥比,有机无机肥料配合施用可使土壤易氧化有机质增加10．91％－20．67％,使浸提腐殖酸提高1．43％－14．28％,使结合态腐殖酸的松／紧比值提高0．07－0．19,HA／FA比值提高0．07－0．24,并且能改善土壤的N、P、K营养状况、土壤水分和土壤孔隙状况,这标志着土壤有机质活性的提高和土壤肥力状况的改善。因此,应该大力提倡玉米秸秆秋季直接还田,其最佳施入量应为当年生产量的30％－50％。     

Transformation of14C labelled plant components in soil in relation to immobilization and remineralization of15N fertilizer

Summary Uniformly¹⁴C labelled glucose, cellulose and wheat straw and specifically¹⁴C labelled lignin component in corn stalks were aerobically incubated for 12 weeks in a chernozem soil alongwith¹⁵N labelled ammonium sulphate. Glucose was most readily decomposed, followed in order by cellulose, wheat straw and corn stalk lignins labelled at methoxyl-, side chain 2-and ring-C. More than 50% of¹⁴C applied as glucose, cellulose and wheat straw evolved as CO₂ during the first week. Lignin however, decomposed relatively slowly. A higher proportion of¹⁴C was transformed into microbial biomass whereas lignins contributed a little to this fraction.After 12 weeks of incubation nearly 60% of the lignin¹⁴C was found in humic compounds of which more than 70% was resistant to hydrolysis with 6N HCl. Maximum incorporation of¹⁵N in humic compounds was observed in cellulose amended soil. However, in this case more than 80% of the¹⁵N was in hydrolysable forms.Immobilization-remineralization of applied¹⁵N was most rapid in glucose treated soil and a complete immobilization followed by remineralization was observed after 3 days. The process was much slow in soil treated with cellulose, wheat straw or corn stalks. More than 70% of the newly immobilized N was in hydrolysable forms mainly reepresenting the microbial component.Serial hydrolysis of soil at different incubation intervals showed a greater proportion of 6N HCl hydrolysable¹⁴C and¹⁵N in fractions representing microbial material.¹⁴C from lignin carbons was relatively more uniformly distributed in different fractions as compared to glucose, cellulose and wheat straw where a major portion of¹⁴C was in easily hydrolysable fractions.     

Edaphic mobility of complete humic acid and fractions of high and medium molecular weight

Soil mobility of a complete humic acid and high and medium molecular weight fractions was determined by a soil TLC method. High and medium molecular weight fractions were obtained by ultrafiltration and then labeled with radioiodine. Infrared, visible- and UV spectra, as well as isotachophoretic studies, showed marked differences among the three humic fractions. The results obtained made evident the presence of soil mobile humic fractions of medium molecular weight. Alkalinization increased the soil mobility of humic acid.     

The transformation of nitrogen and carbon in the soil during humification of straw labelled with N15

Summary Laboratory tests were made on the effect of NaNO₃ or (NH₄)₂CO₃ on the dynamics of humification in the soil of oat straw tagged with N¹⁵. The mixture was incubated for 112 days, at constant temperature and moisture conditions. It was found that NH₄-N accelerated the straw humifications more than NO₃-N. Humification started directly after the straw was introduced into the soil. N¹⁵ derived from straw consituted a part of the forming humic compounds. Already after 14 days of incubation, the N¹⁵ of straw was found in all fractions of humic compounds. Mineralization accompanied humification. The added inorganic-N accelerated not only straw humification, but also the mineralization of forming humic compounds. This is why the added inorganic-N had no influence on the content of humic compounds. The decisive factor in the increase of humic and fulvic acids in the soil, was the straw. The inorganic N added to the straw, had no influence on the quality of humic acids formed in the soil.     

Humic-like substances of bacterial origin. I. Some aspects of the formation and nature of humic-like substances produced by Pseudomonas.

Two bacterial strains Pseudomonas acidovorans No 26 and Pseudomonas sp. No 4 grown in Conn and yeast extract-glucose media, or in the media enriched with tyrosine, were found to produce dark brown pigment. It was shown that in the bacterial cultures numerous phenolic and quinone-type compounds were formed and transformed to humic-like polymers. Formation of humic-like substances started in the bacterial cells and was accompanied by the presence of phenyloxidases in the bacterial cultures. The bacterial "humic acids" were obtained from the supernatants in amounts varing from 0.05 to 0.865 mg/1 mg of dry weight of cells and from the cells in amounts of 0.02 to 0.165 mg/1 mg of dry weight of cells, depending on the medium used and time of incubation. The IR spectra of the bacterial "humic acids" appeared to be very similar to IR spectrum of the synthetic humic acids (Fluka A.G.) and contained the same chemical groups as the soil humic acids. The culture medium after growth of the strain No 26 was fractionated into "fulvic, hymatomelanic and humic acid" fractions. The hydrolysates from the obtained fractions contained amino acids and uronic acids. The amino acid composition appeared to be very similar to that of soil humic acids.     

农田生态条件下植物残体腐解过程腐解物的能态变化特征

用氧弹量熟计法研究了农田生态条件下玉米秸杆腐解过程腐解物的能态变化特征,并探讨了腐解物中不同组分对腐解物能态的影响。结果指出,在试验条件下,玉米秸杆腐解过程腐解物能态呈现波动起伏──趋于稳定２个阶段,其中多以吸能、放能交错的方式迸行,但从整体上看是放能过程。能量活性物质（苯－醇溶性物、水溶性物、纤维素、半纤维素）对腐解前期腐解物能恣变化影响较大;能量非活性物质（木质素、腐殖质等）对维持腐解后期腐解物能态趋于稳定具有重要作用。     

Characterization of humic materials extracted from hazelnut husk and hazelnut husk amended soils

This study was carried out to determine effects of composted hazelnut husk (CHH) on some chemical properties of soil and soil humic acid (HA). Compost application increases organic matter (OM) content of the soil considerably, OM value of 3.18% became 3.89% in 3 years time interval. Before application of compost, the soil pH was found to be 5.37, while after compost application it became 5.61. FTIR characteristics of humic acid/humic acid-like materials extracted from the original hazelnut husk, composted hazelnut husk and composted hazelnut husk amended soil have been investigated. C and O content of humic acid-like/humic acid materials were in the range of 41.4–50.8% and 37.8–50.5%, respectively. The N content of the humic acid/humic acid-like materials are in the expected range for humic materials which is 2–6%. Comparison of FTIR spectra of hazelnut husk and composted hazelnut husk humic acid-like fractions shows that both exhibit similar but not identical series of IR bands indicating the presence of the same functional groups in both samples. The only difference in the spectra seemed to be a decrement in the peak intensities of composted sample compared to uncomposted one. The similar differentiation of the intensities of IR bands of compost applied soil sample has also been observed. The FTIR spectral results show that the characteristics of composted material tend to become similar to that of soil humic acids characteristics in time.     

黑龙江不同玉米秸秆还田方式下土壤动物群落结构及其对秸秆降解的影响

以黑龙江省海伦市典型黑土耕地为试验样区,研究黑土区不同秸秆还田方式下土壤动物群落结构特征及其在秸秆降解中的作用。实验选取6目、30目、260目降解袋,设置5个处理:17kg玉米秸秆+2kg水还田+含微生物100%浓度催腐剂(样方A)、8.5kg玉米秸秆+1kg水还田+含微生物50%浓度催腐剂(样方B)、原始样方(样方C)、8.5kg玉米秸秆+1kg水还田(样方D)、17kg玉米秸秆+2kg水还田(样方E),并于2009—2011每年9月份测定不同样方的玉米秸秆降解率和微生物数量。结果表明:所有样方累积秸秆降解率都达55%以上,秸秆降解率从高到低排序依次为:样方A>样方B>样方C>样方D>样方E;对秸秆降解起主要作用的动物类群为中小型土壤动物中的甲螨亚目、中气门亚目和节跳虫科,约占土壤动物个体数的86.70%;不同处理样方中,土壤动物群落结构相似;相同处理样方中,不同规格的降解袋中土壤动物个数与类群差异显著(P<0.001);不同孔径降解袋中土壤动物的个数、类群数、多样性基本都与秸秆降解率呈正相关,进一步表明土壤动物对秸秆降解具有促进作用。