种植Bt玉米对土壤微生物活性和肥力的影响

在温室种植比较了美国Bt玉米(34B2 4 (Mon810 ) )与同源常规玉米(34B2 3)、中国Bt玉米(12 4 6×14 82 (Cry1A) )与常规玉米(农大3138)对土壤微生物活性和肥力的影响。结果表明,两个Bt玉米品种5次取样(2 5、39、5 3、6 7、82 d)的根际土壤中都能检测到Bt蛋白,含量在2 0～80 ng·g- 1 dry soil之间。4个处理土壤硝化作用和精氨酸氨化作用强度在所有取样时期均没有显著差异;土壤蔗糖酶、土壤蛋白酶和酸性磷酸酶活性则分别只在2 5 d(农大3138<34B2 4与12 4 6×14 82 )、6 7d(34B2 4 >12 4 6×14 82和农大3138)和6 7d(34B2 4 >其它3个处理)存在显著差异;土壤脱氢酶、土壤脲酶和土壤呼吸强度则在多数取样时期多个处理间存在显著差异,说明其与玉米品种特性关系密切,其中,土壤脱氢酶和脲酶活性的差异在两个Bt玉米品种、Bt与同源常规品种(34B2 4与34B2 3)、Bt与常规品种(12 4 6×14 82与农大3138)以及常规与常规品种(34B2 3与农大3138)之间均没有一致的规律,但34B2 4与34B2 3处理的土壤呼吸作用强度高于12 4 6×14 82与农大3138,说明种植该系列品种的土壤中微生物总活性较高、土壤代谢旺盛。82 d后4个处理土壤有机质、NPK全量与速效养分含量均没有显著差异。本试验观测期种植Bt玉米并没有导致土壤微生物活性和土     

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％。     

玉米-大豆间作和施氮对红壤地中小型土壤动物群落特征的影响

通过2年田间定位试验(2013—2014),利用干漏斗法收集土壤中小型动物,探讨不同种植模式(玉米单作、玉米大豆间作、大豆单作)和施氮(0、150 kg·hm^-2)对红壤土壤动物数量和群落结构的影响.结果表明: 两年取样共捕获土壤中小型动物8349只,分属3门10纲29目,优势类群为蜱螨目和弹尾目.2013年间作和施氮均提高了玉米拔节期土壤动物的平均密度.2014年土壤动物类群数较2013年有明显的增加,施氮条件下的土壤动物平均密度较不施氮有所增加.两年多因素方差分析结果表明,种植模式和生育期对土壤动物平均密度、类群数和多样性指数都无显著影响.但在2014年,施氮显著影响了土壤动物类群数、Simpson指数和密度-类群指数;种植模式与玉米生育期的交互作用显著影响了土壤动物平均密度和类群数,同时对密度-类群和丰富度指数也有显著影响;施氮和生育期的交互作用显著影响了Simpson指数、密度-类群指数和Shannon指数.从两年的土壤动物群落去趋势分析结果来看,红壤地土壤动物群落在种植模式和施氮水平之间均没有明显的差异,群落组成的变化与玉米生育期相关.合理施氮条件下的玉米-大豆间作模式有利于提高红壤地土壤中小型动物平均密度和类群数,保持较好的多样性.     

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.     

转植酸酶基因玉米种植对土壤线虫群落的影响

土壤是生态系统中物质循环和能量转化的重要场所,转基因作物外源基因对土壤非靶标生物的影响已经引起人们的广泛关注.我国转植酸酶基因玉米(即自交系BVLA430101)于2009年9月27日获得了生物安全证书,该转植酸酶基因玉米可提高饲料利用效率,减少动物粪便造成的环境污染.本文以转植酸酶基因玉米(简称转基因玉米)和常规对照亲本玉米(简称对照玉米)为试验材料,通过大田试验研究了转基因玉米和对照玉米种植对土壤线虫群落组成与生态指标的影响.结果表明： 转基因玉米和对照玉米大田土壤分别分离出29个属和26个属的线虫.与对照玉米相比,转基因玉米种植田食细菌线虫相对多度与数量、捕/杂食线虫数量和土壤线虫总数,以及群落多样性指数等都有升高的趋势,而植食线虫相对多度与线虫总成熟度指数呈降低趋势.重复测量方差分析表明,整个生长季节内转基因玉米与对照玉米田间不同营养类群土壤线虫相对多度与数量及生态指标均无显著差异;而T检验分析表明,玉米乳熟期转基因玉米田食细菌线虫、捕/杂食线虫数量和土壤线虫总数显著高于对照玉米田,这可能与乳熟期转基因玉米田土壤总氮含量显著升高有关.     

秸秆颗粒还田对黑土土壤酶活性及细菌群落的影响

为探讨不同玉米秸秆颗粒还田量对黑土生物学特性及细菌群落的影响,在内蒙古兴安盟扎赉特旗农业科技示范园试验地设置秸秆0%还田,还田量0kg/hm^2(CK)、秸秆60%还田,还田量4500kg/hm^2(JG1)、秸秆70%还田,5250kg/hm^2(JG2)、秸秆80%还田,6000kg/hm^2(JG3)、秸秆90%还田,6750kg/hm^2(JG4)和秸秆100%还田,7500kg/hm^2(JG5)6个处理,通过连续2年大田试验,研究土壤蔗糖酶、脲酶、过氧化氢酶、碱性磷酸酶活性、微生物生物量碳氮以及细菌群落的变化。结果表明:秸秆还田能够增加土壤蔗糖酶(3.29%—32.12%),脲酶(5.32%—52.66%),过氧化氢酶(0.60%—27.11%),碱性磷酸酶的活性(10.89%—64.20%),土壤微生物生物量碳(1.32%—7.07%)、氮(16.35%—80.46%)含量;秸秆施入土壤也提高了黑土变形菌门和厚壁菌门相对丰度,提高了土壤固氮、分解养分及抵御病害能力,并降低了放线菌门相对丰度,降低了土壤病害发生概率,还出现了具有固氮、吸磷、改良土壤特性的新细菌,可见玉米秸秆还田具有重要的生态学意义,可在一定程度上增加细菌数量和种类多样性,进而使土壤系统向稳定健康的方向发展。综合研究结果在本试验条件下,以6750kg/hm^2为较适宜的玉米秸秆颗粒还田量。     

Preliminary determination of mycotoxin binding to soil when leaching through soil with water

Mycotoxin-contaminated crops that are left in the field are potential contaminants of groundwater. Aflatoxin B₁ (AFB₁) and fumonisin B₁ (FB₁) distribution in soil-water systems and the comparative response of aflatoxin-contaminated corn and pure aflatoxin when leached through soil were investigated using columns. Each experiment was repeated once. Eluates and soil extracts were analyzed for AFB₁ and its metabolites and FB₁ along with different amounts of pure FB₁ and water mixtures. AFB₁ was detected in water samples from columns containing 10% and 20% silty clay loam soil and aflatoxin-contaminated corn mixtures and in the upper (top) 2.5 cm of soil from the 10 cm soil column. Aflatoxin B₂ (AFB₂) was detected in eluates from the column containing 10% soil and aflatoxin-contaminated corn mixture and from the column containing aflatoxin-contaminated corn alone. No AFB₂ was detected in eluates from the column containing 20% soil and aflatoxin-contaminated corn mixture. No detectable amount of aflatoxin was observed in eluates from the containing 50% silty clay loam soil and aflatoxin contaminated corn. No detectable amount of FB₁ was observed in eluates or soil extracts, but FB₁ was detected in the mixtures of pure FB₁ and water.     

Dairy manure and tillage effects on soil fertility and corn yields

Organic amendments have received renewed attention to improve soil fertility for crop production. A randomized complete block split plot experiment was conducted to evaluate the dairy manure (DM) amendments of soil for corn (Zea mays L. cv. Monsanto 919) production under different tillage systems. Main plot treatments were no-till (NT), conventional tillage (CT), and deep tillage (DT), and subplot treatments were chemical fertilization (DM(0)), and DM at 10Mgha(-1)yr(-1) (DM(10)) and 20Mgha(-1)yr(-1) (DM(20)) with supplemental chemical fertilization. Results show that tillage and DM had significantly reduced bulk density (rho(b)) with greater porosity (f(t)) and hydraulic conductivity (K(fs)) than soils under NT and DM(0). Manuring was effective to improve soil physical properties in all tillage treatments. While manure significantly increased C sequestration, the N concentration was influenced by both tillage and manure with significant interaction. The CT significantly increased P as did the addition of manure. However, with manure, K was significantly increased in all tillage treatments. While tilled soils produced taller plants with higher grain yields, and water-use efficiency than NT soils, manuring, in contrast, increased corn harvest index. Manure exerted significant quadratic effect on corn biomass N and K uptake. The variable effects of tillage and dairy manuring on soil properties and corn growth are most probably related to "transitional period" in which soil ecosystems may have adjusting to a new equilibrium.     

Using NCSWAP to simulate seasonal nitrogen dynamics in soil and corn

The objective of this study was to determine if a re-calibrated version of the computer model NCSWAP (version 36) could accurately predict corn growth and soil N dynamics in conventionally tilled (CT) and no-till (NT) corn supplied with legume green manure or ammonium nitrate as N sources. We also attempted to ascertain the reasons for limitations in the model's ability to simulate corn growth and soil N dynamics found by our colleagues in a previous study and to propose potential improvements. The model was calibrated to accurately simulate total available N (N in plant above-ground biomass plus soil nitrate in the 0 to 45 cm profile) for a control and a fertilizer CT treatment in the 1992 growing season. To do so, input values defining the quantities of active soil organic N had to be reduced to 19% of the values proposed by the model developers and a solute transport factor defining the mobile vs. immobile fractions of soil nitrate adjusted from 0.8 to 0.2. The discrepancies between the proposed values and the lower values employed in this study might be due to the uncertainties in quantitatively describing soil N mineralization processes and the way they are handled in the model, as well as the lack of a component simulating macroporous-influenced water flow and solute transport in the model. With the current version, until one knows how to predict what these values are, the model needs to be re-calibrated for each experimental site and condition and thus is of limited value as a general model.With no further adjustment of input values, model validation success was mixed. The model accurately predicted total available N for treatments in the second year of the experiment that had the same N source and tillage as the treatments used for the calibration year but with the different weather and growing conditions. However, total available N was underpredicted where legume green manure was the N source and overpredicted with no-till cultivation. The model was accurate in simulating seasonal corn growth for nearly all the treatments, judged by nonsignificant mean difference (MD) values and highly significant correlation coefficients (r). Prediction of seasonal soil nitrate concentration was less accurate compared to total available N and corn growth variables. Potential improvements in the model's simulation of a no-till system as well as for predicting corn harvest yield and seasonal soil nitrate concentration where N deficiency occurs were discussed.     

Bioaccessibility of total bound fumonisin from corn flakes

Fumonisin B₁ (FB₁) is often found as a natural contaminant of corn and corn-based food. Several publications have demonstrated the presence of fumonisin bound to proteins and to other compounds of the matrix. In spite of the low oral bioavailability of FB₁ in rats, pigs, chickens, cows, and monkeys, FB₁ can cause agriculturally significant disease and possibly human cancer. The aim of this work was to determine the bioaccessibility of total bound FB₁ (TB FB₁) (percentage of TB FB₁, released from corn flakes to the chyme) after in vitro digestion. Two samples of corn flakes washed with solvents were incubated with gastrointestinal tract solutions simulating saliva plus stomach and duodenal juices. After hydrolysis of the chyme with KOH, TB FB₁ was determined as hydrolyzed FB₁ (HFB₁). The bioaccessibility of TB FB₁ in chyme from corn flakes was 37–64%, indicating that these derivatives should be considered in evaluation of exposure to fumonisin.     

Impact of Bt corn on rhizospheric and soil eubacterial communities and on beneficial mycorrhizal symbiosis in experimental microcosms

A polyphasic approach has been developed to gain knowledge of suitable key indicators for the evaluation of environmental impact of genetically modified Bt 11 and Bt 176 corn lines on soil ecosystems. We assessed the effects of Bt corn (which constitutively expresses the insecticidal toxin from Bacillus thuringiensis, encoded by the truncated Cry1Ab gene) and non-Bt corn plants and their residues on rhizospheric and bulk soil eubacterial communities by means of denaturing gradient gel electrophoresis analyses of 16S rRNA genes, on the nontarget mycorrhizal symbiont Glomus mosseae, and on soil respiration. Microcosm experiments showed differences in rhizospheric eubacterial communities associated with the three corn lines and a significantly lower level of mycorrhizal colonization in Bt 176 corn roots. In greenhouse experiments, differences between Bt and non-Bt corn plants were detected in rhizospheric eubacterial communities (both total and active), in culturable rhizospheric heterotrophic bacteria, and in mycorrhizal colonization. Plant residues of transgenic plants, plowed under at harvest and kept mixed with soil for up to 4 months, affected soil respiration, bacterial communities, and mycorrhizal establishment by indigenous endophytes. The multimodal approach utilized in our work may be applied in long-term field studies aimed at monitoring the real hazard of genetically modified crops and their residues on nontarget soil microbial communities.     

Contribution of above‐ and belowground bioenergy crop residues to soil carbon

GHG mitigation by bioenergy crops depends on crop type, management practices, and the input of residue carbon (C) to the soil. Perennial grasses may increase soil C compared to annual crops because of more extensive root systems, but it is less clear how much soil C is derived from above‐ vs. belowground inputs. The objective of this study was to synthesize the existing knowledge regarding soil C inputs from above‐ and belowground crop residues in regions cultivated with sugarcane, corn, and miscanthus, and to predict the impact of residue removal and tillage on soil C stocks. The literature review showed that aboveground inputs to soil C (to 1‐m depth) ranged from 70% to 81% for sugarcane and corn vs. 40% for miscanthus. Modeled aboveground C inputs (to 30 cm depth) ranged from 54% to 82% for sugarcane, but were 67% for miscanthus. Because 50% of observed miscanthus belowground biomass is below 30 cm depth, it may be necessary to increase the depth of modeled soil C dynamics to reconcile modeled belowground C inputs with measured. Modeled removal of aboveground corn residue (25–100%) resulted in C stock reduction in areas of corn–corn–soybean rotation under conventional tillage, while no‐till management lessoned this impact. In sugarcane, soil C stocks were reduced when total aboveground residue was removed at one site, while partial removal of sugarcane residue did not reduce soil C stocks in either area. This study suggests that aboveground crop residues were the main C‐residue source to the soil in the current bioethanol sector (corn and sugarcane) and the indiscriminate removal of crop residues to produce cellulosic biofuels can reduce soil C stocks and reduce the environmental benefits of bioenergy. Moreover, a switch to feedstocks such as miscanthus with more allocation to belowground C could increase soil C stocks at a much faster rate.     

旱地全膜双垄沟播玉米的土壤水热效应及其对产量的影响

以春玉米品种沈单16号为试验材料,研究半干旱区（年均降雨量415 mm）旱地不同覆盖种植方式的土壤水热效应及其对玉米产量的影响.结果表明： 与裸地平作（CK）相比,全膜双垄沟播（PMF）、全沙覆盖平作（SM）在玉米抽雄前均能提高0～25 cm土层平均地温,其中PMF增温最高;随种植年限增加,各处理对土壤水分的耗散深度增加,种植第1年对20～120 cm土层的水分耗散最多,种植第2年对120～200 cm土层的水分耗散最多,其中PMF耗水量最高.PMF的穗粒数、穗粒重和百粒重最高,SM次之,CK最低;与SM和CK相比,2009和2010年PMF平均穗粒数分别增加13.5%和114.2%,平均穗粒重分别增加29.8%和321.1%,平均百粒重分别增加14.4%和95.4%;PMF和SM的产量分别比CK高333.1%和240.2%,水分利用效率（WUE）分别提高290.6%和227.6%.PMF玉米连续种植两年后,120～200 cm土层土壤水分消耗达72 mm,显著高于SM（45 mm）和CK(40 mm).由于PMF能提高苗期-抽雄期地温,促进作物前期生长,提高玉米对土壤水的利用,从而使穗粒数、百粒重等增加,表现出较高的产量和水分利用效率,但该模式对1 m以下土壤水分消耗较多,对保持水分年际平衡不利.     

玉米连作及其施肥对土壤微生物群落功能多样性的影响

采用Biolog技术,借助吉林农业大学1984年建立的长期定位试验,以撂荒和非玉米连作(当季作物为芸豆)为对照,研究玉米连作及其不同施肥措施对土壤微生物功能多样性的影响。结果表明,反映土壤微生物活性的平均颜色变化率(AWCD)呈现出以下变化规律:撂荒(UC)非玉米连作(NCC)玉米连作不施肥(CK);玉米连作配施秸秆(S、SN、SNPK)玉米连作配施NPK(NPK)玉米连作不施肥(CK)玉米连作单施N(N)。微生物培养72h活性旺盛,各处理AWCD在0.395—0.732之间,其中撂荒AWCD显著高于非玉米连作和玉米连作不施肥(P0.05);玉米连作配施秸秆明显提高微生物活性,玉米连作配施秸秆(S、SN、SNPK)AWCD是玉米连作不施肥和单施化肥(N、NPK)的1.26—1.62倍。玉米连作不施肥土壤微生物群落多样性指数(H、E、S)低于撂荒处理,但高于非玉米连作处理,非玉米连作提高了土壤微生物优势度指数。玉米连作配施秸秆土壤微生物物种丰富度指数和均匀度指数高于玉米连作不施肥和玉米连作施化肥,玉米连作单施氮肥优势度指数较高,其它多样性指数降低。主成分分析结果表明,不同处理土壤微生物碳源利用特征出现分异:撂荒和玉米连作配施秸秆处理集中在第1主成分正方向,得分系数在2.39—4.17之间,土壤微生物碳源利用特征相似;玉米连作不施肥、玉米连作单施化肥和非玉米连作处理分布在第1主成分负方向,得分系数在-5.43—-1.59之间。土壤微生物利用的碳源主要是糖类、羧酸类、氨基酸和聚合物。玉米连作配施秸秆和撂荒有利于提高土壤微生物代谢活性和土壤微生物群落功能多样性,玉米连作单施化肥尤其单施氮肥土壤微生物活性和功能多样性下降。     

Aboveground productivity and soil carbon storage of biofuel crops in Ohio

Biofuel crops may help achieve the goals of energy‐efficient renewable ethanol production and greenhouse gas (GHG) mitigation through carbon (C) storage. The objective of this study was to compare the aboveground biomass yields and soil organic C (SOC) stocks under four crops (no‐till corn, switchgrass, indiangrass, and willow) 7 years since establishment at three sites in Ohio to determine if high‐yielding biofuel crops are also capable of high levels of C storage. Corn grain had the highest potential ethanol yields, with an average of more than 4100 L ha^?1, and ethanol yields increased if both corn grain and stover were converted to biofuel, while willow had the lowest yields. The SOC concentration in soils under biofuels was generally unaffected by crop type; at one site, soil in the top 10 cm under willow contained nearly 13 Mg C ha^?1 more SOC (or 29% more) than did soils under switchgrass or corn. Crop type affected SOC content of macroaggregates in the top 10 cm of soil, where macroaggregates in soil under corn had lower C, N and C : N ratios than those under perennial grasses or trees. Overall, the results suggest that no‐till corn is capable of high ethanol yields and equivalent SOC stocks to 40 cm depth. Long‐term monitoring and measurement of SOC stocks at depth are required to determine whether this trend remains. In addition, ecological, energy, and GHG assessments should be made to estimate the C footprint of each feedstock.     

土壤水分变化对玉米苗期吸收积累镉的影响

采用土壤盆栽试验研究不同土壤水分含量对玉米苗期吸收积累 Cd的影响。试验结果表明 ,玉米生物量及其吸收 Cd量在玉米不同的生长时期差异较大。2 2 d收获时 ,玉米地上部和地下部生物量均随着田间持水量 (35 %～ 85 % )的增加而提高 ;而 16 d收获时 ,玉米生物量在田间持水量为 35 %和 85 %时比在其它水分时低许多。 16 d和 2 2 d收获时 ,玉米地上部 Cd含量在田间持水量 5 5 %时分别达到最大值 ,5 5 .4 1mg/ kg和 39.33mg/ kg;而在田间持水量 85 %时分别达最小值 ,2 7.97mg/ kg和 2 3.5 2 m g/kg。在玉米根系的影响下 ,土壤溶液 Cd含量基本上随着玉米的不断生长而降低。田间持水量为 6 5 %时的土壤溶液 Cd含量比田间持水量为 75 %和 85 %时大。玉米总吸 Cd量与水分蒸腾量之间呈极显著的线性正相关关系     

Perennial warm‐season grasses for producing biofuel and enhancing soil properties: an alternative to corn residue removal

Removal of corn (Zea mays L.) residues at high rates for biofuel and other off‐farm uses may negatively impact soil and the environment in the long term. Biomass removal from perennial warm‐season grasses (WSGs) grown in marginally productive lands could be an alternative to corn residue removal as biofuel feedstocks while controlling water and wind erosion, sequestering carbon (C), cycling water and nutrients, and enhancing other soil ecosystem services. We compared wind and water erosion potential, soil compaction, soil hydraulic properties, soil organic C (SOC), and soil fertility between biomass removal from WSGs and corn residue removal from rainfed no‐till continuous corn on a marginally productive site on a silty clay loam in eastern Nebraska after 2 and 3 years of management. The field‐scale treatments were as follows: (i) switchgrass (Panicum virgatum L.), (ii) big bluestem (Andropogon gerardii Vitman), and (iii) low‐diversity grass mixture [big bluestem, indiangrass (Sorghastrum nutans (L.) Nash), and sideoats grama (Bouteloua curtipendula (Michx.) Torr.)], and (iv) 50% corn residue removal with three replications. Across years, corn residue removal increased wind‐erodible fraction from 41% to 86% and reduced wet aggregate stability from 1.70 to 1.15 mm compared with WSGs in the upper 7.5 cm soil depth. Corn residue removal also reduced water retention by 15% between ?33 and ?300 kPa potentials and plant‐available water by 25% in the upper 7.5 cm soil depth. However, corn residue removal did not affect final water infiltration, SOC concentration, soil fertility, and other properties. Overall, corn residue removal increases erosion potential and reduces water retention shortly after removal, suggesting that biomass removal from perennial WSGs is a desirable alternative to corn residue removal for biofuel production and maintenance of soil ecosystem services.     

Alleviation of soil acidity in Ultisol and Oxisol for corn growth

Malaysian Ultisols and Oxisols are characterized by low pH, high soil solution Al concentration and Ca and/or Mg deficiencies, which are limiting to corn growth. An experiment was conducted to determine the changes in solid and soil solution phase properties of a representative Ultisol and Oxisol following applications of ground magnesium limestone (GML), gypsum and their combinations, and their effects on corn growth. A plot of pAl against lime potential (pH-1/2 pCa) showed that the points were mostly positioned between the theoretical lines for kaolinite-quartz and gibbsite equilibrium, reflecting the kaolinitic-oxidic mineralogy of the Ultisol and Oxisol. Gypsum application increased Al concentration in the soil solutions of the Ultisol, but had no significant effect on that of the Oxisol. The increase in Al concentration in the Ultisol was due to an increase in ionic strength. Gypsum application increased soil solution pH of the Oxisol due to release of OH as a result of ligand exchange between SO₄ and OH ions on the oxides of Fe and/or Al. Exchangeable Al in both soils was reduced by gypsum application. The reduction was associated with solid phase immobilization through alunite formation; the soil solutions of soil samples treated with 2 and 4 t gypsum ha⁻¹ were supersaturated with respect to alunite. Application of GML at 2 t ha⁻¹ together with 1–2t gypsum ha⁻¹ gave high top weight of corn. Relative top weight of corn was positively correlated with a soil solution Mg and Ca/Al concentration ratio, but negatively correlated with soil solution Al concentration. Foliar Al corn was positively correlated with soil solution Al concentration. Soil solution Al and Mg concentrations, and Ca/Al concentration ratio can be used as indices of soil acidity in Ultisols and Oxisols. ei]{gnB E}{fnClothier}     

农田生态系统不同土地利用方式与管理措施对土壤质量的影响

于2005年在北京市延怀盆地选择农田生态系统中的玉米地、大豆地两种传统土地利用方式,以及近10～20 年由传统农业用地转化而来的蔬菜和果园用地,研究农田生态系统不同土地利用方式与管理措施对土壤质量的影响.结果表明,菜地、果园和高投入玉米地土壤总有机碳(SOC)、全氮(TN)和全磷(TP)含量明显高于中、低投入玉米地和大豆地土壤.在各种土地利用类型中,SOC、TN和TP的变化范围分别为7.67～10.00 g·kg^-1、0.75～1.12 g·kg^-1和0.63～1.00 g·kg^-1;菜地土壤有效磷(AP)含量和电导率(EC)显著高于其他土壤,不同农田生态系统土壤物理性状差异不明显.果园和菜地土壤质量指数分别为0.525和0.503,高于传统农田玉米和大豆土壤(0.417～0.494).菜地土壤的养分有效性最高,水分有效性和根系适宜性低于果园土壤,应注意菜地非点源污染的潜在风险.在传统农业用地中应采取培肥地力等方式提高土壤质量.