异噁草酮对土壤微生物和土壤酶活性的影响

本试验检测了异噁草酮处理土壤后土壤中微生物群落数量和土壤酶活性变化,目的在于研究异噁草酮对土壤微生态产生的影响。结果表明:土壤中异噁草酮有效成分浓度为200、500μg/kg和700μg/kg时,促进土壤中细菌和真菌数量增长,该数量在处理7d之内就会明显变化,并且此影响随异噁草酮使用浓度的提高而增强,但异噁草酮对放线菌的数量无显著影响。施用异噁草酮后,土壤酶活性反应程度由高到低的顺序为:转化酶多酚氧化酶过氧化氢酶。本研究中异噁草酮施入土壤后,除对多酚氧化酶有明显抑制作用,且该抑制作用在短时间内可恢复外,对土壤微生物数量和土壤酶活性都有促进作用。     

苦参碱在土壤中的环境行为研究

农药在土壤中的吸附、移动及消解等特性是评价其环境安全性的重要指标。为评价植物源农药苦参碱对土壤环境的安全性,依据《化学农药环境安全评价试验准则》,探讨了苦参碱在东北黑土、江西红土、关中娄土及河南二合土等典型土壤中的吸附、移动、消解特性及其影响因素。结果表明:苦参碱在4类典型土壤中均为中等吸附、易移动,且土壤有机质含量与其吸附性呈正相关;在未灭菌条件(25℃,避光)下,苦参碱在4类6种不同土壤中的消解半衰期为4.1~9.8 d,而在灭菌条件下,半衰期为11.6~13.7 d,均为易降解。研究表明,苦参碱对土壤环境较为安全。     

Photolytic versus microbial degradation of clomazone in a flooded California rice field soil

BACKGROUND: Clomazone is a popular herbicide used on California rice fields and exhibits rapid anaerobic microbial degradation (t_1/2 = 7.9 days). To test the potential of direct and indirect photolytic degradation as a cofactor in the overall degradation rate, sacrificial time‐series microcosms were amended with water, non‐sterilized soil + water and sterilized soil + water. Clomazone was added to each microcosm, which was then exposed to natural and artificial sunlight over 35 days. Water and acetonitrile extracts were analyzed for clomazone and metabolites via LC/MS/MS. RESULTS: The calculated pseudo‐first‐order degradation rate constants (k) were k_water = 0–0.005 ± 0.003 day^?1, k_sterile = 0–0.005 ± 0.003 day^?1 and k_non?sterile = 0.010 ± 0.002–0.044 ± 0.007 day^?1, depending on light type. The formation of ring‐open clomazone, a microbial metabolite, correlated with clomazone degradation. Trace amounts of 5‐hydroxyclomazone (m/z = 256 → 125), aromatic hydroxyclomazone (m/z = 256 → 141) and an unknown product (m/z = 268 → 125) were observed. CONCLUSIONS: The photolytic degradation rate depends on both light type and the quality of the chromophores that induce indirect photolysis. Microbial degradation was found to be sensitive to temperature fluctuations. Overall, microbes are shown to be more detrimental to the environmental fate of clomazone than photolysis. Copyright © 2012 Society of Chemical Industry     

棉粕腐植酸肥对土壤团聚体、酶及养分的影响

采用田间试验方法,以小麦新春38号作为供试品种,设置3个处理:空白对照、等养分复合肥和等养分棉粕腐植酸复合肥,研究了棉粕开发的腐植酸水溶性肥料对土壤团聚体、酶和养分的影响。结果表明:与不施肥处理相比较,腐植酸肥处理使土壤团聚体含量向2~0.25 mm和2 mm粒级有显著转移;土壤脲酶活性、过氧化氢酶和碱性磷酸酶活性显著提高,对蔗糖酶活性差异不明显;可显著提高碱解氮、速效钾和有效磷含量,腐植酸肥处理能平均提高全生育期0~20 cm土层碱解氮37.27%、速效磷42.24%、速效钾37.02%,20~40 cm土层碱解氮提高15.55%、速效磷提高61.52%、速效钾提高57.36%。与等养分复合肥处理相比,腐植酸肥处理使不同土层土壤团聚体百分含量向2~0.25 mm和2 mm粒级均有转移;前期抑制土壤脲酶活性,后期提高壤脲酶活性,提高过氧化氢酶和碱性磷酸酶活性,蔗糖酶活性差异不明显;可提高土壤中碱解氮含量,显著提高速效钾和速效磷含量,腐植酸肥处理可平均提高全生育期0~20 cm土层碱解氮5.92%、速效磷8.8%、速效钾4.29%,20~40 cm土层碱解氮提高1.9%、速效磷提高15.39%、速效钾提高8%。     

东北黑土区农业生态环境问题与对策

黑土是一种自然肥力很高的耕作土壤,主要分布在松嫩平原东部。黑土区一直以肥沃的土壤,优越的气候条件,多样的生境和雄厚的农业科技条件而著称。然而,随着全球气候的变化,经济的发展,城镇用地和农村居民地的扩展,黑土区在自然和人为两方面因素的影响下,出现了严重的生态环境问题,如土壤侵蚀严重,土壤退化导致的土地生产力降低、水资源短缺、农田污染以及自然灾害加剧等。在分析环境问题现状和产生原因的基础上,提出改善黑土区生态环境的对策,为东北地区农业的持续发展提供参考。     

影响降解菌W2修复异噁草酮污染土壤的三种因子的优化

［目的］ 确定降解菌W2对土壤中异噁草酮的最优生物修复条件。［方法］ 采用3因素5水平正交旋转组合设计,室外盆栽生物测定方法,研究降解菌W2接种量、土壤含水量和肥料添加量3种田间可控因子对降解菌W2修复异噁草酮污染土壤效果的影响。［结果］ 确定修复条件的优化数学回归模型为:y=62.363 9+5.872 8×C1-4.494 1×C2C3-1.262 1×C21-4.076 7×C22,不同因子对土壤修复影响大小顺序依次为土壤含水量、肥料添加量、降解菌W2接种量。［结论］ 降解菌W2对土壤中异噁草酮的最优生物修复条件为：降解菌W2接种量8.19～11.81 mL/kg（A650=0.4）,土壤含水量18.6%～20.84%,肥料添加量1.83～2.52 g/kg。在此范围内降解菌W2对异噁草酮有效成分浓度为500 μg/kg的风干土壤30 d后的降解率可达60%以上,可接近该修复天数的理论极值65.56%。     

Response of soil nitrogen,phosphorous and organic matter to vegetation succession on the Loess Plateau of China

 Revegetation is a traditional practice widely used for soil protection. We evaluated the effect of natural revegetation succession on soil chemical properties and carbon fractions (particulate organic carbon (POC), humus carbon (HS-C), humic acid carbon (HA-C) and fulvic acid carbon (FA-C)) on the Loess Plateau of China. The vegetation types, in order from the shortest to the longest enclosure duration, were: (a) abandoned overgrazed grassland (AbG3; 3 years); (b) Hierochloe odorata Beauv. (HiO7; 7 years); (c) Thymus mongolicus Ronnm (ThM15; 15 years); (d) Artemisia sacrorum Ledeb (AtS25; 25 years); (e) Stipa bungeana Trin Ledeb (StB36; 36 years) and (f) Stipa grandis P. Smirn (StG56; 56 years). The results showed that the concentrations of soil organic carbon, total nitrogen and available phosphorus increased with the increase of restoration time except for ThM15. The concentration of NH₄-N increased in the medium stage of vegetation restoration (for ThM15 and AtS25) and decreased in the later stage (for StB36 and StG56). However, NO₃-N concentration significantly increased in the later stage (for StB36 and StG56). Carbon fractions had a similar increasing trend during natural vegetation restoration. The concentrations of POC, HS-C, FA-C and HA-C accounted for 24.5%–49.1%, 10.6%–15.2%, 5.8%–9.1% and 4.6%–6.1% of total carbon, respectively. For AbG3, the relative changes of POC, HS-C and FA-C were significantly higher than that of total carbon during the process of revegetation restoration. The higher relative increases in POC, HS-C and FA-C confirmed that soil carbon induced by vegetation restoration was sequestrated by higher physical and chemical protection. The increases of soil C fractions could also result in higher ecology function in semiarid grassland ecosystems.     

The basis for the safening of clomazone by phorate insecticide in cotton and inhibitors of cytochrome P450s

Clomazone may be safely used in cotton to manage weeds when applied following treatments of the organophosphate insecticides phorate or disulfoton. The loss of chlorophyll and carotenoids with 6 days of 100 nM clomazone treatment of cotton seedlings was partially prevented with phorate in hydroponic solution in a rate-dependent manner. In a study to examine the timing of safening from a one-day clomazone (100 nM) treatment, maximum safening was achieved when phorate (50 μM) was applied the same day as clomazone. Phorate decreased metabolism of ¹⁴C-clomazone to polar metabolites in excised cotton shoots and shoots of intact cotton plants. Microsomal studies of corn shoots showed an NADPH-dependent/cytochrome P450 reaction was inhibited by phorate. Additional studies with corn microsomes, corn seedlings and cotton seedlings supported the basis of clomazone safening is the inhibition of toxic clomazone metabolism by P450 inhibitors.     

东北半干旱黑土区玉米秸秆还田方式对土壤水溶性有机碳含量及其组分的影响

为明确不同秸秆还田方式下土壤有机碳组分的变化特征,基于6 a秸秆还田长期定位试验,利用三维荧光光谱技术,对无秸秆还田（CK）、秸秆覆盖还田（FG）、秸秆翻埋还田（FM）处理下土壤有机碳（SOC）含量及水溶性有机碳（WSOC）含量及其结构特征进行分析。结果表明：（1）与CK相比,FM处理0~40 cm土层SOC含量提高7.87%~29.54%,FG处理0~30 cm土层SOC含量增加1.91%~18.61%,30~40 cm土层SOC含量降低7.67%;FM和FG处理0~40 cm土层土壤WSOC含量分别提升13.42%~39.42%和0.28%~26.34%。（2）通过WSOC三维荧光光谱发现,各土层CK（Ex/Em=300/34、Ex/Em=300/340、Ex/Em=240/340、Ex/Em=300/340）处理WSOC荧光特征峰为溶解性微生物代谢产物和类色氨酸蛋白质物质荧光峰;FM（Ex/Em=340/430、Ex/Em=340/430、Ex/Em=340/435、Ex/Em=340/435）和FG（Ex/Em=270/440、Ex/Em=270/435、Ex/Em=340/435、Ex/Em=340/430）处理为类腐殖酸类物质荧光特征峰,腐殖化程度较高,结构较为复杂;荧光区域积分表明,FM和FG处理类腐殖酸类物质（Ⅴ）和富里酸类物质（Ⅲ）的积分百分比分别较CK增加12.18%~27.39%、11.98%~30.72%和3.96%~5.73%、2.99%~5.40%。（3）土壤WSOC包含两个组分,C1（Ex/Em=340/435, 270/435）组分为类腐殖酸类物质,C2（Ex/Em=290/345, 240/345）组分为溶解性微生物代谢产物和类色氨酸蛋白质物质;F_max值结果表明,0~40 cm土层的C1组分相对含量表现为FM>FG>CK,表明秸秆翻埋还田更有助于土壤中营养物质含量增加和形成更高分子量的有机物。综上,不同秸秆还田方式均可提升SOC和土壤WSOC含量,增加腐殖化程度,加强土壤的供肥能力,翻埋还田处理提升作用更为显著。     

The effect of soil moisture content on the sorption of five sterol biosynthesis inhibiting fungicides as a function of their physicochemical properties

We investigated the sorption of five widely used sterol biosynthesis inhibitor fungicides (SBIs: flusilazole, propiconazole, epoxiconazole, fenpropimorph and prochloraz) on a loam soil to assess availability of the SBI residues that are usually left in soil after crop treatments. We focused particularly on the soil moisture content effect, which is poorly documented and is difficult to investigate under realistic conditions. SBI sorption was determined (using diuron as a reference) at two soil moisture contents (26.1% and 46.6% w/w) over a period of 3 weeks using a direct soil solution sampling method. After 24 h of contact, <1% of each applied fungicide was recovered in the soil solution. Despite their low availability in the liquid phase, long‐term sorption was observed for all the compounds, reducing concentrations in the soil solution and doubling the value of the partition coefficient. Significant effects of soil moisture on long‐term sorption were observed, depending on the properties of the chemicals and the sorption mechanisms. Wershaw's humus model (humic substances have a membrane‐like structure) was adapted to fit our observations. Low soil moisture content is assumed to modify the structure of humic substances and to generate hydrophobic surfaces, which favour sorption of hydrophobic fungicides (flusilazole, propiconazole and epoxiconazole). This effect is likely to decrease with the increase in the hydrophobic character of non‐ionic pesticides. It becomes adverse for the more hydrophilic compounds (diuron), which are more sorbed at high soil moisture content due to their higher affinity for hydrophilic regions of humus and to diffusion. Soil moisture effects are more complex when compounds are likely to be protonated in soil. Weakly basic compounds (prochloraz) may partition rapidly into the liquid‐like interior of humus at low soil moisture content but increased diffusion at high soil moisture content may cause additional sorption by ion exchange at colloid surfaces. Strongly basic compounds (fenpropimorph) may essentially adsorb due to ionic interactions with colloids, and their sorption is enhanced at high soil moisture content due to diffusion. Consequences for environmental fate and biological activity of pesticides are briefly discussed. © 2000 Society of Chemical Industry     

Sorption/desorption behaviour of sulfonylurea herbicides as affected by the addition of fresh and composted olive cake to soil

The olive industry generates residues which can be applied as amendments to soils in their original form (olive cake) or after composting or vermicomposting processes. The addition, fresh or incubated, of these amendments to soil and of their different organic fractions was studied in relation to the sorption/desorption of three sulfonylurea herbicides, bensulfuron‐methyl, chlorsulfuron and prosulfuron. Herbicide sorption was low or very low, slightly promoted by the addition of the agricultural by‐products, especially olive cake, and mainly affected by pH of the soil solution, with the organic carbon content having no significant effect on herbicide retention. Desorption was only reduced when fresh olive cake was added. The incubation of soil and amendments for 3 months did not modify herbicide sorption, but made desorption reversible except for olive cake. The transformation of the organic matter of the amendments due to humification and maturity processes are likely to be responsible for this behaviour. Different organic fractions were removed to assess the influence of each fraction on sulfonylurea sorption. Only the removal of all studied organic fractions increased herbicide sorption, revealing the role of humin and mineral fractions in this process. Therefore, the use of organic amendments is not useful for reducing the risk of movement of ionisable molecules in soil.     

Comparative actions of clomazone on beta-carotene levels and growth in rice (Oryza sativa) and watergrasses (Echinochloa spp)

Seedlings of rice, early watergrass (thiobencarb-resistant and thiobencarb-susceptible biotypes, R and S, respectively), and late watergrass (thiobencarb-resistant and thiobencarb-susceptible biotypes, R and S, respectively) were hydroponically exposed to clomazone at concentrations ranging from 0.08 to 7.9 microM. Whole-plant growth (mg fresh wt) and beta-carotene concentrations (microg g(-1) fresh wt) were measured after a 7-day exposure period. For growth, the no observed effect concentrations (NOECs) were 7.9, 0.21, 0.21, 0.46 and 0.46 microM clomazone for rice, early watergrass (R), early watergrass (S), late watergrass (R) and late watergrass (S), respectively, while the concentrations causing 25% inhibition in response (IC25) were 5.6 (+/-1.6), 0.46 (+/-0.06), 0.42 (+/-0.08), 0.92 (+/-0.45) and 0.79 (+/-0.08) microM clomazone, respectively. Clomazone inhibits beta-carotene synthesis via inhibition of the non-mevalonate isoprenoid synthetic pathway. For assessment of clomazone effects, beta-carotene levels proved to be a more sensitive toxicological endpoint than growth. For rice, early watergrass (R), early watergrass (S), late watergrass (R) and late watergrass (S), the beta-carotene NOECs were 0.21, <0.08, <0.08, 0.08 and 0.46 microM clomazone respectively, while IC25 values were 0.42 (+/-0.26), 0.08 (+/-0.02), 0.08 (+/-0.02), 0.33 (+/-0.09) and 0.54 (+/-0.15) microM, respectively. No evidence was found that the thiobencarb-resistance mechanisms present in early and late watergrasses impart resistance to clomazone. Due to similar sensitivity between rice and late watergrass, use of clomazone in rice culture will require the use of a safening technique.     

玉米秸秆还田下深松年限对土壤有机碳含量及胡敏酸结构特征的影响

为明确不同秸秆还田结合耕作措施下土壤有机碳组分的变化特征,基于6 a秸秆还田长期定位试验,利用三维荧光光谱技术,对CK（不深松+不秸秆还田）、NFG（不深松+每年秸秆还田）、EFG（隔一年深松+每年秸秆还田）、TFG（隔两年深松+每年秸秆还田）和SFG（连年深松+每年秸秆还田）处理下土壤有机碳（SOC）含量及胡敏酸（HA）结构特征进行分析。结果表明：与CK相比,EFG处理0~10 cm土层的SOC、HA含量和PQ值分别显著增加25.23%、16.19%和4.27%,FA含量降低4.55%。10~20 cm土层,EFG处理的SOC含量最高,较CK增加13.18%;SFG处理的HA和FA含量较CK提高最多,增幅分别为13.27%和32.74%。通过HA三维荧光图谱发现,与CK(Ex/Em=270/455,270/460)相比,EFG(Ex/Em=280/455,270/465)处理下0~10 cm和10~20 cm土层中的HA荧光峰波长均有红移现象。土壤胡敏酸中包含两个组分,C1(Ex/Em=270/280)和C2(Ex/Em=440/515)同为类腐殖酸物质,胡敏酸整体腐殖化程度较高,结构较为复杂;其中EFG和TFG处理的C2组分所占比例最高,分别为28.59%和31.38%。各处理的C1和C2组分F_max值均较CK有所增加,即腐殖化程度增加。综上所述,EFG处理（隔一年深松+每年秸秆还田）通过提升土壤有机碳及腐殖酸类物质含量,增加腐殖化程度,加强了土壤的供肥能力,为黑龙江黑土区较佳的耕作技术措施。     

黑液腐植酸肥料对棉花生长及土壤肥力的影响

通过在北疆布设的3种肥料(腐植酸液体肥料HALF-A、HALF-B、HALF-C)5个施肥水平的田间试验,研究了黑液腐植酸肥料对棉花生长及土壤肥力的影响。结果表明:(1)与常规肥料比,应用不同黑液腐植酸液体肥料,增产幅度达到8.54%~10.80%,提高单铃重0.2~0.3 g,对衣分和单株有效成铃数影响不大;(2)施用腐植酸液体肥料能够推迟棉花成熟2~4 d;(3)腐植酸液体肥料施用量2250kg/hm2以上时显著促进了棉花花后干物质的累积;(4)三种腐植酸液体肥料施用量3 000 kg/hm2时对棉花氮素养分的吸收促进作用最大,HALF-B在施用量2250 kg/hm2,HALF-C在3 000 kg/hm2时促进了棉花磷素养分的吸收,腐植酸液体肥料施用量3 750 kg/hm2以上时显著促进了棉花钾素养分的吸收;(5)施用腐植酸液体肥料对当年收获后土壤肥力影响不大。     

东北黑土区土壤水分对大豆生长影响的试验研究

2009年在黑龙江省鹤山农场进行6个土壤水分水平控制的大豆盆栽试验,土壤水分分别是:15%、18%、24%、30%、40%、48%.结果表明:土壤水分和大豆产量有很好的二次曲线关系,决定系数R<'2>达到0.97,大豆产量在田间持水量条件下达到峰值,低干、高于田间持水量时,大豆均减产,田间持水量80%～133%减产幅度...     

耕作方式对黑土耕层孔隙分布和水分特征的影响

为探索耕作方式对黑土孔隙度分布和土壤水分特征的影响,以2010年吉林省德惠市中层黑土上进行了9年的田间定位试验小区土壤为研究对象,对免耕和秋翻两种耕作处理下耕层土壤孔隙度和土壤水分特征曲线进行分析。结果表明不同耕作处理对黑土孔隙度影响较大。与秋翻相比,免耕减小了土壤总孔隙度,增大了0～5cm和20～30cm10%～16%的>100μm大孔隙,减小了耕层5～20cm的100～30μm次大孔隙,两种处理不同深度的中孔隙和微孔隙数量相近。不同耕作方式对土壤水分特征的影响存在较大差异,免耕0～5cm和20～30cm的持水能力高于秋翻,而5～20cm表现出相反的变化趋势。实施免耕后,改变了土壤孔隙分布和持水性能,对土壤通气透水和作物根系发育具有重要作用。     

Imazaquin mobility in tropical soils in relation to soil moisture and rainfall timing

Summary This research studied the influence of soil type, soil moisture and incubation time before rain on the mobility of imazaquin in two highly weathered tropical soils, named clay and sandy clay. The soils were packed in glass columns and treated at three different moisture contents. Then, the applied imazaquin (150 g a.i. ha⁻¹) was incubated for 0, 1 and 30 d before rainfall simulation began. Leaching was significantly higher in the sandy clay soil, when imazaquin was applied to moist samples and rainfall occurred soon after application (in this case, 73.4% of applied imazaquin was leached). Leaching was always low in the clay soil (in all cases, <1.8% of applied imazaquin was leached). In addition, imazaquin leaching potential was overestimated by the low K _d value (1.24 L kg⁻¹) measured for the clay soil using batch equilibration data. For this soil, the vacuum displacement method also failed to predict leaching (in this case, 28.9% of applied imazaquin was leached). Consequently, batch equilibration and vacuum displacement methods cannot be used to predict leaching of anionic organic molecules, such as imazaquin, in fine-textured tropical soils. Moreover, soil type and weather patterns or irrigation timing must be considered before imazaquin application to avoid environmental or carry-over problems and to achieve maximum effectiveness of the herbicide.     

生物炭与腐殖酸配施对盐碱土理化性质的影响

为探索新型盐碱化土壤改良剂,选取玉米秸秆、葵花秸秆制成生物炭与腐殖酸配合,研究玉米秸秆生物炭(A)、混合秸秆生物炭(A₁)、腐殖酸(B)、玉米秸秆生物炭+腐殖酸(AB)、混合秸秆生物炭+腐殖酸(A₁B)5种改良剂与土壤混合后较对照组原土(CK)中盐碱指标、肥力指标的改善情况。结果表明:生物炭和腐殖酸都具有改良土壤盐碱性、提高土壤肥力的作用,二者联合配施对降低土壤pH、电导率(EC)、碱化度(ESP)及提高土壤养分的效果更明显,其中混合生物炭与腐殖酸配施(A₁B)效果最好,A₁B组处理的土壤pH较CK组显著降低10.8%,EC下降55%,ESP降低9.8%;速效钾、有效磷、速效氮及有机质的平均增幅较其他4个处理分别提升59.77%、210%、178%、180%。综上所述,混合施用生物炭及腐殖酸对于改良盐碱土效果明显。     

不同土地利用方式对农田黑土 剖面磷形态分布的影响

不同土地利用方式影响土壤磷形态分布,从而决定土壤潜在供磷能力。本文对4种土地利用方式下（裸地、自然草地、苜蓿地、农田）的黑土土壤剖面磷素分布进行测定分析,结果表明,不同利用方式持续12 a对黑土剖面磷形态分布影响较大,黑土中有机磷含量随土层深度增加而降低,而无机磷、有效磷含量及磷素活化系数随土层深度增加而呈增加趋势,在同一土层磷素活化系数表现为自然草地＞裸地＞苜蓿地＞农田。农田不施肥处理经过12 a玉米种植后,土壤中全磷、有效磷含量均低于其他利用方式,玉米植株主要吸收土壤中无机磷,与裸地相比,农田土壤Ca₂-P、Ca₈-P、Al-P、Fe-P、O-P、Ca₁₀-P含量依次降低了29.4%~75.3%、45.7%~59.5%、72.1%~83.3%、13.3%~36.1%、7.0%~33.2%、19.3%~41.6%。自然草地和苜蓿地比裸地无机磷含量分别降低11.5%~28.5%、2.2%~31.0%;与裸地相比,农田、自然草地和苜蓿地有机磷所占比例分别增加7.0~16.4、1.5~9.0、0.8~13.9个百分点。总之,不施肥农田作物吸收消耗了土壤中无机磷,使有机磷所占比例有所增加;自然草地和苜蓿地可使土壤中无机磷向有机磷转化,使有机磷比例有所增加。