Degradation of chlorsulfuron and triasulfuron in alkaline soils under laboratory conditions

The degradation of chlorsulfuron and triasulfuron was investigated in alkaline soils (pH 7.1–9.4) spiked at 40 μg a.i. kg^–1 under laboratory conditions at 25 °C and a moisture content corresponding to 70% field capacity (–33 kPa), using high-performance liquid chromatography. Degradation data for the two herbicides did not follow first-order kinetics, and observed DT₅₀ values in surface soils ranged from 19 to 42 days and from 3 to 24 days for chlorsulfuron and triasulfuron respectively. Disappearance of both chlorsulfuron and triasulfuron was faster in non-sterile than in sterile soil, demonstrating the importance of microbes in the breakdown process. The persistence of chlorsulfuron increased with increasing depth, which can be attributed to the decline in the microbial populations down the profile. The DT₅₀ value for chlorsulfuron at 30–40 cm depth was nearly four times higher than that in the top-soil. The results obtained show that persistence of these herbicides in alkaline surface soils at 25 °C and at a moisture content of 70% field capacity is similar to those reported in other European and North American soils. The study shows that if these herbicides are contained in surface soil layers, the risk of residue carry-over under southern Australian conditions is small. However, the rate of their degradation in alkaline subsoils is very slow, and under conditions conducive to leaching their prolonged persistence in the soil profile is possible.     

Applicability of ELISA for determination of metsulfuron‐methyl in soil samples

An immunoassay (ELISA) for analysis of metsulfuron‐methyl was evaluated as a method for quantifying residues in soil. Soil samples were extracted with phosphate buffered saline (PBS), PBS + acetone (80 + 20 by volume) or ammonium carbonate and were analyzed with both ELISA and LC‐MS. A tendency for the ELISA to overstimate the metsulfuron‐methyl content was noted and matrix effects were pronounced, particularly in PBS + acetone or ammonium carbonate extracts. Dilution of extracts before analysis improved the situation but reduced the sensitivity of the assay. Using light standard concentrations it was shown that the extracts in PBS on dilutions exhibited a curve parallel with the standard curve, indicating no significant interference due to matrix effects. A working range of 10–250 ng litre⁻¹ was found for ELISA on this type of extracts. © 2000 Society of Chemical Industry     

The relative movement and persistence in soil of chlorsulfuron, metsulfuron-methyl and triasulfuron

Summary. Adsorption and degradation rates of triasulfuron in 8 different soils were negatively correlated with soil pH and were generally lower in subsoils than in soils from the plough layer. The half-life at 20°C varied from 33 days in a top soil at pH 5·8 to 120 days in a subsoil at pH 7·4. Adsorption distribution coefficients in these two soils were 0·55 and 0·19, respectively. Movement and persistence of residues of chlorsulfuron, triasulfuron and metsulfuron-methyl were compared in a field experiment prepared in spring 1987. Triasulfuron was less mobile in the soil than the other two compounds. Residues of all three herbicides were largely confined to the upper 40–50 cm soil 148 days after application. With an initial dose of 32 g ha⁻¹, residues in the surface soil layers were sufficient to affect growth of lettuce and sugar-beet sown approximately one year after application. Laboratory adsorption and degradation data were used with appropriate weather data in a computer model of herbicide transport in soil. The model gave good predictions of total soil residues during the first five months following application, and also predicted successfully the maximum depth of penetration of the herbicides into the soil during this period. However, more herbicide was retained close to the soil surface than was predicted by the model. The model predicted extensive movement of the herbicides in the soil during winter but did not predict that residues sufficient to affect crop growth could be present in the upper 15–20 cm soil after one year.     

Analysis of metsulfuron‐methyl residues in wheat field soil: a comparison of HPLC and bioassay techniques

BACKGROUND: Metsulfuron‐methyl is a low‐application‐rate sulfonylurea herbicide that is widely used to control broad‐leaved weeds in wheat. Owing to its persistent nature, its residues may be present at phytotoxic levels for the next crop in rotation. Therefore, a comparative evaluation of HPLC and bioassay techniques was made for the analysis of this herbicide in wheat field soil. RESULTS: Metsulfuron‐methyl was applied to wheat crop at different rates (4, 8 and 12 AI ha^?1) at 28 days after sowing as a post‐emergence application, and the soil was analysed for metsulfuron‐methyl residues by HPLC and lentil seed bioassay techniques. The bioassay was found to be the more sensitive technique. At the recommended rate of application, 4 g AI ha^?1, the bioassay technique could detect the residue up to 30 days in surface soil, while, with HPLC, residues were not detectable on the 15th day. The half‐lives of metsulfuron‐methyl by HPLC and bioassay were calculated as 6.3–7.8 and 17.5 days respectively. Under field conditions, residues of metsulfuron‐methyl were also detected in subsurface soil by the bioassay technique at trace levels, but were not detected by the solvent extraction/HPLC method. CONCLUSION: Lentil seed bioassay is a more sensitive technique than HPLC. Traces of residues detected in subsurface soil indicated the mobility of metsulfuron‐methyl into lower layers. Copyright © 2009 Society of Chemical Industry     

Hydrolysis and photolysis of flumioxazin in aqueous buffer solutions

To determine the degradation rates and degradation products of the herbicide flumioxazin in aqueous buffer solutions (pH 5, 7 and 9), its hydrolysis and photolysis were investigated at 30 degrees C in the dark, and in a growth chamber fitted with fluorescent lamps simulating the UV output of sunlight. The rate of hydrolysis of flumioxazin was accelerated by increasing pH. The t(1/2) values at pH 5, 7 and 9 were 16.4, 9.1 and 0.25 h, respectively. Two degradation products were detected and their structural assignments were made on the basis of LC-MS data. Degradation product I was detected in all buffer solutions while degradation product II was detected in acidic buffer only. Both degradation products appeared to be stable to further hydrolysis. After correcting for the effects of hydrolysis, the photolytic degradation rate also increased as a function of pH and was approximately 10 times higher at pH 7 than that at pH 5, showing t(1/2) values of 4.9 and 41.5 h, respectively. Degradation products formed by photolysis were the same as those formed by hydrolysis. Flumioxazin was degraded more extensively at high pH and should degrade in surface water.     

Degradation of the sulfonylurea herbicides chlorsulfuron and triasulfuron in a high-organic-matter volcanic soil

The degradation rates of two sulfonylurea herbicides, chlorsulfuron and triasulfuron, were determined at two application rates, 15 and 30 g a.i. ha^–1, in a sandy loam soil of volcanic origin under controlled environment and field conditions. Residues were measured using a modified gas chromatographic (gc) determination method. Both herbicides degraded rapidly in the acidic soil (pH 5.7) with high organic matter levels (7.3% o.m.), generally according to first-order rate kinetics. The respective half-lives ranged from 22 to 38 d for chlorsulfuron and from 31 to 44 d for triasulfuron under five controlled temperature/soil moisture regimens, ranging from 10 to 30 °C and between 40% and 80% maximum water-holding capacity. Half-lives in the field were considerably shorter (13 d for chlorsulfuron and 12–13 d for triasulfuron). The degradation rates of the herbicides were influenced more by soil temperature than by soil moisture content. Bioassays using white mustard ( Sinapis alba L.) and forage sorghum [ Sorghum bicolor (L.) Moench] were also used to determine the persistence of phytotoxic residues of both herbicides in the field, and the results showed that the effects of chlorsulfuron disappeared within 8 weeks. Triasulfuron residues disappeared within 9 and 14 weeks for the 15 and 30 g a.i. ha^–1 rates respectively.     

Fate of chlorsulfuron in the environment. 1. Laboratory evaluations

The behaviour and fate of chlorsulfuron in aqueous and soil systems were examined in laboratory studies. Aqueous hydrolysis was pH-dependent and followed pseudo-first-order degradation kinetics at 25°C, with faster hydrolysis occurring at pH 5 (half-life 24 days) than at either pH 7 or 9 (half-lives >365 days). Degradation occurred primarily by cleavage of the sulfonylurea bridge to form the major metabolites chlorobenzenesulfonamide (2-chlorobenzenesulfonamide) and triazine amine (4-methoxy-6-methyl-1,3,5-triazin-2-amine). This route is a major degradation pathway in water and soil systems. Aqueous photolysis (corrected for hydrolysis) proceeded much more slowly (half-life 198 days) than aqueous hydrolysis and is not expected to contribute significantly to overall degradation. Hydrolysis in soil thin-layer plates exposed to light (half-life 80 days), however, progressed at a much faster rate than in dark controls (half life 130 days), which suggests that a mechanism other than direct photolysis may have been operative. An aerobic soil metabolism study (25°C) in a Keyport silt loam soil (pH 6·4, 2·8% OM) showed that degradation was rapid (half-life 20 days). Dissipation in an anaerobic sediment/water system (initial pH of water phase 6·7, final pH 7·4) progressed much more slowly (half-life >365 days) than in aerobic soil systems. Major degradation products in aerobic soil included the chlorobenzenesulfonamide and triazine amine as in the aqueous hydrolysis study. Neither of these degradation products exhibited phytotoxicity to a variety of crop and weed species in a glasshouse experiment, and both exhibited an acute toxicological profile similar to that of chlorsulfuron in a battery of standard tests. Demethylation of the 4-methoxy group on the triazine moiety and subsequent cleavage of the triazine ring is another pathway found in both aqueous solution and soils, though different bonds on the triazine amine appear to be cleaved in the two systems. Hydroxylation of the benzenesulfonamide moiety is a minor degradation pathway found in soils. Two soils amended with 0·1 and 1·0 mg kg^-1 chlorsulfuron showed slight stimulation of nitrification. The 1·0 mg kg^-1 concentration of chlorsulfuron resulted in minor stimulation and inhibition of ¹⁴C-cellulose and ¹⁴C-protein degradation, respectively, in the same soils. Batch equilibrium adsorption studies conducted on four soils showed that adsorption was low in this system (K_oc 13–54). Soil thin-layer chromatography of chlorsulfuron (R_f=0·55–0·86) and its major degradation products demonstrated that the chlorobenzenesulfonamide (R_f=0·34–0·68) had slightly less mobility and that the triazine amine (R_f=0·035–0·40) was much less mobile than chlorsulfuron. In an aged column leaching study, subsamples of a Fallsington sandy loam (pH_water 5·6, OM 1·4%) or a Flanagan silt loam (pH_water 6·4, OM 4·0%) were treated with chlorsulfuron, aged moist for 30 days in a glasshouse and then placed upon a prewet column of the same soil type prior to initiation of leaching. This treatment resulted in the retention of much more total radioactivity (including degradation products) than by a prewet column, where initiation of leaching began immediately after chlorsulfuron application, without aging (primarily chlorsulfuron parent). © 1998 SCI     

不同季节强碱土土壤呼吸影响因子分析与模型预测

利用LI-8100土壤碳通量测量仪测定了春夏秋三季晴朗天气下强碱土土壤呼吸速率、温度(气温和地温)、湿度(空气相对湿度和土壤湿度)数据,分析了它们之间的相关关系,获得不同季节对土壤呼吸影响较大的因子,并建立不同类别的多种回归模型;在精度检验及简单易行原则基础上,得到各季节土壤呼吸预测的最优模型。结果表明:(1)虽然温湿度均是影响不同季节强碱土土壤呼吸的主要因素,但均以温度的影响较大,其中气温是春秋两季土壤呼吸的最大直接影响因子,地温是夏季的最大直接影响因子,而土壤湿度为各季节最大的间接影响因子。(2)春秋季土壤呼吸的最佳预测模型均为10 cm处气温和土壤湿度所建的双因子方程,该方程具有较小的均方根误差(RMSE)(分别为0.159和0.259),且相对分析误差(RPD)2(分别为2.9、2.094),具有非常好的预测能力。夏季土壤呼吸最佳预测模型则为包含10 cm处气温、地温、空气相对湿度和土壤湿度所建的4因子方程,RMSE为0.248,RPD2(为2.406),可用于精确预测。(3)各季节土壤呼吸变化趋势与其影响因子的变化,因春季的完全同步,夏季基本一致,而秋季一致性较差,故春季土壤呼吸最佳预测模型的预测精度最高(92.67%),夏季次之(84.99%),秋季较差(77.23%)。     

碱化土壤油用向日葵养分吸收、运转特点的研究

为探明在盐碱胁迫条件下氮磷钾养分在油用向日葵植株体内的动态变化特点、各器官中运转与分布等,采用土壤测试与大田试验相结合的方法,研究了宁夏前进农场碱化土壤油用向日葵氮磷钾养分吸收、运转特点。研究结果表明,无论施肥与否,油用向日葵地上部氮磷钾含量变化随着生育期的推移变化呈现反"S"曲线降低趋势。碱化土壤油用向日葵各器官氮磷钾含量动态变化因施肥水平和生育期不同表现出不同的变化趋势。无论施肥与否油用葵整个生育期各器官中总吸氮量依次为:叶>盘>茎>根>籽;吸磷量依次为:盘>茎>叶>籽>根;吸钾量依次为:茎>盘>叶>根>籽。     

Effects of fencing on vegetation and soil restoration in a degraded alkaline grassland in northeast China

In order to restore a degraded alkaline grassland, the local government implemented a large restoration project using fences in Changling county, Jilin province, China, in 2000. Grazing was excluded from the protected area, whereas the grazed area was continuously grazed at 8.5 dry sheep equivalent（DSE）/hm2. In the current research, soil and plant samples were taken from grazed and fenced areas to examine changes in vegetation and soil properties in 2005, 2006 and 2008. Results showed that vegetation characteristics and soil properties improved significantly in the fenced area compared with the grazed area. In the protected area the vegetation cover, height and above- and belowground biomass increased significantly. Soil pH, electrical conductivity and bulk density decreased significantly, but soil organic carbon and total nitrogen concentration increased greatly in the protected area. By comparing the vegetation and soil characteristics with pre-degraded grassland, we found that vegetation can recover 6 years after fencing, and soil pH can be restored 8 years after fencing. However, the restoration of soil organic carbon, total nitrogen and total phosphorus concentrations needed 16, 30 and 19 years, respectively. It is recommended that the stocking rate should be reduced to 1/3 of the current carrying capacity, or that a grazing regime of 1-year of grazing followed by a 2-year rest is adopted to sustain the current status of vegetation and soil resources. However, if N fertilizer is applied, the rest period could be shortened, depending on the rate of application.     

Resistance levels of sulfonylurea‐resistant Schoenoplectus juncoides (Roxb.) Palla with various Pro197 mutations in acetolactate synthase to imazosulfuron,bensulfuron‐methyl,metsulfuron‐methyl and imazaquin‐ammonium

An investigation, using herbicidal pot tests in a greenhouse condition, was conducted to determine the whole‐plant dose–response relationships to several acetolactate synthase (ALS)‐inhibiting herbicides of sulfonylurea (SU)‐resistant Schoenoplectus juncoides with various Pro₁₉₇ mutations in ALS that was collected from Japanese rice paddy fields. All the tested SU‐resistant accessions with a Pro₁₉₇ mutation were highly resistant to two commonly used SU herbicides (imazosulfuron and bensulfuron‐methyl), but were much less resistant to another SU herbicide, metsulfuron‐methyl, and were substantially not resistant to imazaquin‐ammonium. These cross‐resistance patterns have been known previously in fragments of S. juncoides and other weed species and were comprehensively confirmed in this study with a whole set of Pro₁₉₇ mutations. The analyses of resistance levels, based on ED₉₀ values, newly showed that different accessions with a common amino acid substitution in ALS1 showed similar responses to these herbicides (confirmed with four amino acid substitutions), that the rankings of resistance levels that were conferred by various Pro₁₉₇ mutations in ALS1 differed among the SU herbicides and that the resistance levels of the ALS2‐mutated accessions were higher than, lower than or similar to those of the corresponding ALS1‐mutated accessions, depending on the compared pair, but the deviation patterns were generally similar among the SU herbicides in each compared pair. The final finding might suggest that the abundance of ALS2 is not as stable as that of ALS1. In addition, as a result of these new findings, together with expected further research, a suggested possibility is that substituting amino acids at Pro₁₉₇ generally could be estimated by plotting each accession's ED₉₀ values of imazosulfuron and bensulfuron‐methyl in a two‐dimensional graph.     

三江平原小叶章湿地土壤中碱解氮和全氮含量的季节变化特征

选择三江平原典型小叶章湿地不同水分带上的两种土壤类型(草甸沼泽土和腐殖质沼泽土)为研究对象,对比研究了二者碱解氮(K-N)和全氮(TN)含量的季节变化特征。结果表明:二者不同土层K-N和TN含量的季节变化特征差异较大,前者0-50 cm土层K-N含量以及0-40 cm土层TN含量的变化最为显著,而后者K-N和TN含量的显著变化仅集中在0-20 cm土层;二者不同土层K-N和TN含量的季节变化与不同生长期植物吸收作用、水分条件、降水、有机氮矿化和硝化-反硝化作用等因素有关。TN含量的季节变化还取决于不同时期根际分泌物的产生量以及枯落物分解与有机氮的矿化平衡;尽管K-N和TN含量的季节变化特征在两种土壤不同土层间差别较大,但均可用四次多项式进行模拟,模拟效果比较理想,基本可反映二者K-N和TN含量的季节变化特征。     

土壤中砜嘧磺隆和氯磺隆残留的光化学荧光分析方法研究

用紫外线照射非荧光特性的砜嘧磺隆和氯磺隆,通过生成具有荧光特性的衍生物,分别研究了其在不同介质中的荧光特性及其影响因子,建立了测定土壤中砜嘧磺隆和氯磺隆残留的光化学荧光分析法(PCF)。结果表明:在2×10-3 mol/L、一定酸碱度(砜嘧磺隆pH 7、氯磺隆pH 12)的十六烷基三甲基氯化铵(CTAC)胶体分散体系中,紫外照射150 s是PCF法测定砜嘧磺 隆和氯磺隆残留的最佳条件,在此条件下砜嘧磺隆和氯磺隆的检出限(LOD)分别为0.7和0.6 μg/kg, 相对标准偏差(RSD)分别为1.7%和2.1%;在黄松田水稻土、黄红壤性水稻土和青紫泥田水稻土3种不同性质的土壤中,砜嘧磺隆和氯磺隆同时测定的平均回收率分别为99.0%±1.0%和98.7%±4.1%、97.6%±1.7%和97.0%±4.7%、96.7 %±2.3%和95.4%±5.5%;所建立的PCF法可有效、快速测定土壤中同时残留的微量砜嘧磺隆和氯磺隆。     

Effect of soil physical factors on methyl iodide and methyl bromide

Production and importation of methyl bromide is scheduled to be banned by 2001. Methyl iodide was evaluated as a possible replacement soil fumigant. The effects of soil moisture, temperature, soil texture and fumigation time on the efficacy of methyl iodide for the control of two common weeds, Abutilon theophrasti and Lolium multiflorum, were characterized and compared with those of methyl bromide. The optimal soil moisture for methyl iodide to kill both weed species in sandy soils was 14% water content (w/w). Greater efficacy was obtained when the temperature during fumigation was above 20°C. Compared to methyl bromide, the efficacy of methyl iodide was more consistent in different soils. Time to 100% mortality of weeds was 24 h for methyl iodide fumigation and 36 h for methyl bromide when 200 μM of fumigant was used. On a molar basis methyl iodide was consistently more effective than methyl bromide across the range of environmental factors tested. In terms of application technology and spectrum of activity, methyl bromide can be directly replaced by methyl iodide. © 1998 SCI     

A simulation model for fate and transport of methyl bromide during fumigation in plastic‐mulched vegetable soil beds

A coupled water‐heat and chemical transport model was used to describe the fate and transport of methyl bromide fumigant in low‐density polyethylene plastic‐mulched soil beds used for vegetable production. Methyl bromide transport was described by convective‐dispersive processes including transformations through hydrolysis. Effects of non‐isothermal conditions on chemical transport were considered through inclusion of temperature effects on transport parameters. An energy‐balance approach was used to describe the plastic‐mulched boundary condition that controls the thermal regime within the soil bed. Simulations were made for variable water‐saturation regimes within the bed and for different depths of fumigant injection. Simulations for various scenarios revealed that large amounts (20–44% over a 7‐day period) of applied methyl bromide are lost from the un‐mulched furrows between the beds. Plastic mulching of the bed was found to be only partially effective (11–29% emission losses over a 7‐day period) in reducing atmospheric emissions. Deep injection of fumigant and saturating the soil with water both led to increased retention of methyl bromide within the soil and less emission to the atmosphere. However, deep injection was unfavorable for effective sterilization of the crop root zone. © 2000 Society of Chemical Industry     

Sorption–desorption of 'aged' isoxaflutole and diketonitrile degradate in soil

Isoxaflutole is a relatively new herbicide used for weed control in maize. The objective of this research was to increase the understanding of the behaviour and environmental fate of isoxaflutole and its diketonitrile (DKN) degradate in soil, including determination of the strength of sorption to soil and whether sorption is affected by ageing. In sandy loam (SL) and silty clay (SiCl) soils, ¹⁴C‐isoxaflutole was found to dissipate rapidly after application to soil; recovery ranged from ～42% to 68% at week 0, and recovery had decreased to <10% at week 12. Decreases in ¹⁴C isoxaflutole residues over time in SL and SiCl soils are consistent with hydrolysis of isoxaflutole and formation of bound DKN residues in the soil. DKN recovery from freshly treated SiCl and SL soils was 41% to 52%. After a 12‐week incubation in SL soil at pH 7.1 and 8.0, recoveries were similar, ～40%. However, at week 12 in SL soil pH 5.7, DKN recovery decreased to ～28%. DKN recovery in SiCl soil at week 12 was <10%. Increases in sorption of DKN in SL at pH 5.7 and SiCl soil over time indicate that the DKN degradate is tightly bound to the soil and sorption is affected by soil pH and soil type. Sorption of ¹⁴C‐DKN in the SiCl soil more than doubled with ageing compared with the lower K_d sorption coefficient values of the SL soils. In the SiCl soil at time 0, the K_d was 0.6; at 1 week, K_d increased to 2; and at the end of the 12‐week incubation period, K_d was 4.5. This strong binding of DKN to the soil may be due to chelate formation in the interlayer of the clay.     

屠宰场废弃物堆肥对苜蓿生长和碱化土壤肥力指标的影响

对屠宰场猪、牛、羊废弃物堆肥施入退化土壤后作物生理指标、土壤肥力指标和微生物区系变化进行系统研究。结果表明：施用废弃物堆肥明显提高了苜蓿出苗率,并缩短了出苗时间,但不同种类、不同施用量（22．5 t·hm－2、30．0 t·hm－2和37．5 t·hm－2）废弃物提高的幅度不同。苜蓿鲜生物量随着废弃物施用量的增大而增加,其中羊废弃物施用量为37．5 t· hm－2的处理最大,为11．95 g · plant－1,不施用废弃物的处理鲜生物量最小,其最大值为10．26 g·plant－1;施用猪废弃物30．0 t·hm－2的处理其干生物量最高（3．91 g·plant－1）。施用屠宰场废弃物堆肥后土壤有机质及养分都有不同程度的增加,如10月中旬土壤有机质和速效钾含量增幅略低,分别为9．92％～27．12％和5．77％～34．03％,碱解氮和速效磷增幅分别为11．79％～47．66％和16．92％～44．97％。猪废弃物施用量为37．5 t·hm－2的处理细菌数量在8月底达到3．98×107 cfu·g－1,羊和牛废弃物相同时期相同用量条件下细菌数量相近,一般废弃物施用量越大土壤中细菌、真菌和放线菌数量也越多。     

脱硫石膏施用时期和深度对改良碱化土壤效果的影响

选择宁夏西大滩碱化土壤,以油葵为供试作物,采用两因素随机区组设计,进行脱硫石膏改良碱化土壤的田间试验研究.结果表明,脱硫石膏施用时期和施用深度不同,对改良土壤碱性和促进作物生长发育的效果不同.秋季施用较春季施用油葵出苗率提高38.0%,产量提高39.0%;深施(25 cm)脱硫石膏较浅施(10 cm)油葵出苗率提高6.3%,产量提高6.0%.秋季深施较秋季浅施、春季深施、春季浅施油葵出苗率分别提高12.0%、25.6%、21.5%,产量分别提高14.4%、32.7%、29.9%,表明秋季深施较秋季浅施、春季深施及春季浅施对促进油葵生长发育,提高产量效果更显著.     

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%。