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1.
神东矿区复垦地土壤酶活性变化和分布特征 总被引：3，自引：0，他引：3
土壤酶活性可用于衡量土壤养分供应能力及土壤质量,而其季节变化可反映养分供应与植物需求的耦合关系。以马家塔矿复垦地为研究对象,对不同植物群落下土壤酶活性的季节变化进行了监测,结果表明:复垦土壤的表层过氧化氢酶、脲酶、磷酸酶和蔗糖酶活性均显著高于下层和对照的原状土壤,说明复垦可以提高土壤的酶活性。不同植被下土壤的酶活性大小总体上以苜蓿、油蒿、桧柏和侧柏对土壤质量的贡献较大。4种酶活性的动态变化趋势基本相同,都表现为前期先增加,增加到最大值后又开始下降,总体上均以夏季(7-8月份)活性最高。酶活性的变化和大小可以体现有机质含量的变化和转化方向,也能体现基础氮素的变化方向,复垦后酶活性提高,但是和农田土壤相比还有一定差距,所以复垦工作还需继续开展。 相似文献
2.
FAJRI ANUGROHO MAKOTO KITOU FUJIO NAGUMO KAZUTOSHI KINJO YOSHIHIRO TOKASHIKI 《Weed Biology and Management》2009,9(2):129-136
Weeds emerge throughout the year in agricultural fields in subtropical regions. The weed suppression and improved soil fertility resulting from a living mulch of hairy vetch were investigated. Hairy vetch was sown in October and in December 2006. The fallow condition was without the sowing of hairy vetch, with the weeds allowed to grow naturally. The biomass of the top parts (BOT) of hairy vetch increased from February to April and then decreased in May on both sowing dates. The BOT of hairy vetch sown in October was significantly higher in February, March, and April than that sown in December. Hairy vetch sown in October and harvested from February to April varied from 372–403 × 10−3 kg m−2 , with weed suppression percentages of 62.8% in comparison with the fallow plots. The fixed C, N, P, and mineral uptake of hairy vetch showed similar patterns to its biomass. The nitrate (NO3 -N) content increased from February to May for the soils in the October and December plots, in contrast to the fallow plots. Moreover, the NO3 -N and available N of the October and December soils sampled from February to May were higher than that of the fallow soils. In subtropical agriculture, hairy vetch should be sown in October in order to achieve a higher biomass for suppressing weeds effectively and improving the soil fertility, mainly N. 相似文献
3.
银川平原不同类型盐渍化土壤酶活性及其与土壤养分间相关分析研究 总被引：5，自引：1，他引：4
为了研究银川平原不同类型及程度盐碱地土壤酶活性及其分布特征,文中采用高锰酸钾滴定法、硫代硫酸钠滴定法及比色测定法和相关分析法研究了银川平原不同类型及盐渍化不同程度土壤酶活性及其与土壤养分间的相关关系。结果表明:随着碱化土壤pH值和盐化土壤全盐含量的增加,土壤过氧化氢酶、转化酶、碱性磷酸酶和脲酶活性均呈现逐渐降低的趋势(p<0.01)。土壤碱性磷酸酶活性表现为碱化土壤显著高于盐化土壤,过氧化氢酶、转化酶和脲酶活性在不同类型土壤间差异不显著。0-20cm深度土壤酶活性表现出明显的季节变化,碱化土壤碱性磷酸酶活性、盐化土壤过氧化氢酶活性表现8月>6月>9月;碱化盐化土壤转化酶活性、碱化土壤脲酶活性、盐化土壤碱性磷酸酶活性季节变化表现为随着取样时间的推移而逐渐增加,即9月>8月>6月。碱化、盐化土壤过氧化氢酶、转化酶、碱性磷酸酶和脲酶活性之间及其与土壤有机质、全氮、全磷、有效磷、全钾、碱解氮、速效钾含量之间有很好的正相关关系。 相似文献
4.
ZongQiang CHANG XiaoQing LIU Qi FENG ZongXi CHE HaiYang XI YongHong SU JianHua SI 《干旱区科学》2013,(4):488-499
Most soil respiration measurements are conducted during the growing season.In tundra and boreal forest ecosystems,cumulative,non-growing season soil CO2 fluxes are reported to be a significant component of these systems' annual carbon budgets.However,little information exists on soil CO2 efflux during the non-growing season from alpine ecosystems.Therefore,comparing measurements of soil respiration taken annually versus during the growing season will improve the accuracy of estimating ecosystem carbon budgets,as well as predicting the response of soil CO2 efflux to climate changes.In this study,we measured soil CO2 efflux and its spatial and temporal changes for different altitudes during the non-growing season in an alpine meadow located in the Qilian Mountains,Northwest ChinaField experiments on the soil CO2 efflux of alpine meadow from the Qilian Mountains were conducted along an elevation gradient from October 2010 to April 2011.We measured the soil CO2 efflux,and analyzed the effects of soil water content and soil temperature on this measure.The results show that soil CO2 efflux gradually decreased along the elevation gradient during the non-growing season.The daily variation of soil CO2 efflux appeared as a single-peak curve.The soil CO2 efflux was low at night,with the lowest value occurring between 02:00-06:00.Then,values started to rise rapidly between 07:00-08:30,and then descend again between 16:00-18:30.The peak soil CO2 efflux appeared from 11:00 to 16:00.The soil CO2 efflux values gradually decreased from October to February of the next year and started to increase in March.Non-growing season Q10(the multiplier to the respiration rate for a 10℃ increase in temperature) was increased with raising altitude and average Q10 of the Qilian Mountains was generally higher than the average growing season Q10 of the Heihe River Basin.Seasonally,non-growing season soil CO2 efflux was relatively high in October and early spring and low in the winter.The soil CO2 efflux was positively correlated with soil temperature and soil water content.Our results indicate that in alpine ecosystems,soil CO2 efflux continues throughout the non-growing season,and soil respiration is an important component of annual soil CO2 efflux. 相似文献
5.
In order to investigate the spatio-temporal variability of soil water content to rainfall under Caragana microphylla shrub in Horqin Sandy Land,a plot of 25 m × 25 m,where there were 6 shrub canopies of C. microphylla,was sited for measuring soil water content at two soil layers of 0-20 cm (top layer) and 20-40 cm (lower layer). Soil water content was measured on the 1st,5th,10th and 15th day after a 42 mm rainfall in Naiman of Inner Mongolia. The results showed that soil water contents at both layers under C. microphylla shrub were gradually decreased after the rain. Soil water content at the top layer outside the shrub canopy was higher than that inside the shrub canopy within 5 days,and became similar inside and outside the shrub canopy on the 10th day after the 42 mm rainfall,and it was lower outside than that inside the shrub canopy on the 15th day. The soil water content at lower layer in the area without shrubs was higher than that under shrub canopy all along. All the measured values of soil water content can be fitted to a variogram model. There was significant autocorrelation of the values of soil water content between top layer and lower layer,except for the fourth measured values of soil water content at top layer. The range and spatial dependence of soil water content at top layer were lower than that at lower layer. 相似文献
6.
实验旨在研究不同种植模式、作物种间不同的根部隔离处理对线辣椒根际与非根际土壤微生物数量、土壤酶活性及土壤养分有效含量的影响。结果表明：套作栽培的线辣椒根际、非根际土壤微生物数量、酶活性均高于单作栽培。与膜隔处理相比,网隔与无隔处理的根际、非根际土壤微生物数量及酶活性均有提高,其中以网隔处理最高。各处理根际土壤有机质、有效磷、有效钾含量均低于非根际土壤,但碱解氮含量表现为根际土壤高于非根际土壤。网隔处理中尼龙网减缓了玉米根系对线辣椒根系营养的直接竞争,同时玉米根系根际效应使其根际、非根际土壤养分含量在所有处理中最高。土壤微生物主要类群数量是影响土壤酶活性主要因子,与土壤酶活性显著相关。有机质、碱解氮含量与土壤酶活性、微生物数量呈极显著相关,有效磷含量与土壤酶活性、微生物数量呈正相关。土壤真菌数量、脲酶活性与有效钾含量呈负相关。 相似文献
7.
榆林沙区樟子松林土壤酶活性与土壤化学性质的通径分析 总被引：3，自引：0，他引：3
应用通径分析探讨榆林沙区樟子松林地5种土壤化学因子对4种土壤酶活性的影响程度。结果表明:随着林龄增加,土壤酶活性不断增加,土壤化学性质多呈波动性增加的趋势;碱解氮和速效磷是影响蔗糖酶和碱性磷酸酶活性的主要因子,而有机质主要通过强烈的间接作用影响两种酶活性的变化;有机质和碱解氮是影响过氧化氢酶活性的主要因子;pH和速效钾对4种酶活性影响力较小;5种化学因子对脲酶活性的直接效应多与间接效应抵消。与简单相关分析相比,通径分析能更深入地揭示土壤化学性质对酶活性的影响程度。 相似文献
8.
玉米线辣椒套作对线辣椒根际、非根际土壤微生物、酶活性和土壤养分的影响 总被引：6，自引：0，他引：6
实验旨在研究不同种植模式、作物种间不同的根部隔离处理对线辣椒根际与非根际土壤微生物数量、土壤酶活性及土壤养分有效含量的影响.结果表明:套作栽培的线辣椒根际、非根际土壤微生物数量、酶活性均高于单作栽培.与膜隔处理相比,网隔与无隔处理的根际、非根际土壤微生物数量及酶活性均有提高,其中以网隔处理最高.各处理根际土壤有机质、有效磷、有效钾含量均低于非根际土壤,但碱解氮含量表现为根际土壤高于非根际土壤.网隔处理中尼龙网减缓了玉米根系对线辣椒根系营养的直接竞争,同时玉米根系根际效应使其根际、非根际土壤养分含量在所有处理中最高.土壤微生物主要类群数量是影响土壤酶活性主要因子,与土壤酶活性显著相关.有机质、碱解氮含量与土壤酶活性、微生物数量呈极显著相关,有效磷含量与土壤酶活性、微生物数量呈正相关.土壤真菌数量、脲酶活性与有效钾含量呈负相关. 相似文献
9.
Soil salinization has adverse effects on the soil physical-chemical characteristics.However,little is known about the changes in soil salt ion concentrations and other soil physical-chemical characteristics within the Qarhan Salt Lake and at different soil depths in the surrounding areas.Here,we selected five sampling sites(S1,S2,S3,S4,and S5)alongside the Qarhan Salt Lake and in the Xidatan segment of the Kunlun Mountains to investigate the relationship among soil salt ion concentrations,soil physical-chemical characteristics,and environmental variables in April 2019.The results indicated that most sites had strongly saline and very strongly saline conditions.The main salt ions present in the soil were Na+,K+,and Cl-.Soil nutrients and soil microbial biomass(SMB)were significantly affected by the salinity(P<0.05).Moreover,soil salt ions(Na+,K+,Ca2+,Mg2+,Cl-,CO32-,SO42-,and HCO3-)were positively correlated with electrical conductivity(EC)and soil water content(SWC),but negatively related to altitude and soil depth.Unlike soil salt ions,soil nutrients and SMB were positively correlated with altitude,but negatively related to EC and SWC.Moreover,soil nutrients and SMB were negatively correlated with soil salt ions.In conclusion,soil nutrients and SMB were mainly influenced by salinity,and were related to altitude,soil depth,and SWC in the areas from the Qarhan Salt Lake to the Xidatan segment.These results imply that the soil quality(mainly evaluated by soil physical-chemical characteristics)is mainly influenced by soil salt ions in the areas surrounding the Qarhan Salt Lake.Our results provide an accurate prediction of how the soil salt ions,soil nutrients,and SMB respond to the changes along a salt gradient.The underlying mechanisms controlling the soil salt ion distribution,soil nutrients,and SMB in an extremely arid desert climate playa should be studied in greater detail in the future. 相似文献
10.
对干旱地区的红富士苹果园土壤中施沼肥定位试验施肥后收获期土壤主要土壤酶种类及活性进行分析结果表明:施沼肥土壤中主要存在脲酶、磷酸酶、过氧化氢酶和蔗糖酶等4种土壤酶,它们的酶活性存在差异,施工程沼肥果园中除蔗糖酶外其余酶活性均高于施户用沼肥果园.对土壤酶和土壤养分进行相关分析、通径分析、主成分分析结果表明,施户用沼肥果园的脲酶、过氧化氢酶和蔗糖酶和施工程沼肥果园的蔗糖酶都可以作为土壤肥力的指标,且酶活性大小受到土壤化学性质和其它酶活性影响.土壤主成分分析能较为客观地评价土壤肥力水平. 相似文献
11.
ZhengJun GUAN Qian LUO Xi CHEN XianWei FENG ZhiXi TANG Wei WEI YuanRun ZHENG 《干旱区科学》2014,(2):164-173
Soil enzyme activity plays an important role in the conversion of soil organic carbon into inorganic carbon,which is significant for the global carbon cycle.In this study,we investigated the soil enzyme activities of two ligninolytic enzymes(peroxidase and polyphenol oxidase)and five non-ligninolytic enzymes(α-1,4-glucosidase(AG);β-1,4-glucosidase(BG);N-acetyl-β-glucosaminidase(NAG);β-D-cellobiosidase(CBH);andβ-xylosidase(BXYL))in four plant communities of the Sangong River basin in Fukang,North Xinjiang,China.The four typical plant communities were dominated by Haloxylon ammodendron,Reaumuria soongonica,Salsola passerina,and Tamarix rarmosissima,respectively,with saline soils of varied alkalinity.The results showed that the soil peroxidase activity decreased seasonally.The activities of the five non-ligninolytic enzymes decreased with increasing soil depths,while those of the two ligninolytic enzymes did not show such a trend.In the four plant communities,BG had the highest activity among the five non-ligninolytic enzymes,and the activities of the two ligninolytic enzymes were higher than those of the four non-ligninolytic ones(AG,NAG,CBH,and BXYL).The community of H.ammodendron displayed the highest activity with respect to the two ligninolytic enzymes in most cases,but no significant differences were found among the four plant communities.The geometric mean of soil enzyme activities of the four plant communities was validated through an independently performed principal component analysis(PCA),which indicated that different plant communities had different soil enzyme activities.The correlation analysis showed that soil polyphenol oxidase activity was significantly positively correlated with the activities of the five non-ligninolytic enzymes.The soil pH value was positively correlated with the activities of all soil enzymes except peroxidase.Soil microbial carbon content also showed a significant positive correlation(P0.01)with the activities of all soil enzymes except polyphenol oxidase.The results suggested that the H.ammodendron community has the highest ability to utilize soil organic carbon,and glucoside could be the most extensively utilized non-ligninolytic carbon source in the saline soil of arid areas in Xinjiang. 相似文献
12.
施用生物炭后土壤生物活性与土壤肥力的关系 总被引：4，自引：0，他引：4
分析了生物炭不同用量条件下土生物活性与土壤主要肥力指标之间的关系。相关分析表明,除蔗糖酶活性和微生物量碳外,土壤其它生物活性指标与土壤容重间呈显著负相关。土壤脲酶和过氧化氢酶活性、微生物量氮和三大类微生物与土壤主要肥力指标间呈显著或极显著正相关。除蔗糖酶外,酶活性与三类微生物数量间显著相关,但蔗糖酶、土壤脲酶、碱性磷酸酶、过氧化氢酶的活性间并不完全显著相关。通径分析表明,脲酶和微生物量氮对土壤肥力影响以直接作用为主,而过氧化氢酶则以间接作用为主。主成分分析结果表明,可以用微生物因子、酶活性因子和速效磷因子进行综合描述土壤肥力特征。其中,各处理综合得分在玉米季大于小麦季,且随生物炭用量的增加而增加,表明高用量生物炭对土壤肥力的提高作用明显。 相似文献
13.
不同轮作方式对马铃薯土壤酶活性及微生物数量的影响 总被引：5，自引：0，他引：5
在连续种植2年马铃薯的土壤上进行不同轮作方式田间试验,探讨轮作方式对马铃薯土壤酶活性及土壤微生物数量的影响。试验结果表明:与对照(裸地)相比,小麦-豌豆-马铃薯轮作时土壤过氧化氢酶活性有增加的趋势;豌豆-马铃薯-豌豆轮作条件下,土壤的蔗糖酶活性提高,且在马铃薯成熟期提高幅度最大,为47.95%。轮作条件下土壤多酚氧化酶活性低于连作;轮作方式不同,土壤脲酶活性变化明显,在马铃薯块茎膨大期,豌豆-马铃薯-豌豆轮作方式的土壤脲酶活性比小麦-马铃薯-小麦高14.73%。马铃薯块茎膨大期根区土壤微生物数量测定结果显示:随着连作年限的增加,细菌数量及微生物总量降低,真菌数量升高了54.66%;小麦-豌豆-马铃薯轮作后,土壤中的细菌、放线菌数量最高,分别为6.40×106CFU·g-1和2.22×106CFU·g-1。 相似文献
14.
15.
异噁草酮对土壤微生物和土壤酶活性的影响 总被引：2，自引：0，他引：2
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。 相似文献
16.
Ecological restoration by Tamarix plants on semi-arid saline lands affects the accumulation, distribution patterns and related mechanisms of soil water content and salinity. In this study, spatio-temporal variations of soil water content and salinity around natural individual Tamarix ramosissima Ledeb. were invetigated in a semi-arid saline region of the upper Yellow River, Northwest China. Specifically, soil water content, electrical conductivity(EC_e), sodium adsorption ratio(SAR_e), and salt ions(including Na~+, K~+, Ca~(2+), Mg~(2+) and SO_4~(2–)) were measured at different soil depths and at different distances from the trunk of T. ramosissima in May, July, and September 2016. The soil water content at the 20–80 cm depth was significantly lower in July and September than in May, indicating that T. ramosissima plants absorb a large amount of water through the roots during the growing period, leading to the decreasing of soil water content in the deep soil layer. At the 0–20 cm depth, there was a salt island effect around individual T. ramosissima, and the EC_e differed significantly inside and outside the canopy of T. ramosissima in May and July. Salt bioaccumulation and stemflow were two major contributing factors to this difference. The SAR_e at the 0–20 cm depth was significantly different inside and outside the canopy of T. ramosissima in the three sampling months. The values of SAR_e at the 60–80 cm depth in May and July were significantly higher than those at the 0–60 cm depth and higher than that at the corresponding depth in September. The distribution of Na~+ in the soil was similar to that of the SAR_e, while the concentrations of K~+, Ca~(2+), and Mg~(2+) showed significant differences among the sampling months and soil depths. Both season and soil depth had highly significant effects on soil water content, EC_e and SAR_e, whereas distance from the trunk of T. ramosissima only significantly affected EC_e. Based on these results, we recommend co-planting of shallow-rooted salt-tolerant species near the Tamarix plants and avoiding planting herbaceous plants inside the canopy of T. ramosissima for afforestation in this semi-arid saline region. The results of this study may provide a reference for appropriate restoration in the semi-arid saline regions of the upper Yellow River. 相似文献
17.
贺兰山西坡不同类型草地土壤酶活性特征 总被引：3，自引：0，他引：3
以阿拉善左旗境内贺兰山中段（西坡）山前地带的主要草地类型为对象,分析不同类型草地土壤酶活性的分布特征,及其与气候、植被和土壤等环境因子的关系。结果表明：① 随着海拔高度的降低,土壤脲酶、蔗糖酶、碱性磷酸酶和过氧化氢酶活性表现为：高山草甸＞山地草原＞山地荒漠草原＞草原化荒漠,且在0～10 cm土层的差异尤其显著;② 各类草地土壤酶活性均沿土壤垂直剖面依次降低,差异呈显著性水平;③ 偏相关及逐步回归分析表明,影响该区草地土壤脲酶和蔗糖酶活性最主要的因素为土壤微生物碳氮、有机碳和全氮,碱性磷酸酶主要受土壤微生物碳和全氮影响,对过氧化氢酶影响最大的因子为土壤微生物碳、pH、全氮和降水量。 相似文献
18.
Biological soil crusts(BSCs) are capable of modifying nutrient availability to favor the establishment of biogeochemical cycles. Microbial activities serve as critical roles for both carbon and nutrient transformation in BSCs. However, little is known about microbial activities and physical-chemical properties of BSCs in the Gurbantunggut Desert, Xinjiang, China. In the present research, a sampling line with 1-m wide and 20-m long was set up in each of five typical interdune areas selected randomly in the Gurbantunggut Desert. Within each sampling line, samples of bare sand sheet, algal crusts, lichen crusts and moss crusts were randomly collected at the depth of 0–2 cm. Variations of microalgal biomass, microbial biomass, enzyme activities and soil physical-chemical properties in different succession of BSCs were analyzed. The relationships between microalgal biomass, microbial biomass, enzymatic activities and soil physical-chemical properties were explored by stepwise regression. Our results indicate that microalgal biomass, microbial biomass and most of enzyme activities increased as the BSCs developed and their highest values occurred in lichen or moss crusts. Except for total K, the contents of most soil nutrients(organic C, total N, total P, available N, available P and available K) were the lowest in the bare sand sheet and significantly increased with the BSCs development, reaching their highest values in moss crusts. However, pH values significantly decreased as the BSCs developed. Significant and positive correlations were observed between chlorophyll a and microbial biomass C. Total P and N were positively associated with chlorophyll a and microbial biomass C, whereas there was a significant and negative correlation between microbial biomass and available P. The growth of cyanobacteria and microorganism contributed C and N in the soil, which offered substrates for enzyme activities thus increasing enzyme activities. Probably, improvement in enzyme activities increased soil fertility and promoted the growth of cyanobacteria, eukaryotic algae and heterotrophic microorganism, with the accelerating succession of BSCs. The present research found that microalgal-microbial biomass and enzyme activities played important roles on the contents of nutrients in the successional stages of BSCs and helped us to understand developmental mechanism in the succession of BSCs. 相似文献
19.
施用氮磷钾对黄土丘陵区山地红枣林土壤酶与土壤肥力的影响 总被引：8，自引：0，他引：8
采用野外试验与室内分析,研究了连续4 a施氮磷钾肥对黄土丘陵区山地枣园土壤酶活性及土壤养分含量的影响。结果表明:连续4 aNPK1施肥处理能够明显增强土壤脲酶、磷酸酶、过氧化氢酶和蔗糖酶的活性,提高土壤有机质、全氮、速效氮、速效磷和速效钾含量;在土壤剖面中总的趋势是土壤酶活性和土壤速效氮、速效磷和速效钾含量随土层深度加深而降低。土壤酶活性与土壤养分因子的相关分析表明,在0~20 cm土层,磷酸酶与有机质、速效磷,过氧化氢酶与有机质、全氮呈显著或极显著性正相关。在20~40 cm,脲酶与有机质、全氮、速效氮,磷酸酶与速效钾,过氧化氢酶与速效磷,蔗糖酶与有机质、速效钾呈显著或极显著性正相关。在40~60 cm,脲酶与全氮、速效磷,磷酸酶与有机质、速效氮,过氧化氢酶与速效磷,蔗糖酶与有机质、全氮、速效磷呈显著或极显著正相关。 相似文献
20.
为明确异噁唑草酮对玉米根际土壤微生物碳、氮及酶活性的影响, 采用田间试验的方法, 以1倍、5倍和10倍田间推荐剂量为供试除草剂剂量, 测定了异噁唑草酮土壤封闭处理对玉米根际土壤微生物量碳、氮及土壤脲酶、过氧化氢酶、蔗糖酶、脱氢酶和中性磷酸酶活性的影响。结果表明:推荐剂量的异噁唑草酮对玉米根际土壤微生物量碳、氮含量无显著影响, 5倍和10倍推荐剂量的异噁唑草酮对玉米根际土壤微生物量碳、氮含量具有抑制作用。推荐剂量的异噁唑草酮对玉米根际土壤脲酶、过氧化氢酶和蔗糖酶影响较小, 5倍和10倍推荐剂量的异噁唑草酮对其具有明显的抑制作用。异噁唑草酮对土壤脱氢酶活性具有抑制作用, 且施用剂量越高, 抑制作用越强。异噁唑草酮对土壤中性磷酸酶活性的影响表现为前期促进, 后期抑制, 且施用剂量越大, 促进或抑制作用越强。研究表明:推荐剂量的异噁唑草酮对玉米根际土壤微生物量碳、氮及土壤脲酶、过氧化氢酶和蔗糖酶活性的影响较小, 但对土壤脱氢酶、中性磷酸酶活性有影响。 相似文献