排序方式: 共有65条查询结果,搜索用时 31 毫秒
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Wu Yanyu 《环境科学学报(英文版)》1990,2(1):55-73
Soil background contents of a number of elements of different soil groups, sub-groups and genus on Liaohe River Plain were investigated. It appeared that: the background levels for most elements studied were around the lower limits of the world's averages, variation coefficients of the background content values were from 0.3-0.5 and the element migration coefficients were between 0.9 and 1.0. It was found that the element background contents in soils of eastern and southern parts of the area were generally higher than that of western and northern parts. 相似文献
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CompoundpollutionofCd,Pb,Cu,Zn,Asinplant-soilsystemanditsprevention¥WuYanyu;WangXin;LiYing(InstituteofAppliedEcology,ChineseA... 相似文献
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为了研究氮添加对森林土壤有机碳氮组分稳定性的影响,选取我国亚热带典型常绿阔叶林(浙江桂天然林和罗浮栲天然林)和针叶林(杉木人工林),开展为期5年的野外模拟氮沉降试验,分别设置对照〔0 kg/(hm2·a),以NH4NO3中的N计,下同〕、低氮〔75 kg/(hm2·a)〕和高氮〔150 kg/(hm2·a)〕3个氮添加水平,用H2SO4分2步酸水解获得LPⅠ(活性有机库Ⅰ)、LPⅡ(活性有机库Ⅱ)和RP(惰性有机库),定量研究土壤活性和惰性有机碳氮组分以及微生物生物量碳氮对氮添加的响应. 结果表明:氮添加仅对w(LPⅡ-C)(LPⅡ-C为活性有机碳Ⅱ)有显著影响,而对其他活性和惰性有机碳氮组分的影响不显著,并且对不同林分的影响存在差异. 与对照处理相比,低氮处理下浙江桂天然林、罗浮栲天然林和杉木人工林土壤w(LPⅡ-C)的增幅分别为15.3%、29.8%、68.8%;高氮处理下杉木人工林土壤w(LPⅠ-C)(LPⅠ-C为活性有机碳Ⅰ)、w(LPⅠ-N)(LPⅠ-N为活性有机氮Ⅰ)和w(RP-C)(RP-C为惰性有机碳)的增幅分别为32.4%、78.6%、28.7%;氮添加使得土壤w(SMB-C)(土壤微生物生物量碳)的增幅为18.1%~202.5%、w(SMB-N)(土壤微生物生物量氮)的增幅为0%~103.6%;在氮添加处理下,除杉木人工林土壤SMB-N/LPⅠ-N〔w(SMB-N)/w(LPⅠ-N)〕是随着氮添加水平的增加而降低外,微生物对其他林分土壤活性有机氮的利用均表现为随着氮添加水平的增加而增加. 研究显示,氮添加对阔叶林和针叶林土壤活性和惰性有机碳氮组分的影响存在差异,但差异不显著,这与它们归还土壤的凋落物性质差异有关,并且凋落物的分解差异也可能是影响土壤不同碳氮组分变化的原因. 相似文献
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An inventory of N(2)O emissions from agriculture in China using precipitation-rectified emission factor and background emission 总被引:5,自引:0,他引:5
Fertilized agricultural soils are a major anthropogenic source of atmospheric N2O. A credible national inventory of agricultural N2O emission would benefit its global strength estimate. We compiled a worldwide database of N2O emissions from fertilized fields that were consecutively measured for more than or close to one year. Both nitrogen input (N) and precipitation (P) were found to be largely responsible for temporal and spatial variabilities in annual N2O fluxes (N2O–N). Thus, we established an empirical model (N2O–N = 1.49 P + 0.0186 P · N), in which both emission factor and background emission for N2O were rectified by precipitation. In this model, annual N2O emission consists of a background emission of 1.49 P and a fertilizer-induced emission of 0.0186 P · N. We used this model to develop a spatial inventory at the 10 × 10 km scale of direct N2O emissions from agriculture in China. N2O emissions from rice paddies were separately quantified using a cropping-specific emission factor. Annual fertilizer-induced N2O emissions amounted to 198.89 Gg N2O–N in 1997, consisting of 18.50 Gg N2O–N from rice paddies and 180.39 Gg N2O–N from fertilized uplands. Annual background emissions and total emissions of N2O from agriculture were estimated to be 92.78 Gg N2O–N and 291.67 Gg N2O–N, respectively. The annual direct N2O emission accounted for 0.92% of the applied N with an uncertainty of 29%. The highest N2O fluxes occurred in East China as compared with the least fluxes in West China. 相似文献
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采用具有遗传毒性的受试化学物处理λDNA后,经体外包装,形成噬菌体颗粒,感染宿主菌LE392,噬菌斑发生率将显著降低。用这一方法对22种化学物和紫外线测试的结果表明,丝裂霉素C等13种受试化学物和紫外线对λDNA具有遗传毒性。根据用限制性内切酶消化和凝胶电泳分析的结果认为,丝裂霉素C(MMC)、甲基磺酸乙酯(EMS)和9-氨基吖啶(9-AA)对λDNA的遗传毒作用机理,可能是它们分别造成了λDNA分子发生随机断裂、DNA交联和在碱基热点上结合的移码突变。 相似文献
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三江平原小叶章湿地土壤微生物活性特征研究 总被引:9,自引:1,他引:8
选取三江平原河滨湿地、沼泽湿地和草甸化湿地3种类型小叶章湿地0~20cm土壤,研究了不同类型湿地土壤总有机碳(TOC)、微生物生物量碳(MBC)、微生物生物量氮(MBN)、基础呼吸(BR)、呼吸势(PR)、微生物熵(Cmic/Corg)和代谢熵(qCO2)变化规律.结果表明,不同类型小叶章湿地土壤总有机碳、微生物生物量碳和基础呼吸分别为46.60~75.44g.kg-1、1106.86~2319.42mg.kg-1和5.72~10.10mg.kg-.1h-1.河滨湿地和沼泽湿地土壤总有机碳、微生物生物量碳、微生物生物量氮、基础呼吸、呼吸势和微生物熵均显著高于草甸化湿地(p0.01),而河滨湿地和沼泽湿地代谢熵明显低于草甸化湿地(p0.05).各土壤微生物活性指标在河滨湿地和沼泽湿地间均无明显差异.因而,相对于河滨湿地和沼泽湿地,草甸化湿地土壤微生物活性处于较低水平,土壤总有机碳和水分含量低是限制草甸化湿地土壤微生物活性的重要因素. 相似文献