湖北省主要城市园林绿地土壤养分评价

根据湖北城市地形,对2个山地城市(恩施、十堰)、3个丘陵城市(荆门、襄樊、宜昌)和6个平原城市(武汉、孝感、咸宁、荆州、随州、黄石)绿地土壤进行采样.每个城市又按照4种不同利用类型,包括公园绿地、住宅区、事业单位(包括学校、医院、政府机关等)和交通主干道绿地分别取样.结果表明:湖北省主要城市绿地土壤pH较自然土壤明显偏高,均值7.9;土壤有机质(6.8g·kg-1)明显处于缺乏水平;有效N、P、B含量处于较低水平;其他中微量元素(Ca、Mg、S、Fe、Cu、Mn、Zn和B)有效态含量适中.土地利用方式对平原城市土壤养分含量影响显著,住宅区绿地土壤pH显著高于公园、街道旁和事业单位,街道绿地微量元素S、Cu、Mn、Zn有效态含量显著高于其他利用类型,公园绿地养分含量最低.不同地形城市土壤养分含量存在显著差异,平原城市土壤有机质、铵态氮、有效K、有效P和许多中微量养分元素(Ca、Mg、S、Fe、Cu和Mn)的含量显著高于丘陵城市.     

Cu污染土壤中溪荪和花菖蒲的生长状况及对Cu的积累及转运能力

采用土壤栽培方法,研究了在Cu添加量为0(CK)、200、400、600、800和1 000μg·g-1的土壤中溪荪(Iris sanguinea Donn es Horn.)和花菖蒲(I.ensata Thunb.var.hortensis Makino et Nemoto)叶和根的数量、长度及生物量(干质量)6个生长指标的变化趋势,并对叶和根中的Cu含量和积累量、全株的Cu积累量、Cu的富集系数及转运系数进行了比较分析.结果表明:随土壤中Cu添加量的提高,溪荪的根数逐渐降低且显著低于对照;而溪荪的其余5个生长指标和花菖蒲的6个生长指标均总体呈现出在Cu添加量较低的条件下逐渐增加并显著高于对照、在Cu添加量较高的条件下逐渐减小且显著小于对照的变化趋势;其中在Cu添加量1 000μg·g-1的土壤中2种植物的生长均受到显著抑制(P＜0.05);而添加400和600μg·g-1Cu则分别对2种植物的生长有一定的促进作用.随土壤中Cu添加量的增加,溪荪和花菖蒲叶及根中的Cu含量均逐渐提高;溪荪对Cu的富集系数和转运系数以及花菖蒲对Cu的富集系数均显著小于对照,而花菖蒲对Cu的转运系数则呈现在Cu添加量较低的条件下高于对照、Cu添加量较高的条件下低于对照并逐渐减小的趋势;在添加了Cu的土壤中,溪荪叶、根和全株对Cu的积累量均低于花菖蒲,但均显著高于对照,且2种植物根的Cu含量及积累量均大于叶片,表明溪荪和花菖蒲均具有一定的Cu积累能力,且主要积累在根中,花菖蒲对Cu的积累能力优于溪荪.综合分析结果显示:溪荪和花菖蒲不是Cu超积累植物,但对Cu胁迫均具有一定的耐性,且花菖蒲的耐性略强于溪荪;溪荪和花菖蒲分别适宜栽植于Cu含量400和600μg·g-1以下的土壤中,可用于轻度和中度Cu污染土壤的植物修复和环境美化.     

不同植被恢复模式下中亚热带黄壤坡地土壤微量元素效应

以武陵山区女儿寨小流域为例,研究了中亚热带黄壤坡地7种典型植被恢复模式下土壤微量元素有效性及其与土壤有机质、pH值之间的关系.结果表明： 0～20 cm土层荒草灌丛的B、Mn含量、油桐人工林Mo、Cu含量、杜仲人工林Zn含量和毛竹 杉木混交林Fe含量最高;20～40 cm土层润楠次生林B、Fe、Mn含量、荒草灌丛模式Mo含量、油桐人工林Zn含量和杜仲人工林Cu含量最高;毛竹 杉木混交林B、Mo、Cu、Mn含量在各层土壤均最低.各元素有效性指数以Mn最高,Cu最低,排序为Mn>Zn>Fe>Mo>B>Cu;土壤微量元素有效性综合指数以荒草灌丛模式最高(12.28),毛竹 杉木混交林最低(2.95),排序为Ⅶ>Ⅴ>Ⅲ>Ⅳ＞Ⅰ＞Ⅱ＞Ⅵ.土壤有机质含量与B、Zn有效态含量之间线性关系显著,二次多项式亦可较好地描述有机质与有效态Mn之间的关系,而有机质与Mo、Fe、Cu之间曲线回归关系不显著.土壤pH值与土壤Zn、Cu呈显著正相关,与Mn、Mo也有较好的相关性,而与B相关性较低,与Fe为弱负相关.     

土壤与大气Cu处理下迎春的耐性和富集特征研究

作为北京市常见园林灌木树种之一，迎春(Jasminum nudiflorum)因其在早春独特的观赏性而深受市民喜爱。Cu污染是北京市较为严重的重金属污染类型之一。为探讨迎春对城市Cu污染的修复作用，该文通过模拟北京市土壤和大气Cu污染条件，采用盆栽试验，设置9种不同浓度的土壤和大气Cu处理，以验证迎春Cu富集能力及生理生长特性。结果表明：(1)土壤和大气沉降处理均能显著增加迎春根、茎、叶中的Cu含量，其中土壤贡献率为63.48%～96.99%。各处理中Cu含量均表现为根>茎>叶。(2)大气处理下光化学转化效率(F_v/F_m)和相对叶绿素含量(SPAD值)提高，初始荧光(F₀)降低，光合能力增强，而土壤处理及土壤和大气双重处理则对迎春的光合作用产生抑制影响。(3)与大气处理相比，土壤处理及土壤和大气双重处理导致活性氧(ROS)积累增多，膜脂过氧化作用加剧，丙二醛(MDA)含量大幅升高，抗氧化酶活性与脯氨酸(PRO)含量逐渐下降，造成生物膜系统损伤。(4)低浓度Cu处理对迎春生长有促进作用，而高浓度Cu处理(SHA...     

新疆棉田土壤质量综合评价方法

以新疆主要棉区为研究对象,测定了哈密、博乐、昌吉、奎屯、石河子、阿克苏及喀什棉田土壤耕层的pH、盐分、有机质、全氮、速效磷、速效钾及Cr、Cu、Zn、As、Pb 共计11个指标,综合分析土壤理化性质和重金属含量,采用土壤质量综合指数(SQI)对新疆主要棉区棉田土壤质量进行综合评价.结果表明: 新疆棉区棉田土壤呈碱性,pH均值为7.87,盐分含量均值为3.44 g·kg^-1,为轻度盐化土壤,有机质和全氮含量均偏低,速效磷、速效钾含量较为丰富,与第二次全国土壤普查数据相比,土壤pH、盐分含量、有机质和全氮均呈下降趋势,土壤速效磷明显增长,部分地区土壤速效钾呈现出不同程度的升高趋势;Cr、Cu、Zn、As、Pb 5种重金属含量分别为45.88、40.66、68.30、12.88、16.68 mg·kg^-1,均未超过国家二级标准,但与新疆土壤元素背景值相比,Cu、Zn、As均有累积现象.当重金属内梅罗综合污染指数(PN)小于0.5时,土壤理化性质越好,土壤综合质量越好.土壤有机质、全氮、Cu、Zn和As是影响新疆棉区棉田土壤质量的重要因素.新疆棉区棉田土壤质量总体属于中等水平,昌吉、奎屯质量最高,SQI为0.52,阿克苏质量最低,SQI为0.31,不同棉区土壤质量呈现为:北疆>东疆>南疆.     

杉木人工林土壤活性有机质变化特征

在中国科学院会同森林生态实验站对第一代、第二代杉木林和地带性阔叶林土壤活性有机质主要组分进行了研究.结果表明,土壤活性有机质各组分含量均为杉木林低于阔叶林,而第二代杉木林又低于第一代杉木.第一代杉木林活性有机质总量、微生物生物量碳、水溶性有机碳和碳水化合物含量分别为18.79 g·kg^-1、421.7 mg·kg^-1、22.2 mg·kg^-1和136.3 mg·kg^-1,上述活性有机质组分在第二代杉木林中的含量分别是第一代杉木林的73.6%、87.9%、66.3%和3.2%,地带性阔叶林则分别为22.31 g·kg^-1、800. mg·kg^-1、361.1 mg·kg^-1和220.1 mg·kg^-1.相关性分析结果表明,土壤活性有机质各组分之间具有不同程度的相关性,其中土壤微生物生物量碳与其它活性有机质组分的相关性相对较高.     

白术连作根际土壤的理化性质及微生物区系变化

对不同种植年限白术(Atractylodes macrocephala Koidz.)根际土壤的部分理化指标、酶活性和微生物区系进行了测定和比较。结果表明:随白术种植年限的增加(0、1和2 a),根际土壤pH值显著下降(P<0.05),根际土壤中有机质和全氮含量呈先升高后降低趋势,速效钾含量则逐渐升高,而有效磷含量和C/N比小幅波动,总体上不同种植年限根际土壤的这些指标差异不显著;根际土壤中有效铁、有效铝和交换性锰含量显著或极显著(P<0.01)增加,且较对照(未种植白术的土壤)分别增加了127.51%、18.38%和106.83%,但有效铅含量变化幅度较小;2年生白术根际土壤中过氧化氢酶、脲酶和蛋白酶活性显著低于对照;2年生白术根际土壤中细菌和放线菌数量及微生物总量较1年生白术根际土壤显著下降,真菌数量则显著上升。结果显示:土壤酸化严重、金属离子大量积累、主要酶活性失调以及微生物区系改变可能是白术连作障碍的潜在原因。     

长期施肥对设施菜田土壤酶活性及土壤理化性状的影响

利用沈阳农业大学蔬菜长期定位施肥试验田,研究了长期施肥对设施菜田土壤酶活性及土壤理化性状的影响.结果表明:长期施用有机肥或有机肥与氮肥配合施用可明显提高土壤有机质和氮、磷、钾养分含量,改善土壤物理性状,增强土壤转化酶、脲酶和中性磷酸酶的活性;而长期单施氮肥造成土壤pH值和土壤酶活性降低.土壤酶活性与土壤养分因子的相关分析表明,转化酶活性与土壤有机质、全磷含量呈显著正相关;脲酶活性与土壤有机质、全磷和速效钾含量呈极显著正相关,与碱解氮和速效磷含量呈显著正相关;中性磷酸酶活性与土壤有机质、全磷和速效钾含量呈显著正相关;脱氢酶活性与土壤各养分因子均无明显相关性.     

廊道式工程建设对土壤生态环境影响的meta分析

廊道式工程建设对沿线区域生态环境造成不可避免的影响,定量化研究廊道式工程建设对沿线地区土壤生态环境的影响具有重要意义。本文基于meta分析方法,研究了3种廊道式工程(输油/气管道、公路和铁路)对土壤生态环境的影响。结果表明,廊道式工程对土壤理化性质产生一定的影响:3种工程周边的土壤养分指标和土壤含水量的结合效应值均<1;管道工程建设对土壤有机质、有效氮、总氮、总磷和pH的扰动达到显著水平(P<0.05);公路显著降低周边土壤总磷、含水量和CEC的含量(P<0.05),同时公路显著增加了周边土壤容重和pH,结合效应值分别达到1.2265和1.1649,公路造成周边土壤Cu、Zn、Pb、Ni、Cd、Cr和As的显著污染(P<0.05);铁路显著降低沿线土壤有机质和总氮的含量(P<0.05),并且导致周边土壤Cu、Zn、Pb、Cd的显著污染(P<0.05)。     

人工油松林恢复过程中土壤理化性质及有机碳含量的变化特征

采用时空替代法,选取岷江上游大沟流域内不同恢复时期(12、18、25、35a)的人工油松林为研究对象,研究了植被恢复过程中土壤理化性质及有机碳含量的变化特征,同时探讨了它们之间的相互关系.研究结果表明沿恢复梯度,土壤质量得到了改善,主要表现为土壤粘粒含量、比表面积、有机质含量显著增加,土壤粉粒含量和pH值则显著下降.土壤有机质与土壤粘粒和比表面积呈显著正相关,与土壤容重呈显著负相关.此外,土壤有机碳含量沿恢复梯度显著增加,0-50 cm内土壤有机碳含量从5.59 kg/m2增加到12.64 kg/m2,土壤年平均固碳速率为0.31 kg/m2.     

铜尾矿库区狗牙根根际土壤铜的形态变化

通过野外调查和室内分析,对安徽省铜陵市铜尾矿库区狗牙根根际土壤Cu的形态进行了研究．结果表明,尾矿库区狗牙根根际与非根际土壤Cu大部分为矿物态Cu,交换态Cu含量偏低．与非根际土壤相比,狗牙根根际土壤pH值下降,有机质含量显著增加．随着狗牙根的生长,根际土壤有机结合态Cu和交换态Cu含量显著增加,其占土壤总Cu量的比例分别增加7．89％和超过5％,碳酸盐结合态Cu和铁锰氧化物结合态Cu含量则有所下降．狗牙根生长促进了根际土壤Cu形态的转化,提高了Cu在土壤中的迁移能力,加之狗牙根的吸收作用,其根际土壤Cu含量显著降低．     

长期施用猪粪红壤稻田土壤Cu、Zn累积规律

为揭示长期施用猪粪红壤稻田土壤Cu、Zn累积规律,以设立于1981年的红壤稻田有机肥定位试验为载体,选取PM1(早稻施猪粪和紫云英)、PM2(早稻施紫云英+晚稻施猪粪)、GMS(早稻施紫云英+晚稻秸秆还田)和NPK(早稻施化肥)等处理为对象,分析了不同试验年限土壤全量和有效态Cu、Zn含量。结果表明:长期施用猪粪显著提高了土壤Cu、Zn含量;连续施用猪粪30 a后,土壤全量Cu、Zn含量分别增加了7.69—9.52 mg/kg和22.42—35.46 mg/kg;生物有效性显著增加,有效态Cu、Zn含量占全量Cu、Zn的比例分别由15%和5%增加到51%和27%。猪粪年度内的施用时间对土壤Cu的累积没有显著影响,早稻施用猪粪加剧了土壤Zn的累积。土壤铜、锌累积分为两个差异显著的阶段,1981—2002年为缓慢增长期,2002—2010年为快速增长期,这可能与2002年后施用的猪粪中Cu、Zn含量增高有关。以研究的结果推算,红壤稻田鲜猪粪施用量在9.5 t hm-2a-1以下,50 a内不会造成土壤Cu、Zn含量超标。     

Effect of annual variation in soil pH on available soil nutrients in pear orchards

Soil pH is an important factor affecting the availability of soil nutrients that impact plant growth. Given the susceptibility of soil pH to excessive fertilization and the widespread use of manures, it is essential to examine the influence of soil pH on the distribution and availability of soil nutrients. We sampled and analyzed brown soils from pear orchards in thirteen towns in Wendeng county. Samples were obtained from areas along or between rows of trees at specified distances and depths. The results showed that the soil pH fluctuated from 4.06 to 6.59 in October 2008 and from 4.24 to 7.57 in April 2009. The quantity of soil samples with pH below 5.50 increased by 34.6%. Analysis of the soil pH for samples obtained along the rows of trees showed that the pH decreased as the depth increased (except for the range 5.5 to 6.0); soil pH in the samples obtained between the rows of trees demonstrated different trends. The average organic matter (O.M.) content as well as the N (NH₄⁺) and available P, K, Cu, Zn, Fe, and Mn contents in the samples collected in October 2008 were higher than those observed in April 2009. Conversely, the values for other available nutrients were lower than those in the samples collected in April 2009. The available nutrients and organic matter (O.M.) content in different pH ranges varied. The soil pH was significantly or very significantly correlated with N (NH₄⁺ and NO₃^-), available K, Cu, Fe, and exchangeable Ca for the October 2008 samples, while a significant or very significant correlation existed between N (NH₄⁺), available P, Zn, exchangeable Ca, and exchangeable Mg for the April 2009 samples. The correlations between soil pH and the amounts of available nutrients and organic matter (O.M.) along the rows of trees in September 2009 were nearly consistent with those between the rows.     

Effect of annual variation in soil pH on available soil nutrients in pear orchards

Soil pH is an important factor affecting the availability of soil nutrients that impact plant growth. Given the susceptibility of soil pH to excessive fertilization and the widespread use of manures, it is essential to examine the influence of soil pH on the distribution and availability of soil nutrients. We sampled and analyzed brown soils from pear orchards in thirteen towns in Wendeng county. Samples were obtained from areas along or between rows of trees at specified distances and depths. The results showed that the soil pH fluctuated from 4.06 to 6.59 in October 2008 and from 4.24 to 7.57 in April 2009. The quantity of soil samples with pH below 5.50 increased by 34.6%. Analysis of the soil pH for samples obtained along the rows of trees showed that the pH decreased as the depth increased (except for the range 5.5 to 6.0); soil pH in the samples obtained between the rows of trees demonstrated different trends. The average organic matter (O.M.) content as well as the N (NH₄⁺) and available P, K, Cu, Zn, Fe, and Mn contents in the samples collected in October 2008 were higher than those observed in April 2009. Conversely, the values for other available nutrients were lower than those in the samples collected in April 2009. The available nutrients and organic matter (O.M.) content in different pH ranges varied. The soil pH was significantly or very significantly correlated with N (NH₄⁺ and NO₃^-), available K, Cu, Fe, and exchangeable Ca for the October 2008 samples, while a significant or very significant correlation existed between N (NH₄⁺), available P, Zn, exchangeable Ca, and exchangeable Mg for the April 2009 samples. The correlations between soil pH and the amounts of available nutrients and organic matter (O.M.) along the rows of trees in September 2009 were nearly consistent with those between the rows.     

Role of earthworm-straw interactions on phytoremediation of Cu contaminated soil by ryegrass

It is well known that the earthworm's activities can increase the availability of soil nutrients, improve soil structure, and enhance the biomass of plants in uncontaminated soil. Recently, many researchers found that some metal-tolerant earthworms can survive and even change the fractional distribution of heavy metals in contaminated soil. Furthermore, it has been revealed that earthworms are able to increase metal availability, and therefore, accumulate more metals in plants through their burrowing and casting activity. It is clear that the influence of soil animals is an important factor for phyto-remedation that must be taken into account. ~In this article, the authors studied some effects of addition of earthworms (Metaphire guillelmi), corn straw, and in combinations of earthworms and corn straw on the growth and Cu uptake by ryegrass in Cu contaminated pot soils. The experiment consisted of four levels of Cu addition (0, 100, 200, 400 mg·kg?1) and four treatments. The treatments were 1. control (CK); 2.straw mulching only (M); 3. earthworm additions to soil only (E); and 4.straw mulching plus earthworm additions (ME). Each treatment had three replicates. 10 seeds of ryegrass (Lolium multiflorum) were sowed in each pot and harvested after 30 days. After 30 days of incubation, all earthworms were found to be alive and the pot soils were burrowed through by earthworms. Results showed that the biomass of earthworm declined with the increase of the dosage of Cu additions. The biomass of earthworm increased significantly in treatment 4 (ME) as compared with treatment 3 (E). Not only the earthworms could get more food from the straw, but also could counteract some negative effects of Cu on the earthworms. The rates of straw decomposition in ME treatment increased by about 58.11% ?77.32%. The earthworm activities increased root biomass of ryegrass significantly, but did not show the effect on plant root growth. On the contrary, straw enhanced roots biomass significantly instead of shoots biomass. It was also found that the concentration of Cu in the plant shoot and the plant root, as well as plant Cu uptake were enhanced by earthworm's activities and straw mulching. The increased amount by straw mulching was lower than that of earthworms (E). The treatment of the earthworm–straw mulching combinations enhanced plant Cu concentration, and the amount increased by it was lower than that of the earthworm treatment (E) but higher than that of straw mulching treatment (M). The accumulation factors of copper in the shoots of ryegrass were increased by 31.22% ?121.07%, 2.12% ?61.28% and 25.56% ?132.64%, respectively, in treatment 3(E), 2(M), and 4(ME), respectively. In conclusion, the earthworm activities, straw-mulching and their interactions may have potential roles in elevating phyto-extraction efficiency in low to medium level Cu contaminated soil.     

Effects of microplastics and biochar on soil cadmium availability and wheat plant performance

Biochar is a promising amendment to promote cadmium (Cd) sorption and fixation in agricultural soil, where microplastics are emerging contaminants in soil. Herein, a greenhouse pot experiment was conducted to elucidate the effects on Cd availability in a soil–plant system by biochar and fresh/aged microplastics application. The fresh microplastics led to an obvious increase in soil Cd availability and Cd uptake by wheat plant, while the aged microplastics increased the available Cd in soil but had no effect on Cd uptake by wheat plant, which was likely attributed to the blocking effect of the aged microplastics on Cd transportation from the soil to the wheat plant. Unexpectedly, biochar had increased Cd availability and Cd uptake. The increased soil soluble Cd was because of both decreased soil pH and elevated dissolved organic matter (DOM) content resulted by biochar addition. Also, the unchanged Cd adsorption of the soil was likely responsible for the increased tested soil Cd availability. In addition, the combined effects of a greater decrease in soil pH, an increase in soil DOM content, and a reduction in Cd adsorption after the addition of microplastics to biochar-amended soil resulted in a significant increase (ranging from 2.63% to 47.73%) in Cd availability compared to soil treated with biochar alone. Moreover, fresh microplastics inhibited wheat growth, and greater inhibition effect was observed for their aged ones. The biochar elevated the wheat biomass; however, the coexistence of microplastics and biochar decreased the wheat plant biomass compared with biochar alone, due to the negative influence of microplastics in plant growth.     

Effects of soil acidification on the chemical extractability of Fe,Mn, Zn and Cu and the growth and micronutrient uptake of highbush blueberry plants

Summary The effects of soil acidification and micronutrient addition on levels of extractable Fe, Mn, Zn and Cu in a soil, and on the growth and micronutrient uptake of young highbush blueberry plants (Vaccinium corymbosum L. cv. Blueray) was investigated in a greenhouse study.Levels of 0.05M CaCl₂-extractable Fe, Mn, Zn and Cu increased as the pH was lowered from 7.0 to 3.8. However, the solubility (CaCl₂-extractability) of Fe and Cu was considerably less pH-dependent than that of Mn and Zn. With the exception of HCl-and DTPA-extractable Mn, micronutrients extractable with 0.1M HCl, 0.005M DTPA and 0.04M EDTA were unaffected or raised only slightly as the pH was lowered from 6.0 to 3.8. Quantities of Mn and Zn extractable with CaCl₂ were similar in magnitude to those extractable with HCl, DTPA and EDTA whilst, in contrast, the latter reagents extracted considerably more Cu and Fe than did CaCl₂. A fractionation of soil Zn and Cu revealed that soil acidification resulted in an increase in the CaCl₂- and pyrophosphate-extractable fractions and a smaller decrease in the oxalate-extractable fraction.Plant dry matter production increased consistently when the soil pH was lowered from 7.0 to 4.6 but there was a slight decline in dry matter as the pH was lowered to 3.8. Micronutrient additions had no influence on plant biomass although plant uptake was increased. As the pH was lowered, concentrations of plant Fe first decreased and then increased whilst those of Mn, and to a lesser extent Zn and Cu, increased markedly.     

Mineralization of nitrogen from15N labelled fungi,soil microbial biomass and roots and its uptake by barley plants

The effect of vesicular-arbuscular mycorrhizal fungi (VAM) on field bean and spring wheat dry matter production and on phosphorus, zinc, copper, iron and manganese uptake was determined under greenhouse conditions. Nutrient availability was varied by using different sizes of pots and by diluting the soil with sand. VAM increased plant dry matter production under all sets of growth conditions. VAM were found to directly increase the uptake of P, Zn, Cu and Fe by field beans and of P and Zn for wheat in both experiments. Increased uptake of the other nutrients measured was attributed to increased dry matter production or other factors. The effect of VAM decreased as the pot size holding the host plants decreased, but was not affected by the ratio of soil to sand if the pot size was kept constant. Nutrient uptake by beans as a proportion of total amount of nutrient present increased as the amount of nutrient decreased. Increase in root-soil contact and altered chemical equilibria are probable reasons for increased efficiency of nutrient uptake by beans as the level of available nutrient decreased. For wheat, which has a relatively fibrous root system, decreasing the nutrient availability had minimal effects on nutrient uptake in these experiments. Increases in total uptake of a particular nutrient resulting from inoculation with VAM are not necesarily indicative of a direct uptake of that nutrient by the VAM.     

栽培模式对旱地小麦产量和土壤肥力的影响

通过田间试验,研究地膜覆盖、秸秆还田和种植绿肥对冬小麦籽粒产量和土壤肥力的影响.结果表明: 与传统模式相比,地膜覆盖并不总能提高旱地小麦产量,3年平均产量无显著变化,但降低20～40 cm土壤全氮、有效磷、速效钾、有效硫、有效锌和有效锰含量,对土壤有机质、硝态氮、有效铁和有效铜含量无显著影响.秸秆还田的小麦产量3年平均降低12.1%,收获期0～20 cm土层全氮提高5.8%,20～40 cm土层有效铜含量提高6.2%,而有效磷和有效锰分别降低36.1%和10.2%,对开花期和收获期土壤有机质、硝态氮、速效钾、有效硫、有效锌和有效铁无显著影响.种植绿肥的籽粒产量降低12.1%,同时土壤pH、有效磷和有效硫含量降低,有机质、全氮、硝态氮、有效锌和有效锰均增加,对土壤速效钾、有效铁和有效铜均无显著影响.综上,在旱地土壤肥力较低的条件下,地膜覆盖和秸秆还田不利于土壤肥力的提升,使小麦增产受到限制;种植绿肥培肥效果最好,但应考虑区域降水情况,注意其带来的减产问题.     

铜陵矿区土壤和油菜中铜的分布特征

采集铜陵市几个矿区周围土壤和油菜作物样品,研究了铜在矿区不同土壤及油菜中的分布特征.结果表明:铜陵矿区周边耕作土壤铜含量普遍较高;矿区周围残坡积母质上发育的旱作土壤和下游水稻土的污染较严重,而距矿区较远的潮土污染水平较低;水稻土与矿区周围残坡积母质上发育的旱作土壤全铜含量相近,前者的铜主要来自受污染的灌溉水并有着较高的生物有效性.3种类型土壤的有效铜与全铜含量均显著相关.供试土壤中铜的平均活化率(有效铜占全铜含量的百分比)为15.0%,且与土壤全铜和有机质含量呈正相关,与土壤pH和锰含量呈负相关.油菜籽和油菜秸秆中铜的平均含量分别为4.0和5.8mg.kg-1.当土壤中有效铜含量较低时,油菜中的铜含量随着土壤中有效铜含量增加而上升的趋势十分明显,当土壤中有效铜含量大于30mg.kg-1时,油菜作物吸收铜的能力下降,油菜富集铜的效率逐渐降低.