再生水灌溉对苜蓿生长及养分吸收的影响

论文在盆栽条件下,研究了再生水灌溉对苜蓿(Medicago sativa L.cv.‘Algonquin’)生长及养分吸收的影响。试验设置了清水、再生水两种灌水类型,高、中、低3个不同灌水水平。结果表明:同一灌水类型条件下,苜蓿植株生长高度随灌水量减少而降低,同一灌水水平下,灌溉水类型对植株高度无明显影响;不同的灌水水平对植株侧枝数的影响差异不显著,但灌溉水类型对植株侧枝数影响差异显著,所有处理中再生水高水平灌溉侧枝数增幅最大;与清水相比,再生水灌溉能显著增加苜蓿干物质产量;在苜蓿生长前期,再生水灌溉对苜蓿根系生长具有阻碍作用;灌溉水类型对苜蓿植株体内吸收氮、磷、钙、镁吸收量的影响主要在其生长前期,灌溉水类型对苜蓿体内钾含量无明显影响。     

种植苜蓿草的生态环境效益和经济效益分析——苜蓿草在台安县洪家农牧场种植实验

2004年台安县洪家农牧场引进加拿大优质苜蓿草进行种植实验.通过清种、林地间作和不种苜蓿草对比实验,对土壤速效氮、速效磷、速效钾、有机质、PH值、含水量进行分析,得出种植苜蓿草所产生的生态环境效益和经济效益.此项实验结论说明,紫色苜蓿是牧草之王,可促进养殖业的发展,对改善生态环境,防止土壤沙化和水土流失,改善农业结构,实现生态良性循环起到积极的促进作用,对改善生态环境起到了良好的示范作用.     

黑河中游边缘绿洲农田退耕还草的土壤碳、氮固存效应

研究黑河中游边缘绿洲农田退耕种植苜蓿5a后土壤碳、氮库的变化,通过对2个土类(开垦耕种的风沙土和灰棕漠土)退耕苜蓿地和相邻农田0～5、5～10和10～20cm土层土壤有机碳(SOC)和全氮(TN)、颗粒有机碳和氮(POC、PON)储量的分析表明:开垦耕种的风沙土和灰棕漠土有极低的SOC和TN含量,退耕种植苜蓿后0～20cm SOC储量提高了22.1%～27.8%,SOC的固存率平均为0.47 Mg/(hm²·a),0～5cm表层SOC储量变化最大,提高32%～66%;TN储量0～20cm储量变化不显著,在0～5cm表层TN储量风沙土和灰棕漠土分别提高12.8%和48.1%.退耕后POC和PON较SOC和TN有更显著的变化,其分配比例增加,0～20cm土层POC和PON储量分别提高22.8%～42.7%和18.6%～57.6%,在0～5cm变化最大;在瘠薄耕地转变为多年生苜蓿地后土壤C库的增加主要是由于POC的形成量增加.SOC含量相对更低的灰棕漠土比风沙土退耕后土壤C、N的增加更为明显.     

泥炭保护紫花苜蓿根系对柴油污染土壤修复的研究

采用盆栽试验,观察了泥炭保护根系移栽和直播2种栽培方式处理的紫花苜蓿在柴油污染土壤中的生长情况及其对土壤中柴油污染物的去除情况,探讨了利用泥炭保护根系措施清除土壤柴油污染物的可行性.结果表明,泥炭保护根系处理有利于紫花营蓿根系形态发育,能促进根系细菌和真菌的繁殖,并显著提高根区土壤柴油降解率.     

苜蓿对土壤生态环境的影响

本文论述了黑龙港低平原缺水盐渍地区苜蓿对土壤结构、土壤水分、养分和盐分的影响。苜蓿对改善土壤生态环境,实现草地生态系统良性循环,起着重要作用。     

多氯联苯污染土壤菌根真菌-紫花苜蓿-根瘤菌联合修复效应

选用紫花苜蓿（Medicago sativa L.）作为宿主植物,盆栽试验研究了丛枝菌根真菌（Glomus caledonium）和苜蓿根瘤菌(Rhizobium meliloti)单接种及双接种对PCBs复合污染土壤的联合修复效应.结果表明,在紫花苜蓿-菌根真菌-根瘤菌共生体系中,紫花苜蓿对土壤中PCBs的降低起到明显作用,使轻度污染和重度污染土壤中PCBs浓度分别下降了15.8%、 23.5%,紫花苜蓿单接种菌根真菌和苜蓿根瘤菌后轻度污染和重度污染土壤中PCBs浓度分别下降了14.8％、 24.1%和20.6%、 25.5%,双接种后土壤PCBs分别降低了23.2％、26.9%,而且也改变了紫花苜蓿根际土壤微生物群落的碳源利用程度,改善了微生物群落功能多样性.可见,紫花苜蓿豆科植物-菌根真菌-根瘤菌特殊共生体对PCBs污染土壤显示了较好的修复潜力.     

熟污泥改良土壤中Cd的形态分布特征和生物有效性

通过苜蓿盆栽实验和Tessier五步提取法,研究了不同比例的堆肥污泥施入黄土后,土壤中Cd的形态分布和生物有效性及重金属在施污土壤-苜蓿中的迁移转化规律。结果表明：不同比例的污泥施入黄土后,随着污泥施入量的增加,土壤中Cd的主要赋存形态由对照组的不可利用态(残渣态)向潜在有效态(铁锰氧化态)转化,污泥的施入提高了重金属Cd的生物有效性;苜蓿的种植对施污根际土中Cd的活性产生了钝化作用,使施污黄土根际土壤中潜在有效态Cd主要向不可利用态的Cd转化;苜蓿各器官对Cd均有富集和转移能力,苜蓿各部位重金属Cd含量的分布规律为：根部>茎叶部;线性回归分析结果表明：碳酸盐结合态Cd是苜蓿茎叶部和根部吸收Cd的主要贡献形态;因此在实际生产时须严格控制污泥的施用量,以避免Cd在苜蓿体内富集危害动物和人体健康。     

Effects of alfalfa coverage on runoff, erosion and hydraulic characteristics of overland flow on loess slope plots

An evaluation of the interactions between vegetation, overland and soil erosion can provide valuable insight for the conservation of soil and water. An experiment was conducted to study water infiltration, runoff generation process, rate of sediment erosion, and hydrodynamic characteristics of overland flow from a sloping hillside with different draw-off discharges from alfalfa and control plots with 20° slope. The effect of alfalfa on runoff and sediment transport reduction was quantitatively analyzed. Alfalfa was discussed for its ability to reduce the overland flow scouring force or change the runoff movement. Compared to the bare-soil plots, alfalfa plots generated a 1.77 times increase in infiltration rate. Furthermore, the down-slope water infiltration rate for the bare soil plots was higher than in the up-slope, while the opposite was found in the alfalfa plots. In addition, alfalfa had a significant effect on runoff and sediment yield. In comparison to the control, the runoff coefficient and sediment transportation rate decreased by 28.3% and 78.4% in the grass slope, respectively. The runoff generated from the alfalfa and bare-soil plots had similar trends with an initial increase and subsequent leveling to a steady-state rate. The transport of sediment reduced with time as a consequence of the depletion of loose surface materials. The maximum sediment concentration was recorded within the first few minutes of each event. The alfalfa plots had subcritical flow while the bare-soil plots had supercritical flow, which indicate that the capability of the alfalfa slope for resisting soil erosion and sediment movement was greater than for bare soil plots. Moreover, the flow resistance coefficient and roughness coefficient for the alfalfa plots were both higher than for the bare-soil plots, which indicate that overland flow in alfalfa plots had retarded and was blocked, and the flow energy along the runoff path had gradually dissipated. Finally, the ability to erode and transport sediment had decreased.     

黄土丘陵沟壑区苜蓿地土壤水分环境效应

根据田间试验资料,分析研究了黄土丘陵沟壑区苜蓿地土壤水分的周年变化规律,并以休闲地和几种一年生作物地作为对照进行对比研究,得出以下主要结论:①雨季降水对苜蓿地土壤水分的补给起着重要的作用,其土壤贮水量动态与年内的降雨周期相吻合,但总体上朝着土壤不断干化的方向发展;②经过一个雨季,苜蓿地的土壤贮水量与平均含水量分别呈不同程度的下降,而休闲地与4月份持平;③相同的降水对不同作物地的补给效果不同,以3m土层计算,苜蓿地的农田蒸散量与谷子、玉米相当,比豆子地高,但要低于高粱地;④长期种植苜蓿引起的深层土壤干化问题必须引起足够的重视,干化土地的水分恢复不是一朝一夕的事情。     

Degradation of Benzo[a]Pyrene in Soil with Arbuscular Mycorrhizal Alfalfa

Mycorrhizal and non-mycorrhizal alfalfa (Medicago sativa) was grown in pots containing soil artificially contaminated with various levels of benzo[a]pyrene (B[a]P)(0, 1, 10 and 100 mg kg^–1). Soil and plants were sampled after 30, 40, 50, 60 and 90 days and compared with unlanted pots. The percentage of mycorrhizal root length colonized by Glomus caledoniun was not significantly affected by the addition of B[a]P up to 10 mg kg^–1 but was significantly lower at 100 mg kg^–1B[a]P compared with low concentrations (p < 0.05). There was no difference in soil polyphenol oxidase and dehydrogenase activity among the controls and applications of 1 and 10 mg kg^–1 of B[a]P. However, enzyme activities were significantly higher at 100 mg kg^–1B[a]P compared with the other three treatments, and there was no mycorrhizal effect. Over a period of 90 days the concentration of B[a]P in soil in which alfalfa was grown was significantly lower than in unplanted soil (p < 0.05). Degradation rates of B[a]P added at 1, 10 and 100 mg kg^–1 without G. caledonium were 76, 78 and 53%, and with mycorrhizal inoculation were 86, 87 and 57%. The degradation rate in unplanted soil was significantly lower than in planted soil, and was significantly higher in medium- and low-B[a]P treatments than in the high B[a]P concentration tested. There is a possibility of enhancement phytoremediation of PAHs in rhizosphere soil with arbuscular mycorrhizal fungi.