含油废水对农作物影响研究

本用盆栽方法研究了含油废水对小麦和玉米生长发育、产量及其品质影响，分析了矿物油和苯并（ａ）芘（Ｂａｐ）在土壤与作物籽粒中的残留情况，并对土壤矿物油净化率进行了计算分析。     

中国北方典型地区农用地膜污染现状调查及其防治对策

通过对我国北方典型地区的调查，初步探索了该地区土壤农膜残留量和残膜特征。研究表明，河北省典型地区温室大棚、蔬菜田和作物田的农膜土壤残留量平均分别为5.629、7.369和2.822 kg·hm^-2，黑龙江省典型地区温室大棚、蔬菜田和作物田残留量平均分别为4.169、3.682和2.430 kg·hm^-2，各采样点之间存在着较大差异，但普遍较高，均明显高于未使用农膜的对照土壤。两地区之间除作物田的土壤农膜残留量没有明显差异外，河北地区其他两类土壤中的农膜残留量水平明显高于黑龙江地区，这种差异与各地区在农事活动及农膜使用上的差异具有一定的相关性。上述两地区土壤中残留农膜尺寸基本一致，主要集中在10～15 cm之间。该文针对我国目前农膜使用情况及其污染现状，提出了相应的防治对策。     

中国北方典型地区农用地膜污染现状调查及其防治对策

通过对我国北方典型地区的调查,初步探索了该地区土壤农膜残留量和残膜特征.研究表明,河北省典型地区温室大棚、蔬菜田和作物田的农膜土壤残留量平均分别为5.629、7.369和2.822 kg·hm-2,黑龙江省典型地区温室大棚、蔬菜田和作物田残留量平均分别为4.169、3.682和2.430 kg·hm-2,各采样点之间存在着较大差异,但普遍较高,均明显高于未使用农膜的对照土壤.两地区之间除作物田的土壤农膜残留量没有明显差异外,河北地区其他两类土壤中的农膜残留量水平明显高于黑龙江地区,这种差异与各地区在农事活动及农膜使用上的差异具有一定的相关性.上述两地区土壤中残留农膜尺寸基本一致,主要集中在10～15 cm之间.该文针对我国目前农膜使用情况及其污染现状,提出了相应的防治对策.     

论农田“白色污染”的防治技术

在调查、试验研究和推广应用的基础上，介绍了农田土壤中地膜残留引起“白色污染”的现状、原因，及对农田土壤、作物生长及其产量的不良影响。认为残留地膜降低了土壤的渗透性能，减少了土壤的含水量，削弱了耕地的抗旱能力。同时，残留地膜阻碍了农作物的根系生长，影响了作物的生长。土壤中残留地膜达到一定数量时，就会引起农作物减产；提出了防治残留地膜污染的技术，即适期揭膜技术。     

农膜残留对大豆光生理特征及生物量累积的影响

农膜覆盖技术的应用及推广极大地提高了干旱半干旱地区的农业产量,促进了当地农业发展及社会经济效益。然而,由于农膜碎片化程度高、回收难度大、降解周期长,使得残留在土壤中的农膜日益增多,严重威胁着作物生长、土壤健康以及农业可持续发展。尽管农膜残留对土壤质量影响的研究较多,但对于其种类(可降解或不可降解)及残留累积量对作物光生理特征的研究还相对较少。本试验以大豆为研究对象,对比普通聚乙烯(PE)和生物降解(BP)两种农膜(残片大小为0.5～2 cm),研究不同农膜残留累积量(土壤重量的0、0.1%、0.5%、1.0%)下大豆花期及初荚期叶片光合作用光、CO_2响应曲线特征及花期、收获期的植株生物量,探讨塑料类型及残留量对大豆光生理特征及生物量累积的影响。结果表明:PE残留导致大豆叶片光补偿点在花期降低23.96%,而初荚期升高51.38%,说明PE残留导致大豆叶片弱光利用能力在花期提升,但在初荚期被抑制。在初荚期,BP残留使光补偿点降低54.82%,且光饱合点升高58.12%,从而提高了叶片强光适应能力,增大了叶片光能利用范围。同时, PE和BP添加使暗呼吸速率分别增长30.56%和22.28%,从而导致干物质消耗增加。土壤中PE、BP残留量的增加,最大光合力分别降低36.49%和23.56%,表明大豆叶片CO_2利用能力减弱; CO_2补偿点分别降低67.96%和38.91%,从而提高了叶片低浓度CO_2的利用能力,并降低光呼吸速率,从而减少了干物质的消耗。此外,不同农膜及残留量处理下,仅在花期0.1%与0.5%残留量的BP处理中,地下生物量随农膜残留量的增加显著降低,其他各处理间地上及地下生物量无明显变化。光响应及CO_2响应曲线各拟合参数与生物量的Pearson相关性分析结果表明,收获期PE处理下,地上生物量与光补偿点呈显著负相关,而光呼吸速率、CO_2补偿点、初始羧化效率与生物量(地上+地下)的积累有较强相关性。因此,PE农膜残留量增加提高了大豆花期叶片对于弱光的利用能力而减弱初荚期对弱光的利用能力,BP农膜残留量增加则会增强初荚期叶片对弱光的利用,也对大豆叶片适应强光的能力有所提升。     

影响无公害设施农业生产的因素及对策

设施内环境和人们的栽培管理技术措施对作物生产和生长发育规律有较大作用影响。影响无公害设施农业生产的两大因素：一是环境因素，包括农膜、光照、温度、湿度、大气、土壤、有害生物等；二是栽培管理技术措施。     

水泥硬壳覆盖对盐渍土水盐运动及作物生长发育的影响

通过田间定位试验,研究了水泥硬壳覆盖对盐渍化土壤蒸发、作物蒸腾、土壤盐分变化、作物生长发育状况、产量及水分利用效率的影响。结果表明：硬壳覆盖能减少农田土壤无效蒸发,调节土壤盐分在土体中的分布,促进春播作物苗全苗壮,提高作物产量和水分利用效率。     

设施菜地土壤酞酸酯污染的初步研究

通过对杭州周边某设施蔬菜大棚基地的土壤采集分析和农田残留农膜的提取分析,结果表明该地区土壤存在一定程度的酞酸酯污染,污染程度与国内大部分农田土壤相当。农膜中酞酸酯含量和农膜类型对土壤酞酸酯含量均有一定影响。农膜中酞酸酯含量和土壤中酞酸酯含量显著正相关,长期农膜覆盖与黑色农膜覆盖土壤的酞酸酯含量相对较高,因此减少农膜在土壤中的残留是减少土壤酞酸酯污染的有效途径之一。大棚覆盖或地膜覆盖等不同农膜覆盖方式对土壤酞酸酯含量在本研究中未发现显著差异。土壤酞酸酯含量与土壤有机质极显著正相关,表明土壤有机质对酞酸酯,尤其是高分子量酞酸酯污染单体的环境行为有重要的影响。     

不同轮作体系土壤残留硒锌对小麦产量与营养品质的影响

采用盆栽试验,通过玉米-小麦和大豆-小麦轮作,探讨了不同种植模式中,土壤残留硒锌对小麦产量与营养品质的影响。结果表明,土壤中残留硒锌对小麦生物量和产量的影响与作物轮作体系有关。玉米-小麦轮作,土壤残留硒锌并没有表现出增加小麦产量的趋势,而大豆-小麦轮作,土壤残留硒锌对小麦生物量和产量呈增加趋势。土壤残留硒锌可改变作物体内元素组成。玉米-小麦轮作,土壤残留硒锌有利于小麦籽粒对氮、钾、硫、钙、铁、锌、硒、铜元素的吸收累积。大豆-小麦轮作,土壤残留硒锌促进小麦对钾、硫、镁、铁、锌、硒、铜、锰、硼的吸收,而氮、磷、钙吸收减少。     

常德市武陵区农膜污染土壤现状分析及控制对策的研究

对常德市武陵区使用农膜蔬菜基地的土壤中农膜残留情况进行调查研究,在农膜技术实现大幅度高产稳产的同时,也产生了大量不溶解、不腐烂的废旧残留农膜,对耕作层土壤结构破坏严重,给农村环境带来了很大程度的污染。如何通过政策及科技手段降低农膜污染,提出了一系列的控制对策。     

Chronosequence of pedogenesis and Quaternary Paleoenvironment in Kunming Basin,Yunnan Province,China

Soils on the terrace groups along the eastern coast of Dianchi Lake located south of Kunming, Yunnan Province, China, consist of a series of chronose-quences reflecting the age of terrace formation and environmental changes since the early Pleistocene. Red-colored soils with reticulated mottlings on the higher terraces are classified as Argillic Latored soils, corresponding to Rhodic Nitisols (FAQ-Unesco) or Rhodic Kandiudults (USDA), whereas red-colored soils on the middle terraces are classified as Agric Red soils, corresponding to Rhodic Nitisols (FAO-Unesco) or Typic Rhodudalfs (USDA). On the other hand, soils on the lower terraces are classified as Haplic Yellow-brown soils, corresponding to Eutric Cambisols (FAO-Unesco) or Dystric Eutrochrepts (USDA). The Argillic Latored soils. Agric Red soils and Haplic Yellow-brown soils date back to the middle Pleistocene, late Pleistocene and Holocene, respectively. It is also possible that the Argillic Latored soils were formed under a subtropical monsoon forest climate, the Agric Red soils under a southern warm-temperate lucidophyllus forest climate, and the Haplic Yellow-brown soils under the present northern warm-temperate deciduous broadleaved forest climate.     

中国土壤分类四十年

建国以来土壤分类是不断完善的过程。涉及全国的土壤分类系统至少有9个。可分为三个时期。解放初，采用美国马伯特土壤分类系统，以土类为基本单元，土系为基层单元，其中就有我国特有的山东棕壤、砂姜黑土和水稻土等类型；从1954年开始采用土壤发生分类系统，之后陆续提出了一些新土类，如黄棕壤、黑土、白浆土、砖红壤性红壤等，接着由于对耕地土壤的普查，充实了水稻土、明确了潮土、灌淤土和塍土等的独立土类地位。并提出了其他许多磷质石灰土等新土类。目前正在开始以诊断层如诊断特性为基础、结合我国丰富土壤类型的实际，在已有基础上，建立具有我国特色、具有空量指标的土壤系统分类。但这需要有一个较长的研究和完善过程。     

Erosion resistance of irrigated soils in the republic of Azerbaijan

It was found that the average size of water-stable aggregates in irrigated soils varies in the range 0.23–2.0 mm, and the eroding flow velocity is 0.03–0.12 m/s. A five-point scale was used for assessing erosion resistance, predicting irrigation erosion, and developing erosion control measures on irrigated soils. According to this system, gray-brown soils and light sierozems were classified as the least erosion-resistant, sierozemic and meadow-sierozemic soils as low erosion-resistant, gray-cinnamonic soils as moderately erosion-resistant, mountain gray-cinnamonic soils as highly erosion-resistant, and steppe mountain cinnamonic soils as very highly erosion-resistant ones. The determination of the erosion resistance of soils is of great importance for assessing the erosion-resistance potential of irrigated areas and developing erosion control measures.     

Morphogenetic features of soils in the Cat Tien National Park,southern Vietnam

Morphogenetic features of soils on the selected plots in the Cat Tien National Park in southern Vietnam have been studied with the use of a set of morphological, analytical, and instrumental methods. The lithological factor and topographic position play the leading role in the development of the particular genetic soil features. The soils can be subdivided into four groups according to these factors. The soils developing from volcanic deposits with a predominance of tephra can be classified as thin clayey brown tropical soils (Dystric Skeletic Rhodic Cambisols (Clayic)), and the soils developed from less weathered colluvial derivatives of basalts with some admixture of tephra can be classified as dark-humus clayey tropical soils (Skeletic Greyzemic Umbrisols (Clayic)). Very poor soils developed from the eluvium of argillites are classified as thin weakly developed clayey tropical soils (Dystric Regosols (Clayic)). The soils forming from the alluvial sediments of different textures are classified as alluvial loamy sandy soils (Dystric Fluvisols (Arenic, Drainic)) and as alluvial clay loamy soils (Eutric Fluvisols (Episiltic, Endoclayic)).     

Some factors affecting behaviour of boron in soil

It has been reported by many workers that various soil properties influence the retention of boron added to soils, but there is little infomration on the relative importance of these properties to boron retention and there is something controversial in the published results regarding the effects of different soil properties such as organic matter content, soil reaction, available calcium content and texture on boron retention (15). The present study was undertaken to obtain more detailed informations on the relationships between boron adsorption and different properties of soils, and on comparative contribution of soil constituents such as organic matter, sesquioxides and inorganic colloids to boron adsorption of soils. In Japan, boron deficiency symptoms of crops often appear in the fields of volcanic ash soils, and many experiments on boron application have been conducted to amend the boron deficiencies of the soils. It is considered that volcanic ash soils may have special characteristics concerning boron retention in comparison with nonvolcanic ash soils. In the present study, therefore, some volcanic ash soils were also taken as samples in addition to non-volcanic ash soils to confirm their speciality to boron retention.     

Influence of microbial inoculation (Pseudomonas sp. strain ADP), the enzyme atrazine chlorohydrolase,and vegetation on the degradation of atrazine and metolachlor in soil

The concentrations of atrazine in the freshly added soils and the soils that had been incubated for 50 days significantly decreased 1 day after the addition of the enzyme atrazine chlorohydrolase or the soil bacterium Pseudomonas sp. strain ADP as compared with those in the uninoculated soils. Atrazine chlorohydrolase or ADP had no effect on the degradation of metolachlor. The half-lives of atrazine in the freshly added soils and in the aged soils after the treatment with atrazine chlorohydrolase or ADP markedly decreased as compared with those in the uninoculated soils. The half-lives of metolachlor in the aged soils were much longer than those of freshly added metolachlor. The percentage atrazine degraded in the freshly treated soils was much higher than that in the aged soils. This indicates that aging significantly decreased the bioavailability of atrazine. Vegetation significantly decreased the concentration of metolachlor. However, vegetation showed no effect on the degradation of atrazine.     

氨基酸有机肥对棉花根际和非根际土壤酶活性和养分有效性的影响

在新疆石河子进行了2年不同氨基酸有机肥施用量的大田试验,测定棉花根际和非根际土壤酶活性和有效养分含量。结果表明,棉花根际土壤过氧化氢酶、蔗糖酶、磷酸酶、脲酶、纤维素酶活性高于非根际,且脲酶、纤维素酶活性达到显著差异。新陆早8号根际过氧化氢酶活性高于新陆早12号,但蔗糖酶、磷酸酶、脲酶、纤维素酶活性低于新陆早12号。根际碱解N呈显著降低,速效P呈增加趋势。膜下滴灌根际和非根际土壤过氧化氢酶、磷酸酶、脲酶、土壤pH及非根际的碱解N、速效P、根际的速效K较淹灌高,而土壤蔗糖酶、纤维素酶、根际碱解N、速效P、非根际的速效K较淹灌低。氨基酸有机肥对棉花根际和非根际土壤酶活性都有增加作用。土壤pH随着有机肥施用量的增加呈下降趋势,根际低于非根际。氨基酸有机肥增加了土壤碱解N、速效P、速效K含量。     

Characteristics and classification of three granite-derived soils in peninsular Thailand

The Phuket, Thung Wa and Huai Pong soils of this study form the Phuket catena and are extensive in Narathiwat province in the southern part of peninsular Thailand where they were studied in the field and sampled. The Phuket soils on the higher-lying positions and the Huai Pong soils on the nearly-level, lower positions, have developed argillic horizons and are Ultisols. The Thung Wa soils, which occur on intermediate positions and receive sediments from upslope, have cambic horizons and are classified as Inceptisols.All soils formed from Late Cretaceous or Early Tertiary granite or from sediments derived frome these granites under a tropical rain forest climate. They contain kaolinite as the predominant clay mineral and are highly leached, with base saturation of less than 35% in their B horizons. Cation exchange capacities are less than 6 mequiv. per 100 g soil and exchange acidity and exchangeable aluminium are high. Field and thin-section studies as well as particle-size analysis indicate considerable clay translocation from A to B horizons in the Phuket and Huai Pong soils and little clay movement in the Thung Wa soils.     

Vertical distribution of radiocesium in soils of the area affected by the Fukushima Dai-ichi nuclear power plant accident

Presented are results of the study of radiocesium vertical distribution in the soils of the irrigation pond catchments in the near field 0.25 to 8 km from the Fukushima Dai-ichi NPP, on sections of the Niida River floodplain, and in a forest ecosystem typical of the territory contaminated after the accident. It is shown that the vertical migration of radiocesium in undisturbed forest and grassland soils in the zone affected by the Fukushima accident is faster than it was in the soils of the 30-km zone of the Chernobyl NPP for a similar time interval after the accident. The effective dispersion coefficients in the Fukushima soils are several times higher than those for the Chernobyl soils. This may be associated with higher annual precipitation (by about 2.5 times) in Fukushima as compared to the Chernobyl zone. In the forest soils the radiocesium dispersion is faster as compared to grassland soils, both in the Fukushima and Chernobyl zones. The study and analysis of the vertical distribution of the Fukushima origin radiocesium in the Niida gawa floodplain soils has made it possible to identify areas of contaminated sediment accumulation on the floodplain. The average accumulation rate for sediments at the study locations on the Niida gawa floodplain varied from 0.3 to 3.3 cm/year. Taking into account the sediments accumulation leading to an increase in the radiocesium inventory in alluvial soils is key for predicting redistribution of radioactive contamination after the Fukushima accident on the river catchments, as well as for decision-making on contaminated territories remediation and clean-up. Clean-up of alluvial soils does not seem to be worthwhile because of the following accumulation of contaminated sediments originating from more contaminated areas, including the exclusion zone.