可降解地膜覆盖棉花增产效应的研究

田间试验结果表明 ,覆膜植棉可明显提高土壤温度 ,促进棉株生长 ,其 5cm土层土壤温度比露地栽培提高0 .1～ 2 .98℃ ,棉花产量提高 11.5 9%～ 18.31%。双解膜和光解膜在地膜降解前的增温效果略优于普通地膜 ,晴天增温幅度大于阴雨天。地膜降解诱导期过后 2种可降解地膜均顺利降解为面积较小碎片 ,而双解膜降解更快 ,缓解了农膜残留所造成白色污染。棉花生产可用可降解膜代替普通地膜 ,且需完善配套栽培技术。     

小麦和土壤中环丙唑醇残留消解动态及膳食摄入评估

为评价环丙唑醇在小麦生产上应用的安全性,通过建立乙腈提取、氮磷检测器检测方法对小麦籽粒、植株和土壤样品中环丙唑醇的残留量进行检测,研究了小麦籽粒、植株和土壤中环丙唑醇的残留及其消解动态,并对小麦中的残留量进行风险评估。结果表明,环丙唑醇在小麦籽粒、植株及土壤空白样品中的添加回收率为79.2%~95.6%,相对标准偏差为1.9%~10.0%,最小检出量为8.2×10?12 g,在小麦籽粒、植株及土壤中的最低检测浓度均为0.05 mg·kg?1,乙腈提取、氮磷检测器检测方法重现性好,准确度、精密度高,可满足环丙唑醇在小麦上的残留分析要求。2010年和2011年,河南省、黑龙江省和江苏省3地环丙唑醇在小麦植株和土壤中的消解半衰期分别为3.0~5.5 d、18.1~34.5 d;不同施药次数、施药量及采样间隔,环丙唑醇在小麦籽粒中的最终残留量均≤0.415 mg·kg?1。采收间隔期为14 d和21 d时,不同施药次数、施药剂量和采收间隔期,环丙唑醇在小麦植株、小麦籽粒和土壤中的残留量差异均不显著;采收间隔期为7 d,有效成分108 g?hm-2施药2次与有效成分162 g?hm-2施药3次时小麦植株、小麦籽粒和土壤中的残留量之间均存在显著性差异。普通人群环丙唑醇的国家估算每日摄入量为0.000 109 9 mg,占日允许摄入量的0.5%左右,按本试验方式进行施药,通常不会对一般人群健康产生不可接受的风险。     

油料作物和粮食作物种子中有机氯农药残留分析

为了调查作物种子中有机氯残留的现状和种子脂质含量与种子中有机氯残留的关系,本文通过GC-ECD对某农产品基地的油料作物花生、大豆、芝麻和粮食作物水稻、小麦、玉米种子中有机氯农药残留进行了分析.结果表明,对照WHO/FAO标准,6种作物种子中的滴滴涕(DDT)和六六六(HCH)残留均不超标;总DDT的残留范围是3.8～10.3 ng/g,残留顺序是花生>芝麻>大豆>玉米>小麦>水稻;总HCH的残留范围是4.3～10.7 ng/g,残留顺序是花生>玉米>芝麻>大豆>小麦>水稻.3种油料作物种子中的总DDT残留浓度显著高于3种粮食作物种子中的残留浓度,种子中的总DDT残留浓度与种子脂质含量的对数显著正相关.     

阿灭净在菠萝与土壤中的残留及消解动态研究

采用气相色谱(GC-NPD)分析技术测定除草剂阿灭净在菠萝与土壤中的残留及消解动态结果表明,GC-NPD方法的最小检出量为0.0232ng,菠萝及土壤的最小检出浓度分别为0.002mg/kg和0.005mg/kg,GC-NPD方法回收率分别为87.23%~92.10%和88.80%~93.77%。喷施阿灭净80%WP4800g(a.i/)hm2,处理检测出菠萝与土壤中原始沉积量分别为0.1448~0.1646mg/kg和3.3318~3.5536mg/kg,消解半衰期分别为29.17~29.45d和25.75~30.68d,按阿灭净用量4800g(a.i/)hm2施药菠萝1次,间隔期为10d,菠萝果实残留量2年分别为0.1646mg/kg和0.1448mg/kg,参照欧共体的MRL值0.2mg/kg,按上述阿灭净剂量方法施用菠萝是安全的。     

Long-term impact of reduced tillage and residue management on soil carbon stabilization: Implications for conservation agriculture on contrasting soils

Residue retention and reduced tillage are both conservation agricultural management options that may enhance soil organic carbon (SOC) stabilization in tropical soils. Therefore, we evaluated the effects of long-term tillage and residue management on SOC dynamics in a Chromic Luvisol (red clay soil) and Areni-Gleyic Luvisol (sandy soil) in Zimbabwe. At the time of sampling the soils had been under conventional tillage (CT), mulch ripping (MR), clean ripping (CR) and tied ridging (TR) for 9 years. Soil was fully dispersed and separated into 212–2000 μm (coarse sand), 53–212 μm (fine sand), 20–53 μm (coarse silt), 5–20 μm (fine silt) and 0–5 μm (clay) size fractions. The whole soil and size fractions were analyzed for C content. Conventional tillage treatments had the least amount of SOC, with 14.9 mg C g⁻¹ soil and 4.2 mg C g⁻¹ soil for the red clay and sandy soils, respectively. The highest SOC content was 6.8 mg C g⁻¹ soil in the sandy soil under MR, whereas for the red clay soil, TR had the highest SOC content of 20.4 mg C g⁻¹ soil. Organic C in the size fractions increased with decreasing size of the fractions. In both soils, the smallest response to management was observed in the clay size fractions, confirming that this size fraction is the most stable. The coarse sand-size fraction was most responsive to management in the sandy soil where MR had 42% more organic C than CR, suggesting that SOC contents of this fraction are predominantly controlled by amounts of C input. In contrast, the fine sand fraction was the most responsive fraction in the red clay soil with a 66% greater C content in the TR than CT. This result suggests that tillage disturbance is the dominant factor reducing C stabilization in a clayey soil, probably by reducing C stabilization within microaggregates. In conclusion, developing viable conservation agriculture practices to optimize SOC contents and long-term agroecosystem sustainability should prioritize the maintenance of C inputs (e.g. residue retention) to coarse textured soils, but should focus on the reduction of SOC decomposition (e.g. through reduced tillage) in fine textured soils.     

Characterization of core collection of lentil germplasm for phenology, morphology, seed and straw yields

Increasing and maintaining crop residues in predominantly cereal-based rotations of the US Pacific Northwest is critical to controlling soil erosion. The core collection of lentil (Lens culinaris Medik.) germplasm comprising 287 accessions was evaluated for variation in phenological, morphological and growth parameters including seed yields and residue amounts over a two-year period under conventional tillage and no-till conditions. The objectives of this study were (i) assess lentil genetic variation in germplasm for variation in biomass production and seed yield, (ii) assess the relationship of phenological and morphological traits with biomass and seed yield and (iii) identify high biomass producing germplasm for use as parents in the breeding program. Days to flowering and days to maturity ranged from 31 to 78 and from 71 to 106 days, respectively. Time to flowering in terms of cumulative heat units was a more efficient measurement than days to flowering. Plant height and plant canopy width had a significant association with total biomass, seed yield and residue amounts. Total biomass ranged from 788–6389 kg ha^–1 under conventional tillage, while the range under no-till conditions was 1045–6195 kg ha^–1. Most of the lines with higher biomass also produced the highest seed yields and residue amounts. Overall, only one accession produced more residue than `Laird'. In the more favorable environment of 1997, six accessions exceeded the control cultivars, `Laird' and `Indianhead', for residue amounts, and seven and twenty-four accessions exceeded control cultivars, `Pardina' and `Brewer', for seed yield. Results indicated that plant height, canopy width at maturity and seed yield explained most of the variation in biomass and residue production. Large seeded germplasm consistently had a longer reproductive growth period than small seeded accessions and had 17%, 7% and 21% more biomass, seed yield and residue, respectively. Our data indicated significant variation in lentil germplasm for biomass, seed yield and residue amounts to warrant their use in the breeding program.     

Recovering decomposing plant residues from the particulate soil organic matter fraction: size versus density separation

 A detailed size separation of particulate organic matter (POM) from soils amended with straw from Hordeum vulgare or Vicia sativa revealed that the loss of C during the first 56 days of incubation mainly occurred from particles >2,000 μm, without a concomitant reduction in the size of these large particles. Preliminary studies of POM from non-amended soil had shown that the stable heavy (>1.4 g cm^–3) POM fraction was mainly (>80%) composed of particles <400 μm, whereas the light fraction was dominated by larger particles (>80%). Therefore we decided to compare the POM <1.4 g cm³ with POM >400 μm. There was a very close relationship between POM>400 μm and POM <1.4 g cm^–3 with regard to amounts of C and N, as well as the appearance of these fractions under the microscope. Similarly there was a close relationship between changes in the C content of the POM fractions and the CO₂ respired, and this was also the case when comparing changes in POM-N with net N mineralization. This indicated that the biological activity during decomposition was actually localized in the POM. Due to the lighter workload and lower expenditure for reagents in connection with size separation of POM, we recommend the size separation procedure in connection with studies of residue decomposition in arable systems. Received: 23 May 2000     

Biomass production and related characters in the core collection of Pisum germplasm

Retention of residue on the soil surface following harvest is an effective method of reducing soil erosion from both wind and water. The pea crop produces small amounts of residue to effectively reduce soil erosion. Severe erosion occurs in pea production areas such as the Palouse Region of the US Pacific Northwest (PNW) when low residue crops such as spring pea or lentil are followed by fall-sown wheat. The current study was conducted to determine the range of total aboveground biomass (TAB), seed yield, and straw (residue) production from the plant identification (PI) accessions that comprise the core collection of Pisum germplasm. In addition, the potential for increasing seed yield and straw production simultaneously was evaluated. Three hundred and ninety PI accessions were screened in the field in 1996 and 1997. The variation for TAB, seed yield and straw production among the PI accessions exceeded that of the controls both years. Seed yield was positively correlated with straw production (r = 0.81, p< 0.01) indicating that seed and straw production can be increased simultaneously through positive selection for both traits. Significant favorable variation is present among accessions in the USDA core collection of Pisum germplasm which could be used to increase both seed yield and total biomass production of adapted breeding lines.     

Influence of wheat residue management on irrigated corn grain production in a reduced tillage system

Management of wheat (Triticum aestivum L.) residues for corn (Zea mays L.) planting is an important issue in southern parts of Iran where these two irrigated crops are consecutively grown. Concerns have been raised in recent years over the burning of the crop residues by farmers in these areas. A 2-year (2001–2002) field experiment was conducted as a randomized complete block design with three replications. The treatments consisted of irrigated corn planted, after burning wheat residues followed by conventional tillage (CT), after residue removal followed by CT, after soil incorporation of 0, 25, 50, 75, and 100% of residue followed by chisel plow, disk harrow, and row crop planter equipped with row cleaner. The CT operations consisted of mollboard plowing followed by two times disk harrowing. Treatments had significant effects on corn grain yield, biological yield, and leaf area index. The highest grain yield (15.73 t ha⁻¹) and grains per ear (709.3) were obtained when 25–50% of wheat residues were soil incorporated and the seeds were sown with planter equipped with row cleaner in both years as compared with conventional tillage practices. It is recommended that complete residue removal or burning should be avoided; hence for successful corn production after wheat, residue management techniques that reduce residue level in the row area should be implemented.     

The effects of long-term conservation tillage, crop residues and P fertilizer on soil conditions and responses of summer and winter crops on an Andosol in Japan

A field experiment was conducted from 1983 to 1992 in Tsukuba, Japan to investigate the effects of tillage on soil conditions and crop growth in a light-colored Andosol. Three tillage methods (NT: no-tillage, RT: no-tillage for summer cropping and moldboard plowing for winter cropping, and CT: conventional rotary tillage to a depth of 15 cm) were employed in combination with crop residue application (+R, −R) and fused magnesium phosphate (FMP) fertilization (+P, −P). Under the combination of NT and +R, diurnal variation of soil temperature at a depth of 5 cm was smaller during the summer cropping season and soil temperature in the daytime was lower during the winter cropping season than under CT. Soil inorganic N concentration at a depth of 0–30 cm was +R > −R and NT > RT > CT. The early growth of summer crops was accelerated under NT in comparison with CT, and yields were higher under NT and RT in comparison with CT. On the other hand, winter crop yields were significantly reduced under NT, while they were still higher under RT in comparison with CT. Yields were higher with +R and +P application, respectively, and these effects were more pronounced in winter cropping. The positive effect of FMP fertilization was greater in combination with NT, and that of residue treatment was greater in combination with RT and NT than with CT. In conclusion, the best tillage practice for Andosols on the Kanto Plain is RT, i.e. a combination of NT for summer cropping and CT for winter cropping. The application of NT for winter cropping is not recommended, although the application of phosphate and crop residues could reduce the risk of yield reduction, because of improved soil nutrient status and moderation of diurnal soil temperature.