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1.
J.A. Díez P. Hernaiz M.J. Muñoz A. de la Torre A. Vallejo 《Soil Use and Management》2004,20(4):444-450
Abstract. The repeated application of pig slurry to agricultural soils may result in an accumulation of salts and a risk of aquifer pollution due to nitrate leaching and salinization. Under Mediterranean conditions, a field experiment on a sandy loam soil (Typic Xerofluvent) was performed with maize (Zea mays) in 1998, 1999 and 2001 to study the effects of applying optimal (P1) and excessive rates (P3) of pig slurry on soil salinization, nitrate leaching and groundwater pollution. The rate of pig slurry was established considering the optimal N rate for maize in this soil (170, 162 and 176 kg N ha?1 for 1998, 1999 and 2001, respectively). Pig slurry treatments were compared to an optimal N rate supplied as urea (U) and a control treatment without N fertilizer (P0). The composition of the slurries showed great variability between years. Mean NO3? leaching losses from 1998 to 2001 were 329, 215, 173 and 78 kg N ha?1 for P3, P1, U and P0 treatments, respectively. The amount of total dissolved salts (TDS) added to the soil in slurry application between 1998 and 2001 was 2019 kg TDS ha?1 for the P1 treatment and 6058 kg TDS ha?1 for the P3 treatment. As a consequence, the electrical conductivity (EC) of the slurry‐treated soils was greater than that of the control soil. The EC correlated significantly with the sodium concentration of the soil solution. Over the entire experimental period, 2653, 2202 and 2110 kg Na ha?1 entered the aquifer from the P3, P1 and P0 treatments, respectively. The P3 treatment did not significantly increase grain production in 1999 and 2001 compared with that achieved with the optimal N rate treatment (P1). This behaviour shows the importance of establishing application guidelines for pig slurry that will reduce the risk of soil and groundwater pollution. 相似文献
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Effects of cover crop growth and decomposition on the distribution of aggregate size fractions and soil microbial carbon dynamics 下载免费PDF全文
D. Linsler M. Kaiser R. Andruschkewitsch C. Piegholdt B. Ludwig 《Soil Use and Management》2016,32(2):192-199
Although the effects of cover crops (CC) on various soil parameters have been fully investigated, less is known about the impacts at different stages in CC cultivation. The objective of this study was to quantify the influence of CC cultivation stages and residue placement on aggregates and microbial carbon (Cmic). Additionally, the influence of residue location and crop species on CO2 emissions and leached mineralized nitrogen (Nmin) during the plant degradation period was also investigated. Within an incubation experiment, four CC species were sown in soil columns, with additional columns being kept plant‐free. After plant growth, the columns were frozen (as occurs in winter under field conditions) and then incubated with the plant material either incorporated or surface‐applied. With CC, concentrations of large and medium macroaggregates were twice that of the fallow, confirming positive effects of root growth. Freezing led to a decrease in these aggregate size classes. In the subsequent incubation, the large macroaggregates decreased far more in the samples with CC than in the fallow, leading to similar aggregate size distributions. No difference in Cmic concentration was found among the CC cultivation stages. CO2 emissions were roughly equivalent to the carbon amounts added as plant residues. Comparison of columns with incorporated or surface‐applied residues indicated no consistent pattern of aggregate distribution, CO2 emission or Cmic and Nmin concentrations. Our results suggest that positive effects of CC cultivation are only short term and that a large amount of organic material in the soil could have a greater influence than CC cultivation. 相似文献
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疏勒河灌区新垦盐碱地洗盐定额试 总被引:2,自引:0,他引:2
马德海 《中国农村水利水电》2007,(7):22-24
根据疏勒河灌区新垦盐碱地土壤含盐量高,需采用水平明沟排水冲洗改良的实际,开展了不同冲洗定额的洗盐效果试验研究,提出了排盐地区系数经验公式与冲洗定额对数函数计算公式。根据表层土壤含盐量高的特点,提出了以0~30cm土层作为冲洗改良盐碱地脱盐控制层的准则,并制定了相应的洗盐定额。 相似文献
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Esperanza Romero Francisco Snchez-Rasero Aranzazu Pea Clara de la Colina Gonzalo Dios 《Pest management science》1996,47(1):7-15
Adsorption, incubation and soil-column experiments with bentazone [3-isopropyl-1H-2,1,3-benzothiadiazin-4(3H)-one 2,2-dioxide] were carried out in ten different soils from the marches surrounding the Doñana National Park (Huelva, SW Spain). Adsorption isotherms for the different soils showed a good fit with the Freundlich equation. Bentazone was poorly adsorbed in all the soils studied, with no significant relationship between theKf values and soil characteristics. A significant correlation was obtained between the soil organic matter content and the distribution constant values (Kd) calculated at an equilibrium concentration of 200 μg cm−3. The low adsorption and non-degradation of bentazone on these soils suggest that the herbicide readily percolates through soils to reach the surface and ground waters. The mobility of bentazone through three soil columns was also studied. The mass balances carried out showed that bentazone was totally eluted from the soil columns. The theoretical model applied to explain bentazone leaching under our experimental conditions seems to be suitable for soil columns with a uniform water-flow rate. 相似文献
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The fate of fenpropimorph and its metabolite fenpropimorphic acid was investigated in a silty sand soil and in a clayey silt soil. In laboratory and field experiments fenpropimorph disappeared without a lag phase. A few days after application fenpropimorphic acid was detected. Additional laboratory experiments with [14C]fenpropimorph emphasized the significance of mineralization and the formation of non-extractable residues. The determination of soil/water distribution coefficients of parent compound and metabolite yielded a higher leaching potential for fenpropimorphic acid due to its higher polarity. This was confirmed by performing a laboratory column test under worst-case conditions. Under field conditions, however, fenpropimorphic acid was detected only in the superficial soil layers (0–5 cm) of both investigation sites at very low concentrations. 相似文献
10.
为明确改良剂在苏打盐化草甸土不同深度土层的改良效果,采用室内淋溶土柱的试验方法,设置S0、S1、S2、S3、S4和S5(每个土柱横截面积0.0113 m~2)分别施用改良剂0.00、0.01、0.05、0.10、0.50 g和1.00 g,折合成公顷用量分别为0.0、8.9、44.3、88.5、442.5 kg·hm~(-2)和885.1 kg·hm~(-2))6个处理,分析淹水条件下不同改良剂用量对苏打盐化草甸土的洗盐效应。结果表明,与未施改良剂处理(S0)相比,S3、S4和S5处理显著降低不同土层(0~30cm)土壤容重(降幅3.88%~8.87%)、增加土壤孔隙度(增幅3.82%~9.38%)、降低土壤pH值(降幅2.36%~8.05%);S2、S3、S4和S5处理显著提高20~40 cm土壤水分入渗量,增幅55.9%~294.6%(P0.05);施用改良剂处理交换性Na~+含量在0~10 cm和10~20 cm土层显著降低,降幅4.84%~56.5%(P0.05),20~30 cm和30~40 cm土层中增幅1.09%~17.1%;S3、S4和S5处理0~10 cm土层电导率显著降低,降幅49.0%~60.4%(P0.05),20~40 cm土层显著增加,增幅3.68%~19.8%(P0.05);S2、S3、S4、S5处理10~20 cm土层碳酸根含量显著降低,降幅5.98%~23.4%(P0.05),S3、S4、S5处理0~30 cm土层碳酸氢根含量降幅1.49%~18.0%;S2、S3、S4和S5处理显著提高0~30 cm≥0.25 mm水稳性团聚体,增幅达16.4%~161.7%(P0.05);S3、S4和S5处理0~30 cm土层MWD显著增加,增幅达5.78%~161.7%(P0.05)。针对本次供试土壤盐渍化程度,综合改良效果及改良剂施用量,改良剂适宜用量为每个土柱0.10 g(88.5 kg·hm~(-2))(S3处理),可达到最优淋洗效果。 相似文献