Simulation of drainage water quality with DRAINMOD

The design and management of drainage systems should consider impacts on drainage water quality and receiving streams, as well as on agricultural productivity. Two simulation models that are being developed to predict these impacts are briefly described. DRAINMOD-N uses hydrologic predictions by DRAINMOD, including daily soil water fluxes, in numerical solutions to the advective-dispersive-reactive (ADR) equation to describe movement and fate of NO₃-N in shallow water table soils. DRAINMOD- CREAMS links DRAINMOD hydrology with submodels in CREAMS to predict effects of drainage treatment and controlled drainage losses of sediment and agricultural chemicals via surface runoff. The models were applied to analyze effects of drainage intensity on a Portsmouth sandy loam in eastern North Carolina. Depending on surface depressional storage, agricultural production objectives could be satisfied with drain spacings of 40 m or less. Predicted effects of drainage design and management on NO₃-N losses were substantial. Increasing drain spacing from 20 m to 40 m reduced predicted NO₃-N losses by over 45% for both good and poor surface drainage. Controlled drainage further decreases NO₃-N losses. For example, predicted average annual NO₃-N losses for a 30 m spacing were reduced 50% by controlled drainage. Splitting the application of nitrogen fertilizer, so that 100 kg/ha is applied at planting and 50 kg/ha is applied 37 days later, reduced average predicted NO₃-N losses but by only 5 to 6%. This practice was more effective in years when heavy rainfall occurred directly after planting. In contrast to effects on NO₃-N losses, reducing drainage intensity by increasing drain spacing or use of controlled drainage increased predicted losses of sediment and phosphorus (P). These losses were small for relatively flat conditions (0.2% slope), but may be large for even moderate slopes. For example, predicted sediment losses for a 2% slope exceeded 8000 kg/ha for a poorly drained condition (drain spacing of 100 m), but were reduced to 2100 kg/ha for a 20 m spacing. Agricultural production and water quality goals are sometimes in conflict. Our results indicate that simulation modeling can be used to examine the benefits of alternative designs and management strategies, from both production and environmental points-of-view. The utility of this methodology places additional emphasis on the need for field experiments to test the validity of the models over a range of soil, site and climatological conditions.     

斜板上流式厌氧污泥床处理低浓度有机废水的试验研究

本文报告了用１６．１升斜板上流式厌氧污泥床在常温下处理低浓度有机废水的启动和运行试验研究。试验使用稀释酒精废水为模拟处理基质，启动阶段仅用７７天时间，装置水力负荷达到２ｍ３／（ｍ３．ｄ），ＣＯＤ去除率达到７８．９％，此时进水ＣＯＤ浓度为７６７．８ｍｇ／Ｌ。在第二阶段试验中，仅用一天时间，装置就恢复了时隔半年的正常运行。以后在温度１２℃以上，ＨＲＴ为１２小时，进水ＣＯＤ浓度在６６０．０～９８２．０ｍｇ／Ｌ范围的１２９天稳定运行中，平均ＣＯＤ去除率为７６．１％。结果表明：采用该工艺处理低浓度有机废水在技术上是可行的，具有启动快，运行稳定，工艺控制简便的优点。水浸没的成组浅层斜板在ＵＡＳＢ／ＩＴＳ反应器中有良好的污泥截留能力和稳流效果，容易生成大颗粒污泥。颗粒污泥最大粒径可达５ｍｍ，ＳＶＩ为１８．２ｍｌ／ｇ。颗粒污泥中以甲烷丝菌为优势菌。     

肥料结构对红壤性水稻土氮磷钾养分状况的影响

本文论述了三种肥料结构对红壤性水稻土氮磷钾养分状况的影响。土壤中的生物学有效性氮、氨基酸态氮、氨基酸、速效磷和活性有机磷的含量变化趋势是,以作物残体+灶灰+猪粪+化肥处理>作物残体+灶灰+化肥处理>绿肥+化肥处理。在各处理中,土壤中速效钾和缓效钾的含量变化不大,但采取秸杆、灶灰、菜籽饼和猪粪还田的措施,在节约化学钾肥提高作物产量中起了良好作用。     

改性木质素对砖红壤磷素有效性的影响

磷肥施入砖土壤后，土壤速效磷随着时间的推移，呈现下降的趋势。利用改性木质素缓释磷铵，可以有效地络合土壤活性钵，降低其活性，从而阻止土壤速效磷被固定，使土壤磷素维持在较高的水平。土壤中交换性钙和交换性镁对土壤速效磷的影响不大。     

饲用复合酶对蛋用种鸡日粮磷的利用和生产性能的影响

本试验旨在研究低磷日粮添加复合酶制剂对蛋用种鸡磷的利用和生产性能的影响。选用972只24周龄罗曼褐父母代种鸡,分为3个处理,每处理6个重复,每重复54只种鸡。采用玉米-豆粕-杂粕型基础饲粮,正对照组含总磷0.55%,非植酸磷0.40%,不加酶;负对照组含总磷0.40%,非植酸磷0.21%,不加酶;试验组含总磷0.40%,非植酸磷0.21%,加酶制剂。试验期18周。结果表明:在低非植酸磷的日粮中添加复合酶,粪便中磷含量极显著低于正对照组(P<0.01);粪便中粗蛋白质含量显著低于正对照组和负对照组(P<0.05);显著改善蛋黃顔色(P<0.05);不影响生产性能、骨骼发育和蛋壳质量。添加200 g/t复合酶替代罗曼褐蛋用种鸡日粮中75%的磷酸氢钙能够降低饲料成本,提高养殖企业的经济效益,对罗曼褐蛋用种鸡生产性能无不利影响。     

典型旱作农田土壤氧化亚氮排放的氨氧化微生物相对贡献

氨氧化过程对氧化亚氮（N2O）排放具有重要贡献。在不同土壤类型和农田管理下,氨氧化微生物类群对N2O排放的相对贡献组成规律还缺乏系统的研究。本研究选取典型农田耕层土壤（潮土、黑土、砖红壤）,以及有机肥改良的砖红壤剖面土壤,采用选择性抑制法（乙炔和辛炔）研究氨氧化细菌（AOB）、氨氧化古菌和全程硝化菌（AOA+comammox）以及异养硝化菌对土壤硝化潜势、净硝化速率及N2O排放的相对贡献。结果表明,在耕层土壤中,潮土、黑土和砖红壤的pH分别是8.0、6.7和5.7,硝化潜势分别是N 32.5、6.6和4.8 mg?kg-1?d-1,净硝化速率分别是N 7.1、3.0和0.5 mg?kg-1?d-1,7天N2O累积排放量分别是N 38.0、35.4和8.7 μg?kg-1。AOB主导耕层土壤的硝化潜势,对硝化潜势的贡献分别是82%、58%和100%。对于净硝化速率,在潮土和砖红壤中,AOB和AOA+comammox贡献相当（均在30%~40%）,而黑土中由AOB主导（72%）。AOB主导耕层土壤的N2O排放,对N2O排放的贡献分别是72%、92%和58%。在改良的砖红壤剖面土壤中,在0~20 cm、20~40 cm和40~60 cm,pH分别是7.0、5.5和4.9,硝化潜势分别是N 6.6、2.0和1.1 mg?kg-1?d-1,净硝化速率分别是N 4.1、0.9和0.2 mg?kg-1?d-1,N2O排放分别是N 16.3、6.5和2.8 mg?kg-1?d-1。随土壤由深层至表层,硝化潜势、净硝化速率及N2O排放显著提高。AOA+comammox主导表层硝化潜势及净硝化速率的提高（分别贡献63%和54%）,AOB主导N2O排放的增加（贡献54%）。本研究为制定与土壤氨氧化特性及土壤性质相匹配的N2O减排措施提供了新的科学依据。     

‘鸭梨’、‘新高’果实发育过程中果肉及种子有机酸含量的变化

为了研究梨种子对果实生长发育的影响,采用高效液相色谱(HPLC)技术对‘鸭梨’和‘新高’果实发育过程中果肉和种子中的有机酸含量进行了分析。结果表明：两个品种果肉中主要的有机酸组分均为苹果酸和奎尼酸,发育初期‘鸭梨’与‘新高’果肉中各组分的比率相近,但果实成熟时‘新高’果肉中苹果酸的比率59.98%显著高于‘鸭梨’的37.51%;两个品种种子中的有机酸组分比率的动态变化相近,与果肉相反,主要表现在奎尼酸比率的增加和苹果酸比率的减少。两个品种果肉和种子中的总酸、草酸、奎尼酸,苹果酸,莽草酸,柠檬酸含量均随着果实的成熟呈下降趋势,‘鸭梨’果肉中的奎尼酸、莽草酸、柠檬酸含量高于‘新高’;‘新高’在果实成熟时种子中的总酸含量4.59mg/g显著低于‘鸭梨’13.00mg/g,‘鸭梨’成熟果实种子中的草酸、奎尼酸、莽草酸含量显著高于‘新高’;在果实发育初期,种子中的苹果酸含量极显著高于果肉,在果实成熟时则显著低于果肉。     

茭虾共作对土壤氮磷含量和茭白干物质积累及氮磷钾吸收分配的影响

为探究茭白种养模式的施肥策略,设置茭虾共作（ZC）、茭白单作（Z） 2个处理,研究茭虾共作对土壤氮磷含量、茭白产量和茭白干物质积累及氮磷钾吸收分配的影响。2021-2022年的研究结果显示,茭虾共作模式较茭白单作模式采茭期土壤中全氮、全磷、速效磷的含量分别提高了10.85%~38.89%、5.45%~13.79%、6.19%~61.79%,净茭产量提高了5.10%~19.54%,采茭期茭白茎、叶、净茭的干物质积累量分别增加14.41%~16.58%、10.28%~15.15%、10.57%~21.45%。2021年茭虾共作处理较茭白单作处理在采茭期叶的氮含量显著增加了25.74%,但在孕茭期茎中磷含量显著减少了16.76%;2022年氮肥减量、减量投喂下,茭虾共作处理较茭白单作处理在孕茭期茎的氮含量显著减少了23.75%,在分蘖期叶中磷含量显著减少了12.08%,2 a全生育期同一器官的钾含量在2个处理间差异不显著。对于养分积累,2021年茭虾共作处理在分蘖期叶的氮、磷、钾积累量较茭白单作处理分别减少26.04%、27.27%、30.11%,但在采茭期茎的氮、钾积累量和叶的氮、磷积累量较茭白单作处理分别增加18.80%、38.41%和44.77%、35.71%;2022年在氮肥减量、饲料减量投喂下,茭虾共作处理在采茭期叶的磷积累量和茎的钾积累量较茭白单作处理显著增加30.0%和30.77%。关于养分分配,2种处理的茭白在孕茭期和采茭期氮素的分配均以茎、叶为主,而磷、钾元素的分配均以茎为主,茎分配比例在42%~66%。对于养分转运,2021年2种处理茭白的根、茎、叶在氮、磷转运上大多为表现为“库”器官,而在钾转运上大多表现为“源”器官;2022年氮肥减量、减量投喂下,茭白的根、茎、叶在氮、磷、钾转运量上大多表现为“源”器官。因此,在茭虾共作模式中适当减少肥料、饲料的投入,能促进形成合理的源库关系,有利于茭白产量的形成。     

Potential chemical time bombs in the schelde estuary

The Schelde estuary is heavily polluted with many different (micro)pollutants. This results in high concentrations in the abiotic and biotic compartments of the Schelde estuary and in various effects. the present day suboxic and anoxic conditions in the upper estuary are probably responsible for the high distribution coefficients for some trace metals in the lower Schelde estuary (Western Schelde). a future reduction in discharges with a high biological oxygen demand will therefore not only result in higher oxygen concentrations, but probably also in lower distribution coefficients for trace metals in the Western Schelde. Simulations show that lower trace metal distribution coefficients will probably result in higher concentrations of dissolved (bioavailable) trace metals, even with substantially reduced discharge rates, due to the desorption of trace metals from resuspended bottom sediments.     

不同有机肥用量对黄瓜生长及养分吸收的影响

在温室基质栽培条件下,研究了配施等量化肥时不同用量有机肥对黄瓜生长及养分吸收的影响。试验采用有机肥系烘干鸡粪,所有供试肥料均以底肥形式一次施入。研究结果表明,高量有机肥处理(有机肥50,100 kg/m3)严重抑制了黄瓜定植初期的生长,黄瓜前期产量也明显低于不施或低量有机肥处理。随着施肥量的增加,黄瓜氮、磷、钾养分吸收量均显著增加。黄瓜定植后74 d,所有处理基质的速效氮养分均已处于极低的水平,黄瓜普遍出现缺肥症状。试验初步证明了长季节栽培条件下一次施用高量有机肥难以及时提供足量的速效氮源,无法满足蔬菜养分需求。