Do cover crops change the lability of phosphorus in a clayey subtropical soil under different phosphate fertilizers?

Plants have developed different mechanisms to absorb and solubilize phosphorus (P) in the soil, especially in environments with low P availability. This study evaluated the effects of different winter cover crops on soil P availability in a clayey subtropical (Hapludox) soil receiving soluble P fertilizer and a rock phosphate applied to the summer crop, under no‐tillage. The experiment was carried out over 3 yrs (2009–2011) with five different cover crop species: common vetch, fodder radish, ryegrass, black oat, white clover and fallow as control. The soil was sampled after the third year of cover crop cultivation and analysed for inorganic and organic P forms according to the well‐established Hedley fractionation procedure. Phosphate fertilizers promoted accumulation of both labile and nonlabile P pools in soil in the near surface layer, especially under rock phosphate. Fertilizer applications were not able to change P fractions in deeper layers, emphasizing that the Brazilian clayey soils are a sink of P from fertilizer and its mobility is almost nil. Although the cover crops recycled a great amount of P in tissue, in a short‐term evaluation (3 yrs) they only changed the content of moderately labile P in soil, indicating that long‐term studies are needed for more conclusive results.     

不同培养条件对鲍鱼菇菌丝生长的影响

通过不同温度、pH值及培养基含水量处理 ,对鲍鱼菇菌丝生长状况进行了研究。结果表明鲍鱼菇菌丝生长适宜的温度范围为 2 0～ 31℃ ,最适温度为 2 5～2 8℃ ;pH值适宜的范围为 4 0～ 7 0 ,最适pH值为 5 5～6 0 ;培养基含水量适宜的范围为 6 0 %～ 80 % ,最适含水量为 80 %。     

Oxygen isotope ratios of plant available phosphate in lowland tropical forest soils

Phosphorus (P) cycles rapidly in lowland tropical forest soils, but the process have been proven difficult to quantify. Recently it was demonstrated that valuable data on soil P transformations can be derived from the natural abundance of stable oxygen isotopes in phosphate (δ¹⁸O_P). Here, we measured the δ¹⁸O_P of soils that had received long-term nutrient additions (P, nitrogen, and potassium) or litter manipulations in lowland tropical forest in Panama and performed controlled incubations of fresh soils amended with a single pulse of P. To detect whether δ¹⁸O_P values measured in the incubations apply also for soils in the field, we examined the δ¹⁸O_P values after rewetting dry soils. In the incubations, resin-P δ¹⁸O_P values converged to ∼3.5‰ above the expected isotopic equilibrium with soil water. This contrasts with extra-tropical soils in which the δ¹⁸O_P of resin-P matches the expected equilibrium with soil water. Identical above-equilibrium resin-P δ¹⁸O_P values were also found in field soils that did not receive P additions or extra litter. We suggest that the 3.5‰ above-equilibrium δ¹⁸O_P values reflect a steady state between microbial uptake of phosphate (which enriches the remaining phosphate with the heavier isotopologues) and the release of isotopically equilibrated cell internal phosphate back to the soil. We also found that soil nutrient status affected the microbial turnover rate because in soils that had received chronic P addition, the original δ¹⁸O_P signature of the fertilizer was preserved for at least eight weeks, indicating that the off-equilibrium δ¹⁸O_P values produced during microbial phosphate turnover was not imprinted in these soils. Overall, our results demonstrate that ongoing microbial turnover of phosphate mediates its biological availability in lowland tropical soils.     

卵叶青藓水提液对玉米种子萌发和幼苗生长的影响

为了解卵叶青藓可能具有的化感效应及其作用机制,以卵叶青藓配子体水提取液为处理液,以玉米种子为受试对象,通过测定不同浓度梯度卵叶青藓水提液对受试种子萌发及幼苗生长的影响,初步阐明卵叶青藓可能具有的化感潜能.结果表明:卵叶青藓配子体水提液对玉米种子发芽率有较大影响,且总体趋势表现为提取液浓度愈高,对其种子萌发率影响愈大,处理组玉米种子萌发率显著低于对照组(p＜0.05);卵叶青藓水提液对玉米幼苗生长的影响表现在对苗高与根长的抑制方面.随着水提液浓度的增高,玉米幼苗根长逐渐变短,在80 mg/mL处理下达到最短,且与对照间差异显著(p＜0.05);对玉米幼苗根部发育状况有较强的影响,即随着水提液浓度的提高,生根数目逐步减少,直至浓度为80 mg/mL时达到最少.实验中,玉米幼苗鲜重及干重均随着提取液浓度的升高而减小,尤其是幼苗于重,在提取液浓度达到40 mg/mL时达到最小.随卵叶青藓提取液浓度不断增高,玉米幼苗叶片总叶绿素含量和叶绿素a含量逐步下降,均在80 mg/mL时达到最低,而叶绿素b在5 mg/mL时反而略高于对照组,在10 mg/mL时达到最低.上述结果表明,卵叶青藓具有一定的化感潜能.     

除虫菊地上部分水浸液对杂草种苗生长的影响

采用室内培养皿法,测试除虫菊地上部分水浸液对田间常见6种杂草种苗生长的影响。结果表明:不同质量浓度水浸液对杂草种苗生长的抑制作用依质量浓度梯度存在差异,除播娘蒿外其他5种总体均表现"低促高抑"趋势,在最高质量浓度0.03g·mL-1处理下,抑制作用最强;杂草种苗所受抑制作用大小依受体杂草种类存在差异,总体抑制作用由大到小依次为播娘蒿泽漆雀麦婆婆纳反枝苋野燕麦;除虫菊地上部分水浸液对试验杂草生理代谢影响测试表明,高质量浓度水浸液处理下,杂草幼苗受氧化胁迫严重。双子叶杂草较单子叶杂草对水浸液更敏感。     

长期施肥下黄土旱塬黑垆土磷平衡及农学阈值

为研究长期施肥条件下土壤磷平衡和土壤有效磷对磷盈亏的响应,明确土壤有效磷(Olsen-P)的农学阈值及合理磷肥施用量,依托甘肃平凉肥料长期定位试验(始于1979),分析了黄土旱塬黑垆土36 a土壤磷盈亏动态、累积磷盈亏与有效磷的响应关系以及土壤磷残余,通过Mitscherlich方程模拟作物相对产量对土壤有效磷的响应关系,计算黄土旱塬黑垆土小麦和玉米的土壤有效磷农学阈值。结果表明:不施肥(CK)和单施氮肥(N)处理土壤磷始终亏缺,N处理每亏缺磷100 kg·hm~(-2),有效磷含量下降1.05 mg·kg~(-1);施磷处理土壤磷当季盈余4.3～207.9 kg·hm~(-2),累积盈余154.9～7 483.6 kg·hm~(-2),其中有机、无机配施(MNP)处理磷盈余最大;土壤累积磷盈余与土壤有效磷增量呈线性正相关,土壤中每盈余100 kg·hm~(-2)磷,秸秆还田配施化肥(SNP,磷肥隔年施)、氮磷配施(NP)、有机肥(M)和有机、无机配施(MNP)处理土壤有效磷分别增加7.55、2.47、0.28 mg·kg~(-1)和0.46 mg·kg~(-1);黄土旱塬黑垆土农田有效磷的小麦和玉米农学阈值分别为22.05 mg·kg~(-1)和13.96 mg·kg~(-1),MNP处理土壤有效磷含量已高于作物农学阈值,NP和SNP处理土壤有效磷含量达到小麦农学阈值分别需要21 a和24 a,达到玉米农学阈值分别需要2 a和8 a,M处理土壤有效磷含量已高于玉米农学阈值,还需要3 a可达到小麦农学阈值。当磷投入量每年平均达22.9 kg·hm~(-2)时,土壤磷呈持平状态;当磷用量达33 kg·hm~(-2)时,不仅作物产量较高,而且磷肥当季利用率也较高;当磷用量增加到233 kg·hm~(-2)时,作物产量对增加磷投入无响应,土壤磷残余超过90%,大量磷素累积在土壤中,增加了土壤磷素的流失风险。黄土旱塬小麦玉米一年一熟轮作黑垆土农田土壤有效磷农学阈值为13.96 mg·kg~(-1)(玉米)和22.05 mg·kg~(-1)(小麦),秸秆还田可促进旱地农田耕层土壤有效磷含量的增加。     

华南地区主要蔬菜磷钾肥料利用率研究现状

总结了近年来在华南地区主要蔬菜生产区进行的田间试验结果,分析了施磷钾肥对叶菜、瓜类、豆类蔬菜产量和养分吸收的影响,以及目前条件下华南地区蔬菜磷钾肥的偏生产力、农学效率、肥料表观利用率、生理利用率、肥料贡献率和地力贡献率。结果表明,叶菜、瓜类和豆类蔬菜施用磷钾肥均能促进蔬菜产量的增加和磷钾养分的吸收。叶菜、瓜类、豆类蔬菜磷肥偏生产力分别为781.9 kg/kg、257.6 kg/kg、211.9 kg/kg,农学效率为30.5 kg/kg、64.1 kg/kg、23.1 kg/kg,表观利用率为17.2%、9.7%、6.1%,生理利用率为222.3 kg/kg、370.6 kg/kg、292.7kg/kg,肥料贡献率为16.4 %、19.4%、12.9%,地力贡献率为83.6 %、80.4%、87.1%。叶菜、瓜类、豆类蔬菜钾肥偏生产力分别为298.8 kg/kg、164.3 kg/kg、165.8 kg/kg,农学效率为29.5 kg/kg、39.5 kg/kg、25.8 kg/kg,表观利用率为24.8%、24.3%、13.0%,生理利用率为152.3 kg/kg、218.6 kg/kg、229.1kg/kg,肥料贡献率为13.8 %、21.6%、17.4%,地力贡献率为86.2 %、78.3%、82.6%。分析肥料利用率分布频率可以看出,磷肥表观利用率＜20%的试验样本和钾肥表观利用率＜30%的试验样本均占总样本的80%以上,表明目前试验条件下各类蔬菜的磷钾肥利用率较低,生产上需同时解决蔬菜产量及肥料利用效率提高的问题。     

磷酸铵镁堆肥产品养分释放特性及其肥效研究

为了研究磷酸铵镁堆肥产品的氮磷养分释放特性及其肥效,分别采用土柱淋溶方法及盆栽试验研究了磷酸铵镁堆肥(MAPC)产品的氮磷养分释放特性及对油菜的肥效,并与普通化肥(CCH)、普通堆肥(CCO)、磷酸铵镁肥(MAP)3种肥料进行对比。结果表明:在整个淋溶过程中,CCH和MAPC处理淋溶液的总氮及总磷浓度均较其他处理高;MAP肥具有缓释性,且堆肥对其养分释放具有促进作用;CCO处理的养分释放最慢。在最后一次淋洗(即第5次)后,总氮及总磷养分浓度排序均为:CCHMAPCMAPCCO。盆栽试验18 d后油菜快速生长,且与对照(不施肥)处理相比,MAP和MAPC处理能显著提高油菜的株高及生物量。在45 d盆栽试验结束时,CCH、CCO、MAP和MAPC处理的生物量分别是对照处理的14.8、4.8、20.5倍和16.0倍。MAP处理能显著提高油菜的养分含量,TN和TP含量分别比对照提高了2.24 g·kg~(-1)和1.54 g·kg~(-1)。研究表明,4种肥料均可改善油菜的生长发育情况,且MAP和MAPC的肥效优于CCH和CCO,在堆肥中利用鸟粪石结晶原理可固定部分氮磷元素,提高堆肥产品肥效。     

硒肥与钝化材料组配对土壤Cd钝化及稻米Cd消减效果

为了探讨不同硒肥施用方式联合钝化材料对土壤镉钝化和稻米镉消减的效果,采用盆栽试验的方式,选用亚硒酸钠作为硒肥,钙镁磷肥和硅藻土作为钝化材料,设置基施硒肥+钙镁磷肥+硅藻土和叶面喷施硒肥+钙镁磷肥+硅藻土2种方式,研究其不同用量对镉污染酸性稻田土壤修复与安全利用的影响。结果表明：随着施用量的增加,稻米产量增加,基施硒肥产量略高于叶面喷施硒肥,产量差为 2.115 g/pot,与对照(CK)相比,基施0.28%钙镁磷肥+0.12%硅藻土+0.004‰硒(T3)能够提高1.68倍的稻米产量;随着施用量的增加,pH升高,有效Cd降低,有机质与CEC变化不大;基施硒肥与叶面喷施硒肥处理对土壤pH、有机质与CEC差异不显著,但基施硒肥处理有效Cd含量略低于叶面喷施硒肥处理,T3对土壤Cd的钝化效果最佳;随着基施硒肥用量的增加,稻米Cd含量降低,随着叶面喷施硒肥用量的增加,稻米Cd含量先降低后升高,基施硒肥处理对稻米Cd的消减程度强于叶面喷施硒肥处理,相差 0.021 mg/kg,与对照(CK)相比,T3处理稻米Cd降低0.063 mg/kg。可见,硒对调控稻米镉累积具有重要作用,且基施硒肥强于叶面喷施。综上所述,基施0.28%钙镁磷肥+0.12%硅藻土+0.004‰硒对土壤Cd钝化与稻米Cd消减的效果最佳,值得在镉污染稻田推广应用。