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1.
为了消减冷浸型中低产田长期浸渍、泥温低、土壤有效养分低等障碍因子,通过田间小区试验和动态取样与室内测定,研究了不同有机无机肥配比对冷浸田土壤肥力及水稻生长的影响。结果表明:与复合肥处理比较,复合肥与40%(N)生鸡粪配施处理的土壤磷酸铁盐和磷酸钙盐含量分别提高11%和17%,复合肥与60%(N)生鸡粪配施处理的土壤磷酸铝盐含量提高44%,且磷酸铝盐、磷酸铁盐和磷酸钙盐占无机磷总量的比例提高,闭蓄态磷占无机磷总量的比例降低,促使土壤中难溶性磷向易溶性磷转化,提高土壤有效磷含量;复合肥配施60%(N)生鸡粪处理的土壤松结态腐殖质占重组腐殖质的比例提高1.9个百分点,紧结态腐殖质占重组腐殖质的比例降低4.6个百分点,土壤活性有机质含量提高14%,土壤阳离子交换量提高11%;复合肥与40%(N)生鸡粪配施处理的土壤真菌和放线菌数量分别提高33%和28%,复合肥配施60%(N)生鸡粪处理的土壤细菌数和微生物活性分别提高160%和19%,水稻磷、钾吸收量分别提高5%和111%;复合肥与40%(N)生鸡粪配施处理的早、晚稻产量分别增加8%和42%,复合肥与60%(N)生鸡粪配施处理的早、晚稻产量分别增加6%和31%。有机无机平衡施肥是适合于冷浸田水稻增产的施肥方式。  相似文献   

2.
利用长期定位田间小区试验,研究不同施肥模式(不施肥、施纯化肥、化肥与生物黑炭共施、有机无机肥配施、有机无机肥配施添加生物黑炭)对旱地土壤磷钾径流流失的影响。结果表明:施肥可显著增加旱地土壤各种形式氮素的流失。与单施化肥相比,化肥与生物黑炭配施、有机无机肥配施、有机无机肥与生物黑炭共施均可显著降低旱地土壤各种氮素(TDN、PN、TD)径流流失,降幅分别为37.13%~65.66%,24.17%~54.04%,30.47%~59.69%,降低作用的大小为化肥与生物黑炭配施有机无机肥配施有机无机肥配施与生物黑炭共施。施肥可显著增加旱地土壤磷钾径流流失,与单施化肥相比,化肥与生物黑炭共施、有机无机肥配施、有机无机肥配施添加生物黑炭均可显著降低旱地土壤磷钾素径流流失,对可溶性磷(TDP)、颗粒态磷(PP)、总磷(TP)降幅分别为17.71%~42.19%,9.82%~29.97%,12.08%~31.22%,对钾素降幅为23.24%~33.91%,其中均以化肥与生物黑炭共施处理对磷钾素的径流流失降低幅度最大。在总磷的径流流失中,各处理均以颗粒态磷为主,占总磷流失量的百分比为89.72%~92.02%。旱地土壤地表径流量是决定颗粒态磷和总磷流失的主要因子之一,而对可溶性磷和钾素的流失无直接影响。综上所述,有机无机肥配施添加生物黑炭可有效的减少旱地土壤氮素径流流失,化肥与生物黑炭共施可有效的减少旱地土壤磷钾素径流流失。  相似文献   

3.
【目的】 研究土壤无机磷和有机磷组分变化,有助于选择和优化特定作物体系下不同肥料管理措施,提高磷资源效率。 【方法】 基于20年土冬小麦/夏休闲体系长期肥料定位试验,利用Tiessen-Moir磷素分级法,测定土壤无机磷和有机磷组分,并分析其与小麦磷吸收量、土壤磷表现平衡之间的关系。试验设7个处理:不施肥 (CK)、单施化学氮肥 (N)、氮钾化肥配施 (NK)、磷钾化肥配施 (PK)、氮磷化肥配施 (NP)、氮磷钾化肥配施 (NPK) 和氮磷钾化肥配施有机肥 (MNPK)。 【结果】 旱作条件下,20年长期NP、NPK和MNPK处理较CK、N、NK、PK处理显著提高了小麦籽粒产量,年平均增产在205~265 kg/hm2之间,以MNPK增幅最高。NP、NPK和MNPK处理较CK处理显著提高了小麦籽粒和秸秆吸磷量。PK、NP、NPK、MNPK处理较CK处理显著提高了树脂磷 (Resin-P)、碳酸氢钠提取无机磷 (NaHCO3-Pi)、氢氧化钠提取无机磷 (NaOH-Pi)、浓盐酸提取无机磷 (C.HCl-Pi) 和残余磷 (Residual-P) 含量,显著降低了碳酸氢钠提取有机磷 (NaHCO3-Po) 和氢氧化钠提取有机磷 (NaOH-Po) 含量。PK、NP、NPK与CK相比,对稀盐酸提取无机磷 (D.HCl-Pi)、浓盐酸提取有机磷 (C. HCl-Po) 含量影响不大,而MNPK显著提高了D. HCl-Pi和C. HCl-Po含量。N、NK处理较CK显著增加了Residual-P和C. HCl-Po,显著降低了NaHCO3-Po和NaOH-Po,对Resin-P、NaHCO3-Pi、NaOH-Pi、C.HCl-Pi和D.HCl-Pi含量没有影响。与试验初始时相比,长期施用化学磷肥和有机肥主要增加了土壤中可利用态无机磷的比例,降低了残余态磷和有机磷的比例。土壤中Resin-P、NaHCO3-Pi和C. HCl-Pi与小麦磷吸收量之间呈显著正相关关系。磷素盈余显著增加了D. HCl-Pi、Resin-P和NaHCO3-Pi的含量。 【结论】 供试土壤条件下,NP、NPK和MNPK三种平衡施肥措施都不仅有利于作物增产,而且有利于保持高比例的土壤有效磷库。   相似文献   

4.
为提高高肥力土壤磷素安全可持续利用,探究高肥力土壤碳磷比特征。选取洱海流域3种典型作物类型(粮食作物—玉米、地方特色高值经济作物—烤烟和高值高投入作物—蔬菜)作为研究对象,采集27个样点土壤,测定土壤碳磷含量并计算碳磷比。结果表明:(1)土壤有机碳(SOC)含量为31.91 g/kg,种植不同作物类型土壤SOC含量无显著差异;(2)土壤有效态无机磷(NaHCO3提取态无机磷,简称NaHCO3-Pi)含量为156.7 mg/kg,有效态有机磷(NaHCO3提取态有机磷,简称NaHCO3-Po)含量为63.43 mg/kg,种植不同作物类型的土壤有效态无机磷/有机磷含量(NaHCO3-Pi/NaHCO3-Po)无显著差异,均表现为蔬菜地>烤烟地>玉米地;(3)洱海流域农田土壤C/NaHCO3-Pi比为321.42,C/NaHCO3-Po比为1 138.25,土壤C/NaHCO3-Pi...  相似文献   

5.
针对南方酸性稻作土壤专性吸附和固定磷素能力强的问题,采用微区试验,以正常施磷(75 kg/hm2)不施生物炭为对照,探讨不同磷肥水平(P2O5 75、60、45、30 kg/hm2)和生物炭配施(40、60、80 t/hm2)对土壤不同形态磷素含量的影响。结果表明:(1)减磷施肥配施生物炭后全磷、有效磷、树脂磷、碳酸氢钠无机磷及稀盐酸磷的含量显著增加,残留态磷的含量显著降低。(2)磷肥水平≥45 kg/hm2时,配施生物炭处理的全磷和有效磷含量较对照分别显著提高17.1%~46.7%和32.5%~76.3%。(3)磷肥水平≥45 kg/hm2时,配施生物炭处理的树脂磷和碳酸氢钠无机磷的含量较对照分别显著增加50.8%~160.3%和36.1%~118.3%。(4)减磷施肥导致氢氧化钠有机磷含量较对照下降38.4%~39.8%;处理间氢氧化钠无机磷的含量无显著差异。(5)配施生物炭后稀盐酸磷含量较对照显著提高57.9%~352.1%;减磷施肥处理的浓盐酸有机磷含量显著低于正常施磷...  相似文献   

6.
长期定位施肥对水稻土磷素形态的影响   总被引:5,自引:2,他引:3  
本文通过长期定位施肥试验研究了21年不同施肥处理水稻土中磷素形态及其含量的变化。结果表明,长期不施肥的土壤无论是有机磷还是无机磷中有效磷含量均呈下降趋势,而有机-无机肥配施的有机磷含量不仅高于无肥处理而且还高于单施化肥的处理,并且有利于活性和中度活性有机磷含量的提高。对无机磷的影响,有机-无机肥配施不仅有利于提高Ca-P、Al-P和Fe-P的含量,而且对促进闭蓄态磷的活化效果明显。可见有机-无机肥配施可提高土壤有机磷含量和增加土壤无机磷有效形态的含量。另从土壤有效磷对水稻产量的影响分析可知:当红壤稻田土壤有效磷含量在20mg/kg左右时,增施磷肥对水稻增产效果不明显。  相似文献   

7.
长期有机无机肥配施提高黑土磷含量和活化系数   总被引:4,自引:1,他引:3  
【目的】 长期不同施肥模式影响着耕层土壤磷库以及各形态磷的变化。研究不同施肥模式下黑土各磷素形态含量及有效性的变化,为黑土的肥力培育和合理施用磷肥提供理论依据。 【方法】 黑土长期定位施肥试验位于吉林省公主岭市,始于1990年,供试作物是连作玉米。肥料试验包括不施肥对照 (CK)、施氮、钾肥 (NK)、氮磷钾平衡施肥 (NPK)、氮磷钾 + 有机肥 (NPKM) 共4个处理。化肥处理施氮肥(N) 165 kg/hm2、磷肥(P) 36 kg/hm2、钾肥(K) 68 kg/hm2、猪粪21 t/hm2,NPKM处理的最终N?P?K养分投入量为165?75?145 kg/hm2。选取了1990、1995、2000、2005和2010年的土样,采用Hedley连续浸提法,分析了土壤全磷、有效磷及各有效磷形态含量,计算了土壤磷活化系数 (PAC)。 【结果】 与初始年份相比,NPKM处理土壤全磷、有效磷和磷活化系数,分别显著提高了88.47%、12.98倍和6.42倍。NPK处理对全磷含量影响较小,土壤有效磷含量和PAC值分别增加了1.65倍和2.67倍。CK和NK处理全磷含量降低了15.12%和32.67%,有效磷含量降低了33.47%和12.57%,土壤磷活化系数 (PAC) 分别降低了52.49%和2.55%。所有处理黑土磷库均以无机磷为主,占全磷的80.53%~90.43%。施磷肥处理的无机磷含量占全磷的比值显著高于不施磷处理,对有机磷含量影响不显著。不同处理均以中活性态磷含量最多,占全磷的50.37%~55.06%,活性态磷含量最少,占全磷的7.61%~19.02%。与不施磷处理相比,施磷处理显著提高了土壤活性态磷的比值,尤其是无机磷中的活性态磷的比值。CK、NK处理中Resin-P、NaHCO3-Pi、NaOH-Pi、Conc.HCl-Pi、Residual-P无机磷形态均呈减少趋势;NPK处理中Resin-P、NaHCO3-Pi、NaOH-Pi、Dil.HCl-Pi呈增加趋势,Conc.HCl-Pi和Residual-P呈减少趋势;NPKM处理中,各无机态磷含量均随施肥年限的增加呈增加趋势。相关分析结果表明有效磷含量的变化值与Resin-P、NaHCO3-Pi、NaOH-Pi、Conc.HCl-Po变化值之间存在显著的相关性,其相关系数为0.972、0.665、0.860和0.605,说明活性较高的无机磷对有效磷效率的贡献最大。 【结论】 与施氮钾肥和氮磷钾肥相比,氮磷钾配合有机肥可显著提高土壤全磷、有效磷含量,显著提高土壤活性态无机磷的比例,进而提高土壤磷活化系数,提高磷素利用率。   相似文献   

8.
长期施肥褐土不同磷组分对磷素盈余的响应   总被引:2,自引:1,他引:2  
  【目的】  研究褐土区玉米田长期不同磷源投入对土壤磷素形态和磷素累积的影响,通过对不同磷组分与磷素盈余之间进行相关性分析,研究不同施肥措施对土壤磷素形态转化的影响,为探索合理的磷肥调控措施,促进土壤中磷素向作物易于吸收的水溶态和碳酸氢钠溶解态转化,提高磷素利用效率提供依据。  【方法】  试验依托始于1992年位于山西省寿阳县北坪旱塬上的长期定位试验。9个施肥处理包括:无肥对照 (CK)、N1P1、N2P2、N3P3、N4P4、N2P1M1、N3P2M3、N4P2M2、N0P0M6,其中N1、N2、N3、N4分别为尿素N 60、120、180、240 kg/hm2,P1、P2、P3、P4分别为过磷酸钙P 16、33、49、66 kg/hm2,M为腐熟厩肥,M1、M2、M3、M6分别折合为施P量14、28、42和83 kg/hm2。1992—2016年,收获后取0—20 cm耕层土壤样品,分析土壤磷素形态及盈余量,并计算不同形态磷素与磷盈余量之间的相关性。  【结果】  连续施肥25年后,土壤磷组分发生了不同的变化,不施肥处理除H2O-Pi、Residual-P外,各形态磷较试验初均有降低。施用无机肥各处理主要增加了土壤中HCl-P含量,以N4P4处理提高幅度最大,比试验初提高了127.7%。有机肥投入可以显著提高土壤中的活性磷含量,高量施用有机肥后,H2O-P总含量较试验初提高了8倍之多,NaHCO3-Pi年增加速率为11.50 mg/(kg·a)。不同施肥各处理土壤磷素盈余量为N0P0M6 > N3P2M3 > N4P4 > N4P2M2 > N3P3 > N2P2 > N2P1M1 > N1P1 > CK。磷素盈余是土壤磷组分变化的重要影响因素,各形态磷组分对磷素累积量响应大小为NaHCO3-Pi > NaOH-Pi > HCl-P > NaHCO3-Po > Residual-P > H2O-Po > NaOH-Po > H2O-Pi。  【结论】  长期施肥使土壤各组分磷素含量发生了显著变化,有机无机肥配施有利于土壤中活性磷的转化,过量施磷导致磷素在土壤中大量盈余,高量施用有机肥磷素盈余量最大。当以无机肥投入时,施用过磷酸钙P 33 kg/(hm2·a)基本可以满足作物生长发育的要求。当有机无机肥配施时,施用过磷酸钙P 16 kg/(hm2·a),配施厩肥P 14 kg/(hm2·a) 时,土壤磷素盈余量最小。  相似文献   

9.
长期定位施肥对潮土磷素形态和有效性的影响   总被引:4,自引:2,他引:2  
研究长期定位施肥对潮土各形态磷含量变化及磷有效性的影响,为潮土合理施用磷肥提供理论依据。长期定位施肥试验开始于1990年,设CK(不施肥)、N2(单施尿素)、N2P(不施钾肥)、N2K(不施磷肥)、N1PK(低量氮肥和磷钾肥)、N2PK(平衡施肥)、N3PK(中高量施肥)、N4PK(高量氮肥和磷钾肥)、N2PKM(化肥和有机肥)、N2PKS(化肥和玉米秸秆还田)10个处理;采用Tiessen-Moir磷素分级法测定各施肥处理土壤不同形态磷含量,用常规方法测定有效磷、全磷含量,分析不同形态磷含量间的相关性。结果表明:经过28年定位施肥处理,N2PKM处理土壤各形态磷含量为盐酸态磷(HCl-P)> 残留态磷(Residual-P)> 氢氧化钠无机磷(NaOH-Pi)> 氢氧化钠有机磷(NaOH-Po)> 碳酸氢钠无机磷(NaHCO3-Pi)> 水溶性磷(Resin-Pi)> 碳酸氢钠有机磷(NaHCO3-Po)。在各施肥处理间,N2P、N1PK、N2PK、N3PK、N4PK、N2PKM、N2PKS处理土壤Resin-Pi、NaHCO3-Pi和NaOH-Pi含量显著高于CK、N2、N2K处理,而处理间NaHCO3-Po、NaOH-Po、HCl-P和Residual-P含量差异不显著。除NaOH-Po外,其它形态磷含量与供试土壤有效磷、全磷含量呈极显著相关,其中Resin-Pi对有效磷贡献最大,说明Resin-Pi是最有效的磷源。供试土壤条件下,合理配施化肥有机肥,可以激发磷素后效,使积累磷素向有效态转化,施用有机肥料能显著提高土壤中各磷组分含量,其中有机无机配施处理(N2PKM)提高程度高于单施化肥(N2PK),施用秸秆处理的各磷组分含量同样显著高于不施肥和化肥处理,且施用有机肥和秸秆处理(N2PKS)的中活性和中等活性磷均与土壤速效磷、全磷呈显著正相关,可在潮土上施用有机肥或秸秆处理,从而保持高比例的土壤有效磷库。  相似文献   

10.
  【目的】  全面认知我国苹果园施肥现状,明确苹果园土壤剖面氮磷分布特征,探究减肥增效和地力提升的果园管理技术,为我国苹果产业高质量发展提供理论依据和技术支撑。  【方法】  基于文献资料,制定我国苹果合理化肥施用量;采用实地调查和文献数据相结合的方法,明确和评价我国苹果主产区化肥施用现状;通过田间采样与室内分析,明晰灌区和非灌区苹果园土壤硝态氮和Olsen-P剖面变化特征;基于文献资料,集成苹果园减肥增效、地力提升和优质高产的管理技术。  【结果】  我国苹果园化肥合理施用量为N 150~420 kg/hm2、P2O5 90~330 kg/hm2和K2O 120~420 kg/hm2。目前我国苹果园化肥平均施用量分别为N 905 kg/hm2、P2O5 570 kg/hm2和K2O 675 kg/hm2,氮、磷、钾过量施肥现象普遍且较为严重;施肥结构上,重化肥轻有机肥现象明显,有机肥养分占比仅7.0%。旱作体系下,8年生苹果园土壤与农田相比,0—600 cm土壤剖面硝态氮含量差异不显著,25年生苹果园土壤在20—500 cm土层硝态氮含量显著高于农田,且在120 cm土层出现215 mg/kg的硝态氮峰值;灌区25年生苹果园0—800 cm土壤剖面硝态氮含量均高于100 mg/kg,在380 cm土层出现265 mg/kg的硝态氮峰值,且140—600 cm土层硝态氮含量显著高于旱作25年生苹果园土壤。土壤Olsen-P含量整体表现为0—100 cm土层下降、100—400 cm土层增加和400—600 cm土层基本稳定的趋势;旱作体系下,土壤Olsen-P含量在0—60 cm土层表现为25年生苹果园土壤 > 8年生苹果园土壤 ≈ 农田土壤,而在60—600 cm土层Olsen-P含量差异不显著;灌区25年生苹果园在60—120 cm土层土壤Olsen-P含量高于旱作25年生苹果园,且在80—100 cm土层出现一个14.5 mg/kg的峰值,460—560 cm土层也表现为灌溉果园的Olsen-P含量高于雨养果园的趋势。水肥一体化和推荐施肥是现实苹果园减肥增效的关键技术,有机无机肥配施、果园生草、施用生物炭是提高苹果园肥料利用效率及土壤肥力的重要途径。  【结论】  我国苹果园过量施肥和不平衡施肥问题严重;高量施肥背景下长期苹果种植导致土壤深层剖面硝态氮和有效磷累积,无效化风险高,且灌溉加剧了氮、磷的淋溶风险;水肥一体化和苹果养分专家系统等推荐施肥,以及有机无机肥配施、果园生草、施用生物炭等是实现我国苹果园减肥增效和地力提升的关键技术,在今后苹果园管理方面,应加强不同生态区适宜的综合技术研究。  相似文献   

11.
溶磷细菌肥对石灰性土壤磷素转化的影响   总被引:7,自引:0,他引:7  
通过室内模拟培养和大豆盆栽土培生物模拟试验,研究了磷细菌溶解磷酸钙的能力及在北方石灰性土壤上施用磷细菌肥对土壤磷素转化的影响。试验结果表明:磷细菌菌株具有较强溶解磷酸钙的能力,磷酸钙的溶出率从第1天的2.80%提高到第8天的22.00%。在贫速效磷和富难溶性磷土壤上施用溶磷细菌肥有利于土壤中难溶态的Ca10-P和缓效态Ca8-P含量下降,促使土壤中Ca2-P和Al-P的含量增加,从而使土壤中有效磷含量增加。而对于富速效磷的土壤,无论施菌肥与否对土壤中各种形杰的无机磷绢分基本没有影响.  相似文献   

12.
磷素活化剂对红壤磷形态及有效性影响的研究   总被引:3,自引:0,他引:3  
在我国南方红壤中加入不同的磷活化剂进行培养试验,结果显示:磷活化剂提高了土壤有效磷含量,不同活化剂的活化能力不同。相关分析和通径分析结果表明,磷活化剂的活化能力大小顺序为:低分子有机酸钠钙盐>腐植酸>腐植酸钠>脲基甲酸乙酯;磷活化剂可以提高红壤中的Al-P、Ca-P和Fe-P等无机磷含量,其中Al-P和Ca-P与有效磷均达到极显著水平,而Fe-P作用效果不显著,可以通过影响Al-P和Ca-P来间接影响有效磷,磷活化剂会抑制土壤中O-P的生成。  相似文献   

13.
Phosphorus (P) in agricultural soils is an important factor for soil quality and environmental protection. Understanding of P and its fractions in soils on a regional scale is imperative for effective management or utilization of P and the improvement of P availability in soils. To study spatial variability and changes of soil P and its fractions as affected by farming practices, soil samples were taken in Rugao County, Jiangsu Province of China, an intensive agricultural area in the Yangtze River Delta region, in years of 1982 (n = 1 514), 1997 (n = 1 651), and 2002 (n = 342). High spatial variabilities of Olsen P and total P (TP) were observed throughout the study area. Loamy Stagnic Anthrosols and clay or loamy Aquic Cambosols had significantly higher concentrations of Olsen P and TP than sandy Ustic Cambosols and Aquic Cambosols. Olsen P and TP were increased from 1982 to 2002. The accumulations of Olsen P and TP in the cultivated soils were likely related to the increased application of P fertilizer, organic input, and soil incorporation of crop residues as well as conversion of soil use. Accumulated soil P was dominantly in labile and semi-labile P fractions. These P fractions may be utilized by future crop production by adjusting management practices, but they also pose a serious threat to nearby water bodies. Future strategies should include decreasing P fertilization in soils and supporting sustainable management. The information from this study can be used to monitor changes in soil fertility and environmental risks so that the use of fertilizers can become more rational.  相似文献   

14.
Abstract

Laboratory drying may alter manure phosphorus (P) distribution. The effects of freeze, air (22°C), and oven (65°C) drying on sequentially fractioned poultry manure P were examined. Higher drying temperatures resulted in lower percentage of dry matter. Increased H2O‐ and decreased sodium bicarbonate (NaHCO3)‐extractable P with drying provided evidence that drying increases poultry manure P solubility. Labile fractions were predominantly inorganic P (Pi), whereas sodium hydroxide (NaOH) and hydrochloric acid (HCl) fractions had significant amounts of organic P (Po). Drying altered H2O‐ and NaHCO3‐extractable Pi but had no consistent effect on Po in these fractions. This work suggests that variations due to drying should be taken into consideration when evaluating manures for P availability or when comparing data in which different drying methods have been utilized.  相似文献   

15.
温室土壤磷素迁移变化特征研究   总被引:1,自引:0,他引:1  
采用野外调查采样和室内分析相结合的方法,研究了典型温室栽培地区山东寿光土壤磷素状况及其迁移变化特征。结果表明:(1)除Ca10-P外,温室土壤耕层(0~20 cm)全磷及无机磷组分含量均显著高于露地土壤,其平均含量分别为露地土壤的2.9、3.7、5.6、4.1、3.4倍和6.1倍,且以耕层累积为主,表现出明显的表聚特征,并有向下迁移的趋势;(2)在温室栽培的前期,磷素累积较快,连续种植了4~8 a时,全磷含量达到一个较高范围,为露地土壤的2~4倍,随着种植年限的继续增加,其再累积磷素的能力较差,甚至略有下降;(3)Ca8-P、Al-P和O-P是温室土壤磷素累积的主要形态,与露地土壤相比,其在0~20 cm耕层的平均增加量分别为296.5、288.5、306.0 mg.kg-1;(4)温室土壤耕层水溶性磷和速效磷的平均含量为10.9 mg.kg-1和248.4 mg.kg-1,分别为露地土壤的8.7倍和5.4倍,磷淋失并造成环境污染的可能性很大。  相似文献   

16.
Recycled phosphorus (P) fertilizers from sewage sludge can contribute to the ongoing effort of closing the P cycle. Five recycled P fertilizers (Struvite SSL, Struvite AirPrex®, P‐RoC®, Pyrolysis coal, and Na‐SSA) were tested for their P availability in a two‐year field experiment with maize. The experiment was conducted on an organic certified research station at soil pH 6.5. Other P fertilizer treatments included: phosphate rock (PR), compost, and an unfertilized control. In addition, the rhizobacteria strain Bacillus sp. Proradix (Proradix®) was applied to test its ability to increase P bioavailability. Each year, shoot DM and P offtake of maize was measured and P use efficiency of the tested fertilizers was calculated. No significant differences in shoot DM were found among fertilized treatments and the unfertilized control in both years of experiment. Fertilization with recycled fertilizers increased P offtake by between 0% (Na‐SSA) and 27.5% (Struvite SSL) compared to the unfertilized control. Rhizobacteria application led to an increase in P offtake of maize from 25.9 to 38.7 kg P ha?1 when combined with PR fertilization in the year of fertilizer application, while no significant effect was found for the recycled fertilizers. Some of the tested recycled fertilizers from urban waste water can be considered as effective fertilizers for their use in organic agriculture.  相似文献   

17.
A large variety of extraction methods are used worldwide for the estimation of “plant‐available P” in soils. In Germany, the standard extractants are Calcium‐Acetate‐Lactate (CAL) and Double‐Lactate (DL). Until now there is no validated transformation procedure available and studies on the comparability of both methods have reported conflicting evidence. The uncertainty about the equivalence of CAL‐P and DL‐P hinders a direct comparison of the P fertility status and P fertilizer recommendations across Germany. Based on 136 datasets for soil samples from an interlaboratory comparison program and three P fertilization field trial sites, for which plant‐available P had been determined by both the CAL and DL method, we assessed the comparability of both extraction methods and derived simple and multiple regression equations to transform DL‐P into CAL‐P values. On average, DL extracted 30% more P than CAL. However, this strongly depended on soil pH and carbonate content. A simple linear regression model explained 70% of the variance. However, if simple linear regression models were fitted to pH‐specific samples (pH range 4.5 to 7.0) the R2 increased to 0.96. Based on an independent validation dataset (n = 48) we demonstrated that such pH‐specific models were more accurate than models that did not consider pH when transforming DL‐P to CAL‐P values. Multiple regression results showed that out of soil pH, Corg, Nt, and C : N ratio, only soil pH improved the model. The transformation equations in this study provide a step towards an improved comparability of P fertility status assessments of soils across Germany.  相似文献   

18.
Abstract

Phosphorus (P) is an essential element and its efficient use is of global importance. This study evaluated the effect of growing potato under legume intercrops on P uptake and use efficiency indices: P harvest index (PHI), P uptake efficiency (PuPE), P partial factor productivity (PPFP) and P partial balance (PPB). The experiment was carried out for four consecutive seasons with treatments comprising potato cultivated under legume intercrops: none (T1), dolichos (Lablab purpureus L) (T2), peas (Pisum sativum L) (T3) and beans (Phaseolus vulgaris L) (T4). Across the seasons, the mean haulm P uptake for T2 (6.7?kg P ha?1), T4 (5.5) and T3 (4.5) were 6%, 23% and 36% lower than that observed in T1 (7.1?kg P ha?1), respectively. On the other hand, tuber P uptake was highest in T1 (21.8?kg P ha?1) and T2 (21.3?kg P ha?1) and were significantly higher than 13.2?kg P ha?1 in T3 and 15.1?kg P ha?1 in T4. This had a profound effect on PuPE, which was equally highest in T1 (0.26?kg total P uptake kg?1 P supply) and T2 (0.25) and lowest in T3 (0.16) and T4 (0.18). Similarly, PPFP, PHI and PPB followed a similar trend, with highest values in T1 (57?kg tuber dry matter yield kg?1 P supply, 76.4?kg tuber P uptake kg?1 total plant’s P uptake and 0.20?kg tuber P uptake kg?1 P supply, respectively). Among the tested legume intercrops, dolichos competed least for P with the main crop (potato) hence it can be integrated into potato-based cropping systems without compromising potato tuber yield.  相似文献   

19.
The phytoavailability of soil phosphorus (P) depends on the different forms in which it occurs and how these forms change after the application of P fertiliser to the soil. Forms of P in the A, B and C horizons of eleven pedons that developed on mafic rocks were characterised by a fractionation method before and after fertilisation with single superphosphate, and a micropot experiment was conducted to assess the short-term use of P fertiliser by rye (Secale cereale L.). The main sources of P to the crop were (i) phosphate adsorbed on mineral surfaces and pedogenic Fe, Al or Ca phosphates in the A horizon and (ii) Ca-phosphates in B and C horizons. In the C horizons, poor in Fe/Al phases and clay, the precipitated Ca-P showed low solubility, resulting in a reduction in shoot biomass. The apparent P recovery by rye was similar in the A (36%) and B (29%) but decreased in the C (15%) horizons. The partial factor productivity (g g?1) decreased from the A (58) to B (11) and C (5) horizons. P phytoavailability decreased with increasing profile depth because the transformation of P fertiliser to poorly soluble Ca-P forms increased with depth.  相似文献   

20.
黄土旱塬冬小麦磷素含量累积动态与磷肥利用效率研究   总被引:3,自引:0,他引:3  
利用旱作长期定位施肥试验,研究施用磷肥对冬小麦植株磷素含量的动态变化以及磷肥利用效率的影响。结果表明,磷肥对冬小麦植株体内含磷量的影响呈V型,冬前期最高,随着作物生长逐渐降低,灌浆期达到最小值,随后又有回升。冬小麦磷素累积主要集中在拔节期—开花期,和灌浆期—成熟期2个阶段进行,保证这2个阶段磷素供应对小麦的良好生长有重要作用。从磷肥利用效率、产量等指标来看,在施用氮肥90 kg/hm2的情况下,磷肥用量应该控制在45~90 kg/hm2的合理范围内。  相似文献   

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