有机共聚物肥料添加剂对玉米磷素发酵肥响应的评价

Sheri Cahill, R. Gehl, D. Osmond, D. Hardy
{"title":"有机共聚物肥料添加剂对玉米磷素发酵肥响应的评价","authors":"Sheri Cahill, R. Gehl, D. Osmond, D. Hardy","doi":"10.1094/CM-2013-0322-01-RS","DOIUrl":null,"url":null,"abstract":"Fertilizer additive products have recently been developed with the intention of reducing phosphate fixation and improving phosphorus plant availability. We conducted two experiments at multiple North Carolina locations from 2007-2009 to evaluate the effects of an organic copolymer phosphorus fertilizer additive, AVAIL Phosphorus Fertilizer Enhancer (Specialty Fertilizer Products, Leawood, KS), on corn (Zea maize L.) nutrient uptake, growth, and yield. Treatments included a combination of diammonium phosphate (DAP, [(NH ) HPO ]) P fertilizer rates with and without AVAIL. Grain yields did not differ across fertilizer treatments or across low, medium, or very high initial soil test phosphorus. Grain P concentration differed among treatments in only 2 of 16 site-years, where the N-only treatment had less tissue P than the treatments including P with or without AVAIL. Also, Nonly plots occasionally had shorter plants compared with DAP and DAP + AVAIL. Treating DAP with AVAIL did not consistently affect corn plant growth parameters in the Piedmont and Mountain Regions of North Carolina, and using treated DAP did not offer a consistent agronomic benefit over DAPor N-only fertilization. Introduction New synthetic organic copolymer phosphorus fertilizer additives have been recently developed to combat P-limited crop productivity by reducing phosphate fixation in soil. These products do not supply nutrients and cannot be evaluated based on nutrient content. Some manufacturers claim that these products enhance cation exchange capacity (CEC), moisture-holding capacity, and soil organism populations, and may also stimulate plant root growth and development (4). However, Crozier et al. (4) report that only a small (0.01 to 0.12 meq/100 g) change in CEC could be expected under typical recommendation rates for many of these products and that an increase of CEC in the root zone or carry-over CEC changes for the subsequent crop is unlikely. Similarly, Jones et al. (8) reported that labeled humic acid rates may not significantly increase organic acid concentrations in the soil, based on their greenhouse wheat study where humic acid coatings on monoammonium phosphate (MAP) did not increase P solubility, availability, or uptake, nor did it increase spring wheat grain yields on Montana calcareous and noncalcareous soils. These two studies imply that in order to substantially increase CEC or soil humate, rates much greater than those recommended on product labeling may be needed. Currently, one organic copolymer phosphorus fertilizer additive being marketed throughout much of the USA is AVAIL Phosphorus Fertilizer Enhancer. The AVAIL product is available for use with either granular or liquid phosphate fertilizers and consists of long chained, high cation exchange capacity maleic-itaconic copolymers (17,18). In dry form, AVAIL is designed to be coated 4 4 4 22 March 2013 Crop Management onto granular phosphate fertilizers and is reported to surround P fertilizer in a water-soluble ‘shield’ that expands to block the elements that tie-up P in soil (e.g., Ca, Mg, Fe, and Al) (17,18). Research results from investigations on the effects of AVAIL have been quite variable. A one-year trial in Ohio did not find a corn yield difference among plots treated with or without AVAIL, though soil sampling indicated that additional P was not required to increase corn yield (11). Thus, starter P with or without AVAIL was not likely to increase yields in that field. McGrath and Binford (12) conducted a 3-year corn trial in the Delmarva area and found that none of their eight site-years showed an early plant growth or yield response on AVAIL treated plots. However, early plant growth was increased in all years and grain yield increased during two site-years when a P starter fertilizer was applied. Ward (19) investigated corn growth and yield response to AVAIL over eight site-years in Kansas during the 2008-2009 growing seasons. While all sites had initial Mehlich-3 extractable P (M3P) of ≤ 15 mg/kg, where a P response could be expected, only one of the eight site-years showed a significant yield response to P fertilizer addition, and there were no significant responses in V4 plant biomass, R1 ear leaf P concentration, grain yield, moisture, test weight, or grain P concentration as a result of the AVAIL-treated P fertilizer treatments. A 3-year corn trial in southern Minnesota on low and medium-high Olsenextractable P soil also found inconsistent yield results when comparing MAP and DAP with AVAIL-treated MAP and DAP; a yield response to broadcastapplied AVAIL-treated DAP over untreated DAP was observed in 1 of 2 years, and no response was seen with AVAIL-treated MAP compared with untreated MAP (15). In contrast, Gordon (7) reported increases in both corn grain and soybean (Glycine max L.) yields averaged over 3-years in north-central Kansas for AVAIL-treated MAP compared with untreated MAP on a soil with a 22 ppm of Bray-1 P. Therefore, the objective of our study was to evaluate corn plant growth and grain yield response to starter P fertilizers applied with and without AVAIL on sites ranging in initial soil test P (STP). Field Studies Study 1. Research was conducted in 2007 and 2008 at seven sites on three research stations in North Carolina: Piedmont Research Station, Salisbury (Salisbury A, B, and C); Mountain Research Station, Waynesville (Waynesville A and B); and Mountain Horticultural Crops Research Station (MHCRS), Mills River (Mills River A and B), and at one cooperating farmer site in Buncombe County (Buncombe), representing 14 site-years. Corn was grown on low (13-30 mg P/kg), medium (31-60 mg P/kg), high (61-120 mg P/kg), and very high (>120 mg P/kg) STP and varying soil textures (Table 1). A representative 0-20 cm soil sample from each plot was analyzed using Mehlich-3 extractant to determine STP before treatment. Treatments were arranged in a randomized complete block design (RCBD) with four replications and included DAP (18-460) at 15 kg P/ha and 13 kg N/ha, DAP plus AVAIL (treated by supplier) at 15 kg P/ha and 13 kg N/ha, or ammonium nitrate (AN [NH4NO3]) only at 224 kg N/ha at planting. Both years, starter P fertilizer was surface applied in a 10-cm band over the row at planting. All DAP and DAP + AVAIL plots received an additional 211 kg N/ha as AN surface-broadcast at planting, while the N-only plots received AN surface-broadcast at planting. Corn was planted in no-till plots 7.6-m long by 3.7-m wide (4 rows, 0.91-m row spacing) at Salisbury and Buncombe. The sites at Mills River and Waynesville were 9.1-m long by 3.7-m wide (4 rows, 0.91-m row spacing) and were managed with conventional tillage (fall moldboard plow followed by two disk passes in subsequent spring). 22 March 2013 Crop Management Table 1. Site locations, year, soil series, and pre-study soil chemical characteristics (0-20 cm) for each of the 16 site-years. Corn plant height has often been used as an indicator of early season growth, corn total biomass, and grain yield (1,6) Thus, average plant height in each plot was measured 3 weeks after emergence; corn plants were measured from the ground to the top of the whorl. Tassel percentage was measured 8 to 10 weeks after planting. Corn grain yield was determined by hand-harvesting and weighing ears from the center 3.05 m of the center two rows of each plot and grain moisture was measured with a grain moisture meter. Grain samples were dried at 40°C for 48 h then ground and analyzed for N and P concentration using a Perkin-Elmer CHN Elemental Analyzer (Model II), and Pregl and Dumas analysis (5). The 2007-2008 growing season rainfall was less than 30-year average growing-season rainfall at each location. The growing seasons both years were exceptionally dry, as the entire state of North Carolina experienced drought conditions throughout that time (13) (Table 2). The average monthly temperatures during the 2007 and 2008 seasons at Mills River, Buncombe, and Waynesville were warmer than average, except in July at Waynesville when temperatures were cooler (Table 2). Salisbury temperatures were cooler than average except for July which was warmer. Analysis of variance for yield, N and P accumulation, plant height, and tassel percentage was performed using SAS PROC MIXED (16). Data were analyzed by location with treatment and rates as fixed effects. Tests of fixed effects were computed using ddmf = kl option of the MODEL statement. Differences in measured variables due to treatments were considered significant at P ≤ 0.05. Location Year Region Soil series HM (g/kg) pH P K (mg/kg) Mills River A 2007 Mountain Hayesville loam 7.6 6.0 72 199 2008 7.1 6.3 136 188 Mills River B 2007 Mountain Statler fine sandy loam 5.8 5.9 194 198 2008 4.6 5.8 121 148 Salisbury A 2008 Piedmont Hiwassee clay 3.0 5.6 57 145 Salisbury B 2007 Piedmont Chewaclo loam 3.8 5.5 110 77 2008 3.5 6.4 166 93 Salisbury C 2007 Piedmont Mecklenburg loam 5.5 6.9 385 409 2008 2.7 7.2 387 327 Waynesville A 2007 Mountain Cullowhee-Nikwasi complex 12.6 5.7 136 133 2008 11.7 5.5 141 110 Waynesville B 2007 Mountain Braddock clay loam 30.0 6.1 174 437 2008 27.0 6.2 159 385 Buncombe 2008 Mountain French loam 6.5 6.1 14 41 MHCRS 2008 Mountain Dillard loam 24.0 6.3 45 159 2009 Comus fine sandy loam 32.8 5.4 29 117 22 March 2013 Crop Management Table 2. Precipitation and temperature data for the 16 site-years, recorded by the State Climate Office of North Carolina. * Source: State Climate Office of North Carolina (www.nc-climate.ncsu.edu). Study 2. Research was conducted in 2008 and 2009 at the MHCRS. Soil test P was determined before planting using procedures as described for Study 1 (Table 1). Corn was grown on low and medium STP soils using conventional tillage (fall moldboard plow followed by spring disking). Average initial STP at Mills River was 35 mg/kg, and ranged from 16.2 to 58.4 mg/kg during the 2 years and plots (data not shown). Eighty-six percent of the plots tes","PeriodicalId":100342,"journal":{"name":"Crop Management","volume":"34 6 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"11","resultStr":"{\"title\":\"Evaluation of an Organic Copolymer Fertilizer Additive on Phosphorus Starter Fertilizer Response by Corn\",\"authors\":\"Sheri Cahill, R. Gehl, D. Osmond, D. Hardy\",\"doi\":\"10.1094/CM-2013-0322-01-RS\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Fertilizer additive products have recently been developed with the intention of reducing phosphate fixation and improving phosphorus plant availability. We conducted two experiments at multiple North Carolina locations from 2007-2009 to evaluate the effects of an organic copolymer phosphorus fertilizer additive, AVAIL Phosphorus Fertilizer Enhancer (Specialty Fertilizer Products, Leawood, KS), on corn (Zea maize L.) nutrient uptake, growth, and yield. Treatments included a combination of diammonium phosphate (DAP, [(NH ) HPO ]) P fertilizer rates with and without AVAIL. Grain yields did not differ across fertilizer treatments or across low, medium, or very high initial soil test phosphorus. Grain P concentration differed among treatments in only 2 of 16 site-years, where the N-only treatment had less tissue P than the treatments including P with or without AVAIL. Also, Nonly plots occasionally had shorter plants compared with DAP and DAP + AVAIL. Treating DAP with AVAIL did not consistently affect corn plant growth parameters in the Piedmont and Mountain Regions of North Carolina, and using treated DAP did not offer a consistent agronomic benefit over DAPor N-only fertilization. Introduction New synthetic organic copolymer phosphorus fertilizer additives have been recently developed to combat P-limited crop productivity by reducing phosphate fixation in soil. These products do not supply nutrients and cannot be evaluated based on nutrient content. Some manufacturers claim that these products enhance cation exchange capacity (CEC), moisture-holding capacity, and soil organism populations, and may also stimulate plant root growth and development (4). However, Crozier et al. (4) report that only a small (0.01 to 0.12 meq/100 g) change in CEC could be expected under typical recommendation rates for many of these products and that an increase of CEC in the root zone or carry-over CEC changes for the subsequent crop is unlikely. Similarly, Jones et al. (8) reported that labeled humic acid rates may not significantly increase organic acid concentrations in the soil, based on their greenhouse wheat study where humic acid coatings on monoammonium phosphate (MAP) did not increase P solubility, availability, or uptake, nor did it increase spring wheat grain yields on Montana calcareous and noncalcareous soils. These two studies imply that in order to substantially increase CEC or soil humate, rates much greater than those recommended on product labeling may be needed. Currently, one organic copolymer phosphorus fertilizer additive being marketed throughout much of the USA is AVAIL Phosphorus Fertilizer Enhancer. The AVAIL product is available for use with either granular or liquid phosphate fertilizers and consists of long chained, high cation exchange capacity maleic-itaconic copolymers (17,18). In dry form, AVAIL is designed to be coated 4 4 4 22 March 2013 Crop Management onto granular phosphate fertilizers and is reported to surround P fertilizer in a water-soluble ‘shield’ that expands to block the elements that tie-up P in soil (e.g., Ca, Mg, Fe, and Al) (17,18). Research results from investigations on the effects of AVAIL have been quite variable. A one-year trial in Ohio did not find a corn yield difference among plots treated with or without AVAIL, though soil sampling indicated that additional P was not required to increase corn yield (11). Thus, starter P with or without AVAIL was not likely to increase yields in that field. McGrath and Binford (12) conducted a 3-year corn trial in the Delmarva area and found that none of their eight site-years showed an early plant growth or yield response on AVAIL treated plots. However, early plant growth was increased in all years and grain yield increased during two site-years when a P starter fertilizer was applied. Ward (19) investigated corn growth and yield response to AVAIL over eight site-years in Kansas during the 2008-2009 growing seasons. While all sites had initial Mehlich-3 extractable P (M3P) of ≤ 15 mg/kg, where a P response could be expected, only one of the eight site-years showed a significant yield response to P fertilizer addition, and there were no significant responses in V4 plant biomass, R1 ear leaf P concentration, grain yield, moisture, test weight, or grain P concentration as a result of the AVAIL-treated P fertilizer treatments. A 3-year corn trial in southern Minnesota on low and medium-high Olsenextractable P soil also found inconsistent yield results when comparing MAP and DAP with AVAIL-treated MAP and DAP; a yield response to broadcastapplied AVAIL-treated DAP over untreated DAP was observed in 1 of 2 years, and no response was seen with AVAIL-treated MAP compared with untreated MAP (15). In contrast, Gordon (7) reported increases in both corn grain and soybean (Glycine max L.) yields averaged over 3-years in north-central Kansas for AVAIL-treated MAP compared with untreated MAP on a soil with a 22 ppm of Bray-1 P. Therefore, the objective of our study was to evaluate corn plant growth and grain yield response to starter P fertilizers applied with and without AVAIL on sites ranging in initial soil test P (STP). Field Studies Study 1. Research was conducted in 2007 and 2008 at seven sites on three research stations in North Carolina: Piedmont Research Station, Salisbury (Salisbury A, B, and C); Mountain Research Station, Waynesville (Waynesville A and B); and Mountain Horticultural Crops Research Station (MHCRS), Mills River (Mills River A and B), and at one cooperating farmer site in Buncombe County (Buncombe), representing 14 site-years. Corn was grown on low (13-30 mg P/kg), medium (31-60 mg P/kg), high (61-120 mg P/kg), and very high (>120 mg P/kg) STP and varying soil textures (Table 1). A representative 0-20 cm soil sample from each plot was analyzed using Mehlich-3 extractant to determine STP before treatment. Treatments were arranged in a randomized complete block design (RCBD) with four replications and included DAP (18-460) at 15 kg P/ha and 13 kg N/ha, DAP plus AVAIL (treated by supplier) at 15 kg P/ha and 13 kg N/ha, or ammonium nitrate (AN [NH4NO3]) only at 224 kg N/ha at planting. Both years, starter P fertilizer was surface applied in a 10-cm band over the row at planting. All DAP and DAP + AVAIL plots received an additional 211 kg N/ha as AN surface-broadcast at planting, while the N-only plots received AN surface-broadcast at planting. Corn was planted in no-till plots 7.6-m long by 3.7-m wide (4 rows, 0.91-m row spacing) at Salisbury and Buncombe. The sites at Mills River and Waynesville were 9.1-m long by 3.7-m wide (4 rows, 0.91-m row spacing) and were managed with conventional tillage (fall moldboard plow followed by two disk passes in subsequent spring). 22 March 2013 Crop Management Table 1. Site locations, year, soil series, and pre-study soil chemical characteristics (0-20 cm) for each of the 16 site-years. Corn plant height has often been used as an indicator of early season growth, corn total biomass, and grain yield (1,6) Thus, average plant height in each plot was measured 3 weeks after emergence; corn plants were measured from the ground to the top of the whorl. Tassel percentage was measured 8 to 10 weeks after planting. Corn grain yield was determined by hand-harvesting and weighing ears from the center 3.05 m of the center two rows of each plot and grain moisture was measured with a grain moisture meter. Grain samples were dried at 40°C for 48 h then ground and analyzed for N and P concentration using a Perkin-Elmer CHN Elemental Analyzer (Model II), and Pregl and Dumas analysis (5). The 2007-2008 growing season rainfall was less than 30-year average growing-season rainfall at each location. The growing seasons both years were exceptionally dry, as the entire state of North Carolina experienced drought conditions throughout that time (13) (Table 2). The average monthly temperatures during the 2007 and 2008 seasons at Mills River, Buncombe, and Waynesville were warmer than average, except in July at Waynesville when temperatures were cooler (Table 2). Salisbury temperatures were cooler than average except for July which was warmer. Analysis of variance for yield, N and P accumulation, plant height, and tassel percentage was performed using SAS PROC MIXED (16). Data were analyzed by location with treatment and rates as fixed effects. Tests of fixed effects were computed using ddmf = kl option of the MODEL statement. Differences in measured variables due to treatments were considered significant at P ≤ 0.05. Location Year Region Soil series HM (g/kg) pH P K (mg/kg) Mills River A 2007 Mountain Hayesville loam 7.6 6.0 72 199 2008 7.1 6.3 136 188 Mills River B 2007 Mountain Statler fine sandy loam 5.8 5.9 194 198 2008 4.6 5.8 121 148 Salisbury A 2008 Piedmont Hiwassee clay 3.0 5.6 57 145 Salisbury B 2007 Piedmont Chewaclo loam 3.8 5.5 110 77 2008 3.5 6.4 166 93 Salisbury C 2007 Piedmont Mecklenburg loam 5.5 6.9 385 409 2008 2.7 7.2 387 327 Waynesville A 2007 Mountain Cullowhee-Nikwasi complex 12.6 5.7 136 133 2008 11.7 5.5 141 110 Waynesville B 2007 Mountain Braddock clay loam 30.0 6.1 174 437 2008 27.0 6.2 159 385 Buncombe 2008 Mountain French loam 6.5 6.1 14 41 MHCRS 2008 Mountain Dillard loam 24.0 6.3 45 159 2009 Comus fine sandy loam 32.8 5.4 29 117 22 March 2013 Crop Management Table 2. Precipitation and temperature data for the 16 site-years, recorded by the State Climate Office of North Carolina. * Source: State Climate Office of North Carolina (www.nc-climate.ncsu.edu). Study 2. Research was conducted in 2008 and 2009 at the MHCRS. Soil test P was determined before planting using procedures as described for Study 1 (Table 1). Corn was grown on low and medium STP soils using conventional tillage (fall moldboard plow followed by spring disking). Average initial STP at Mills River was 35 mg/kg, and ranged from 16.2 to 58.4 mg/kg during the 2 years and plots (data not shown). 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引用次数: 11

摘要

肥料添加剂产品最近被开发出来,目的是减少磷肥固定和提高植物磷素利用率。从2007年到2009年,我们在北卡罗来纳州的多个地点进行了两个实验,以评估有机共聚物磷肥添加剂AVAIL磷肥增强剂(特种肥料产品,Leawood, KS)对玉米(Zea maize L.)养分吸收、生长和产量的影响。处理包括施用磷酸铵(DAP, [(NH) HPO])磷肥,有和无效果。不同施肥处理或低、中、高初始土壤试验磷对粮食产量没有影响。籽粒磷浓度在16个站点年中只有2个处理之间存在差异,其中仅施氮处理的组织磷含量低于施氮或不施氮处理。此外,与DAP和DAP + AVAIL相比,Nonly样地偶尔会出现植株较短的情况。在北卡罗莱纳州的山前和山区,用AVAIL处理DAP对玉米植株的生长参数没有一致的影响,使用处理过的DAP也没有提供与DAPor单氮施肥相比一致的农艺效益。新的合成有机共聚物磷肥添加剂最近被开发出来,通过减少土壤中的磷素固定来对抗磷限制作物的生产力。这些产品不提供营养,不能根据营养含量进行评估。一些制造商声称,这些产品提高阳离子交换能力(CEC)、持湿能力和土壤生物种群,并可能刺激植物根系生长和发育(4)。然而,Crozier等人(4)报告说,在许多此类产品的典型推荐率下,CEC的变化很小(0.01至0.12 meq/100 g),根区CEC的增加或后续作物的CEC变化不太可能发生。同样,Jones等人(8)报道,标记的腐植酸速率可能不会显著增加土壤中的有机酸浓度,基于他们的温室小麦研究,在磷酸铵(MAP)上的腐植酸涂层不会增加P的溶解度、有效性或吸收量,也不会增加蒙大拿钙质和非钙质土壤上的春小麦产量。这两项研究表明,为了大幅增加CEC或土壤腐殖质,可能需要比产品标签上推荐的速率高得多的速率。目前,一种有机共聚物磷肥添加剂在美国大部分地区都有销售,那就是AVAIL磷肥增强剂。AVAIL产品可用于颗粒状或液态磷肥,由长链,高阳离子交换容量的马来共聚物组成(17,18)。在干燥的形式下,AVAIL被设计成包覆在颗粒磷肥上,据报道,它在水溶性“屏蔽”中包裹磷肥,该“屏蔽”会扩展以阻止土壤中与磷结合的元素(例如Ca, Mg, Fe和Al)(17,18)。对AVAIL效果的调查研究结果变化很大。在俄亥俄州进行的一项为期一年的试验并没有发现施磷肥和不施磷肥对玉米产量有什么影响,尽管土壤取样表明不需要额外施磷肥来提高玉米产量(11)。因此,施或不施启动磷肥都不可能提高该地区的产量。McGrath和Binford(12)在Delmarva地区进行了一项为期3年的玉米试验,发现在他们的8个站点年里,在AVAIL处理过的地块上,没有一个显示出早期的植物生长或产量反应。但施用磷素发酵剂后,各年份的植株早期生长均有提高,2个立地年的籽粒产量均有提高。Ward(19)在堪萨斯州2008-2009年的生长季节调查了玉米生长和产量对AVAIL的响应。虽然所有试验点的初始Mehlich-3可提取磷(M3P)均≤15 mg/kg,但8个站点年中只有1个站点年对P肥的添加表现出显著的产量响应,而4个站点年对植物生物量、R1穗叶P浓度、籽粒产量、水分、试验重量或籽粒P浓度均无显著响应。在明尼苏达州南部进行的一项为期3年的玉米试验中,在低磷和中磷土壤上,MAP和DAP与aap处理的MAP和DAP的产量结果也不一致;在2年的试验中,有1年的试验中观察到施用经有效应答处理的DAP比未经有效应答的DAP有产量应答,而与未经有效应答的MAP相比,经有效应答处理的MAP没有应答(15)。相比之下,Gordon(7)报告说,在堪萨斯州中北部,在含有22 ppm Bray-1 P的土壤中,与未经处理的MAP相比,在3年的平均产量中,使用aap处理的MAP增加了玉米和大豆(Glycine max L.)的产量。 因此,本研究的目的是评价玉米植株生长和籽粒产量对初始土壤试验磷(STP)范围内施磷肥和不施磷肥的响应。实地研究研究1研究于2007年和2008年在北卡罗来纳州的三个研究站的七个地点进行:皮埃蒙特研究站,索尔兹伯里(索尔兹伯里A, B和C);韦恩斯维尔山地研究站(韦恩斯维尔A和B);和山地园艺作物研究站(MHCRS),米尔斯河(米尔斯河A和B),以及Buncombe县的一个合作农民站点(Buncombe),代表了14个站点年。玉米在低(13-30 mg P/kg)、中(31-60 mg P/kg)、高(61-120 mg P/kg)和极高(>120 mg P/kg) STP和不同土壤质地下生长(表1)。在处理前,使用Mehlich-3萃取剂对每个地块的代表性0-20 cm土壤样品进行分析,以确定STP。采用随机完全区组设计(RCBD),共4个重复,包括施用15 kg磷/公顷和13 kg氮/公顷的DAP(18-460),施用15 kg磷/公顷和13 kg氮/公顷的DAP + AVAIL(由供应商处理),或施用224 kg氮/公顷的硝酸铵(AN [NH4NO3])。两年播种时,在行上以10厘米带状施磷肥。所有DAP和DAP + AVAIL地块在种植时额外施氮211 kg / hm2,而仅施氮的地块在种植时施氮。在索尔兹伯里和邦库姆,玉米种植在长7.6米、宽3.7米(4行,行距0.91米)的免耕地块上。米尔斯河和韦恩斯维尔的场地长9.1米,宽3.7米(4行,行距0.91米),采用传统耕作方式(秋季犁板犁,随后在春季进行两次圆盘耕作)。2013年3月22日作物管理16个站点年的站点位置、年份、土壤系列和预研究土壤化学特征(0-20 cm)。玉米株高常被用作早季生长、玉米总生物量和籽粒产量的指标(1,6),因此,在出苗后3周测量每个地块的平均株高;测量玉米植株的长度,从地面一直测量到植株的顶部。播种后8 ~ 10周测定雄穗百分率。采用手采法测定玉米籽粒产量,称重玉米穗距每地块中心两行3.05 m处,用谷物水分计测定籽粒水分。谷物样品在40°C下干燥48 h,然后研磨,使用Perkin-Elmer CHN元素分析仪(模型II)和Pregl和Dumas分析分析N和P浓度(5)。2007-2008年生长季降雨量小于每个地点30年平均生长季降雨量。这两年的生长季节都异常干燥,因为整个北卡罗来纳州在这段时间里都经历了干旱(13)(表2)。2007年和2008年季节,米尔斯河、邦库姆和韦恩斯维尔的月平均气温比平均温度高,韦恩斯维尔的7月温度较低(表2)。索尔兹伯里的月平均气温比平均温度低,但7月温度较高。利用SAS PROC mix软件对产量、氮磷积累、株高和抽穗率进行方差分析(16)。数据分析的位置,治疗和率作为固定效果。使用MODEL语句的ddmf = kl选项计算固定效果的测试。处理导致的测量变量差异在P≤0.05时认为有统计学意义。位置年地区土壤HM系列(g / kg) pH值P K(毫克/公斤)米尔斯河2007山Hayesville壤土7.6 - 6.0 7.1 - 6.3 72 199 2008 136 188米尔斯河B 2007山这些良好的砂质壤土索尔兹伯里5.8 5.9 4.6 - 5.8 194 198 2008 121 148 145 2008山麓Hiwassee粘土3.0 - 5.6 57索尔兹伯里B 2007山麓Chewaclo壤土索尔兹伯里3.8 5.5 3.5 - 6.4 110 77 2008 166 93 2007 C山麓梅克伦堡壤土5.5 - 6.9 2.7 - 7.2 385 409 2008 387 327 2007山Cullowhee-Nikwasi Waynesville复杂的12.6 - 5.72013年3月22日韦恩斯维尔B 2007山Braddock粘土壤土30.0 6.1 174 437 2008 27.0 6.2 159 385 Buncombe 2008山法国壤土6.5 6.1 14 41 MHCRS 2008山迪拉德壤土24.0 6.3 45 159 2009 Comus细砂壤土32.8 5.4 29 117 2013年3月22日作物管理表2北卡罗莱纳州气候办公室记录的16个站点年的降水和温度数据。*来源:北卡罗来纳州气候办公室(www.nc-climate.ncsu.edu)。研究2。研究是在2008年和2009年在MHCRS进行的。土壤试验磷在种植前使用研究1中描述的程序(表1)进行测定。玉米在低和中等STP土壤上使用常规耕作(秋季犁板犁和春季圆盘)种植。米尔斯河的平均初始STP为35 mg/kg,在2年和图中范围为16.2至58.4 mg/kg(数据未显示)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of an Organic Copolymer Fertilizer Additive on Phosphorus Starter Fertilizer Response by Corn
Fertilizer additive products have recently been developed with the intention of reducing phosphate fixation and improving phosphorus plant availability. We conducted two experiments at multiple North Carolina locations from 2007-2009 to evaluate the effects of an organic copolymer phosphorus fertilizer additive, AVAIL Phosphorus Fertilizer Enhancer (Specialty Fertilizer Products, Leawood, KS), on corn (Zea maize L.) nutrient uptake, growth, and yield. Treatments included a combination of diammonium phosphate (DAP, [(NH ) HPO ]) P fertilizer rates with and without AVAIL. Grain yields did not differ across fertilizer treatments or across low, medium, or very high initial soil test phosphorus. Grain P concentration differed among treatments in only 2 of 16 site-years, where the N-only treatment had less tissue P than the treatments including P with or without AVAIL. Also, Nonly plots occasionally had shorter plants compared with DAP and DAP + AVAIL. Treating DAP with AVAIL did not consistently affect corn plant growth parameters in the Piedmont and Mountain Regions of North Carolina, and using treated DAP did not offer a consistent agronomic benefit over DAPor N-only fertilization. Introduction New synthetic organic copolymer phosphorus fertilizer additives have been recently developed to combat P-limited crop productivity by reducing phosphate fixation in soil. These products do not supply nutrients and cannot be evaluated based on nutrient content. Some manufacturers claim that these products enhance cation exchange capacity (CEC), moisture-holding capacity, and soil organism populations, and may also stimulate plant root growth and development (4). However, Crozier et al. (4) report that only a small (0.01 to 0.12 meq/100 g) change in CEC could be expected under typical recommendation rates for many of these products and that an increase of CEC in the root zone or carry-over CEC changes for the subsequent crop is unlikely. Similarly, Jones et al. (8) reported that labeled humic acid rates may not significantly increase organic acid concentrations in the soil, based on their greenhouse wheat study where humic acid coatings on monoammonium phosphate (MAP) did not increase P solubility, availability, or uptake, nor did it increase spring wheat grain yields on Montana calcareous and noncalcareous soils. These two studies imply that in order to substantially increase CEC or soil humate, rates much greater than those recommended on product labeling may be needed. Currently, one organic copolymer phosphorus fertilizer additive being marketed throughout much of the USA is AVAIL Phosphorus Fertilizer Enhancer. The AVAIL product is available for use with either granular or liquid phosphate fertilizers and consists of long chained, high cation exchange capacity maleic-itaconic copolymers (17,18). In dry form, AVAIL is designed to be coated 4 4 4 22 March 2013 Crop Management onto granular phosphate fertilizers and is reported to surround P fertilizer in a water-soluble ‘shield’ that expands to block the elements that tie-up P in soil (e.g., Ca, Mg, Fe, and Al) (17,18). Research results from investigations on the effects of AVAIL have been quite variable. A one-year trial in Ohio did not find a corn yield difference among plots treated with or without AVAIL, though soil sampling indicated that additional P was not required to increase corn yield (11). Thus, starter P with or without AVAIL was not likely to increase yields in that field. McGrath and Binford (12) conducted a 3-year corn trial in the Delmarva area and found that none of their eight site-years showed an early plant growth or yield response on AVAIL treated plots. However, early plant growth was increased in all years and grain yield increased during two site-years when a P starter fertilizer was applied. Ward (19) investigated corn growth and yield response to AVAIL over eight site-years in Kansas during the 2008-2009 growing seasons. While all sites had initial Mehlich-3 extractable P (M3P) of ≤ 15 mg/kg, where a P response could be expected, only one of the eight site-years showed a significant yield response to P fertilizer addition, and there were no significant responses in V4 plant biomass, R1 ear leaf P concentration, grain yield, moisture, test weight, or grain P concentration as a result of the AVAIL-treated P fertilizer treatments. A 3-year corn trial in southern Minnesota on low and medium-high Olsenextractable P soil also found inconsistent yield results when comparing MAP and DAP with AVAIL-treated MAP and DAP; a yield response to broadcastapplied AVAIL-treated DAP over untreated DAP was observed in 1 of 2 years, and no response was seen with AVAIL-treated MAP compared with untreated MAP (15). In contrast, Gordon (7) reported increases in both corn grain and soybean (Glycine max L.) yields averaged over 3-years in north-central Kansas for AVAIL-treated MAP compared with untreated MAP on a soil with a 22 ppm of Bray-1 P. Therefore, the objective of our study was to evaluate corn plant growth and grain yield response to starter P fertilizers applied with and without AVAIL on sites ranging in initial soil test P (STP). Field Studies Study 1. Research was conducted in 2007 and 2008 at seven sites on three research stations in North Carolina: Piedmont Research Station, Salisbury (Salisbury A, B, and C); Mountain Research Station, Waynesville (Waynesville A and B); and Mountain Horticultural Crops Research Station (MHCRS), Mills River (Mills River A and B), and at one cooperating farmer site in Buncombe County (Buncombe), representing 14 site-years. Corn was grown on low (13-30 mg P/kg), medium (31-60 mg P/kg), high (61-120 mg P/kg), and very high (>120 mg P/kg) STP and varying soil textures (Table 1). A representative 0-20 cm soil sample from each plot was analyzed using Mehlich-3 extractant to determine STP before treatment. Treatments were arranged in a randomized complete block design (RCBD) with four replications and included DAP (18-460) at 15 kg P/ha and 13 kg N/ha, DAP plus AVAIL (treated by supplier) at 15 kg P/ha and 13 kg N/ha, or ammonium nitrate (AN [NH4NO3]) only at 224 kg N/ha at planting. Both years, starter P fertilizer was surface applied in a 10-cm band over the row at planting. All DAP and DAP + AVAIL plots received an additional 211 kg N/ha as AN surface-broadcast at planting, while the N-only plots received AN surface-broadcast at planting. Corn was planted in no-till plots 7.6-m long by 3.7-m wide (4 rows, 0.91-m row spacing) at Salisbury and Buncombe. The sites at Mills River and Waynesville were 9.1-m long by 3.7-m wide (4 rows, 0.91-m row spacing) and were managed with conventional tillage (fall moldboard plow followed by two disk passes in subsequent spring). 22 March 2013 Crop Management Table 1. Site locations, year, soil series, and pre-study soil chemical characteristics (0-20 cm) for each of the 16 site-years. Corn plant height has often been used as an indicator of early season growth, corn total biomass, and grain yield (1,6) Thus, average plant height in each plot was measured 3 weeks after emergence; corn plants were measured from the ground to the top of the whorl. Tassel percentage was measured 8 to 10 weeks after planting. Corn grain yield was determined by hand-harvesting and weighing ears from the center 3.05 m of the center two rows of each plot and grain moisture was measured with a grain moisture meter. Grain samples were dried at 40°C for 48 h then ground and analyzed for N and P concentration using a Perkin-Elmer CHN Elemental Analyzer (Model II), and Pregl and Dumas analysis (5). The 2007-2008 growing season rainfall was less than 30-year average growing-season rainfall at each location. The growing seasons both years were exceptionally dry, as the entire state of North Carolina experienced drought conditions throughout that time (13) (Table 2). The average monthly temperatures during the 2007 and 2008 seasons at Mills River, Buncombe, and Waynesville were warmer than average, except in July at Waynesville when temperatures were cooler (Table 2). Salisbury temperatures were cooler than average except for July which was warmer. Analysis of variance for yield, N and P accumulation, plant height, and tassel percentage was performed using SAS PROC MIXED (16). Data were analyzed by location with treatment and rates as fixed effects. Tests of fixed effects were computed using ddmf = kl option of the MODEL statement. Differences in measured variables due to treatments were considered significant at P ≤ 0.05. Location Year Region Soil series HM (g/kg) pH P K (mg/kg) Mills River A 2007 Mountain Hayesville loam 7.6 6.0 72 199 2008 7.1 6.3 136 188 Mills River B 2007 Mountain Statler fine sandy loam 5.8 5.9 194 198 2008 4.6 5.8 121 148 Salisbury A 2008 Piedmont Hiwassee clay 3.0 5.6 57 145 Salisbury B 2007 Piedmont Chewaclo loam 3.8 5.5 110 77 2008 3.5 6.4 166 93 Salisbury C 2007 Piedmont Mecklenburg loam 5.5 6.9 385 409 2008 2.7 7.2 387 327 Waynesville A 2007 Mountain Cullowhee-Nikwasi complex 12.6 5.7 136 133 2008 11.7 5.5 141 110 Waynesville B 2007 Mountain Braddock clay loam 30.0 6.1 174 437 2008 27.0 6.2 159 385 Buncombe 2008 Mountain French loam 6.5 6.1 14 41 MHCRS 2008 Mountain Dillard loam 24.0 6.3 45 159 2009 Comus fine sandy loam 32.8 5.4 29 117 22 March 2013 Crop Management Table 2. Precipitation and temperature data for the 16 site-years, recorded by the State Climate Office of North Carolina. * Source: State Climate Office of North Carolina (www.nc-climate.ncsu.edu). Study 2. Research was conducted in 2008 and 2009 at the MHCRS. Soil test P was determined before planting using procedures as described for Study 1 (Table 1). Corn was grown on low and medium STP soils using conventional tillage (fall moldboard plow followed by spring disking). Average initial STP at Mills River was 35 mg/kg, and ranged from 16.2 to 58.4 mg/kg during the 2 years and plots (data not shown). Eighty-six percent of the plots tes
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