秸秆生物炭对黄土区农田土壤养分和作物生长的影响

旨在探索生物炭对黄土区农田的具体应用效果。采用大田试验,在不施氮肥和施氮肥(187.5 kg/hm2)处理下,分别设计了不同生物炭用量(0、6、12、24、48 t/hm2)试验,来观察对黄土高原农田土壤养分和玉米生长的影响。结果发现：当施入187.5 kg/hm2氮肥时,24~48 t/hm2范围内的生物炭施用量对土壤养分促进作用效果最佳,其中48 t/hm2时全氮超出对照26.6%,碱解氮可超过对照约27.67%;6~12 t/hm2的范围时,玉米茎粗、叶绿素在生长中期均相对处于优势,且玉米养分含量和产量结果优于生物炭量大的处理。不施氮的情况下,生物炭也可促进土壤和玉米籽粒养分的积累。其中6~12 t/hm2时,土壤和玉米籽粒养分含量相对较高;24~48 t/hm2时玉米产量结果最佳,比对照高1468.2 kg/hm2,约13.39%。结果表明,生物炭的添加对土壤的养分影响较大,且一定程度上依赖于氮肥的投入情况。     

绿洲膜下滴灌调亏对马铃薯土壤环境及产量的影响

为测定膜下滴灌调亏马铃薯全生育期内不同调亏水平土壤养分、土壤水热动态、生长动态、产量效应和水分利用效率,于2016年在河西荒漠绿洲灌区民乐县益民灌溉试验站开展了马铃薯不同生育阶段水分调亏灌溉的试验研究,结果表明,马铃薯膜下滴灌调亏土壤水热变化均匀且利用率高,有利于马铃薯对土壤养分的充分吸收和利用;土壤养分是土壤肥力的核心,是植物在生长发育过程中不可或缺的重要因素,膜下滴灌调亏栽培能有效减少土壤速效养分的流失,并提高马铃薯对土壤速效养分的利用效率;不同生育阶段马铃薯耗水量受水分调亏程度影响较大,其耗水量随调亏程度增大而显著减少(P0.05),水分调亏处理马铃薯全生育期总耗水量均低于全生育期充分灌水CK处理。块茎形成期轻度水分亏缺马铃薯水分利用效率、灌溉水利用效率、生物量均达到最大,较全生育期充分灌水显著提高29.04%,35.61%。因此,块茎形成期轻度水分亏缺灌溉方式能使马铃薯根区土壤始终保持湿润状态,有效减少渗漏损失和植株间无效蒸发损失,改善土壤水、肥和热量状况,有利于提高作物水分利用效率,且不显著降低马铃薯最终产量。     

优化施肥对滨海盐渍土棉花生长及土壤养分供应特性的影响

通过2年大田试验,研究优化施肥对东营滨海盐渍土棉花生长及土壤养分供应能力的影响。设不施肥、农民传统施肥、优化施肥、优化施肥+有机肥4个处理。结果表明:与农民传统施肥对比,优化施肥及优化施肥+有机肥处理有效提高了棉花产量、肥料农学利用率、偏生产力;施肥改变了土壤盐基离子组成,农民传统施肥、优化施肥、优化施肥+有机肥处理Na+及Cl-所占比分别减少2.29%,3.45%,6.15%,K+、Ca2+、Mg2+、SO_2-4有不同程度的提高;优化施肥+有机肥处理能明显提高土壤微生物和酶活性,其中脲酶、碱性磷酸酶活性分别比传统施肥和优化施肥高7.8%~17.0%和5.0%~13.3%;施肥提高了土壤速效养分,优化施肥+有机肥处理速效P和速效K含量总体处于较高水平,而N0-3-N、NH+4-N含量总体表现为传统施肥优化施肥+有机肥优化施肥不施肥,这说明优化施肥能有效降低土壤NO-3-N、NH+4-N含量,进而NO-3-N、NH+4-N的流失风险也随之减小。采用N、K肥基施+蕾期花期2次追施的优化施肥处理,不仅减少了肥料用量,而且提高了产量,配合施用有机肥增产效果更为显著。     

物联网模式下的农业土壤养分监测及施肥系统研究

针对目前国内传统施肥方式中,存在基肥施用量大,盲目施肥,氮、磷、钾单一品种化肥用量过多,导致土壤肥力退化、土壤养分不均衡,影响到农作物增收等现状,借助物联网技术、近红外分析技术、现代通信技术和无线网络技术,选用近红外分析技术和基于FFT算法及小波变换的光谱微弱信号处理方法,实现实时监测土壤养分的变化,全面而准确地掌握农业土壤养分情况,并智能控制自动施肥执行端施肥。为此,进行了样机试制,并运用于不同的农业土壤,包括褐土、红土、黑土等进行养分监测和施肥试验。结果表明:农业土壤养分监测及施肥系统可稳定运行,精准施肥,能满足不同农业土壤的精确施肥。本系统可指导科学施肥,提高农业生产的施肥水平,减少农业污染。     

滇东北铅锌矿区废弃地的自然演替特征研究

为探究矿区废弃地的自然演替特征,于2020年10月对滇东北两铅锌矿区废弃地进行植物群落调查和群落土样采集分析。结果表明:两区均受到较严重的重金属污染,土壤Pb、Mn、Zn、Cu和Cd的含量均超过相关背景值。其中,两区土壤Pb和Zn以及富乐镇矿区土壤Mn和Cd的有效态占比大体上都呈现随演替进行而降低的趋势,富乐镇矿区土壤Cu的有效态占比呈现随演替发生而先增后减的趋势,矿山镇矿区土壤Mn、Cu和Cd的有效态占比在不同演替阶段呈现不规则波动。两区土壤全氮随着演替的发生均呈现先增后减的趋势;两区土壤全磷含量变化趋势不同,矿山镇矿区呈现持续增加,富乐镇矿区则呈现先减后增;两区土壤有机质含量都呈现持续增加的趋势。在矿山镇矿区中,Pb和Zn、Pb和SOM呈极显著正相关性,Pb和TP、Mn和TN、Cd和TN、Zn和SOM、SOM和TN呈显著正相关性,Pb和Cu、Zn和Cu、Cu和SOM、Cu和TP呈显著负相关性。在富乐镇矿区中,Pb和Zn呈极显著正相关性,Zn和Mn、Zn和Cu、Zn和SOM、Pb和TP、SOM和TN呈显著正相关性,Pb和Cu、Zn和Cd、Cu和Cd呈显著负相关性。研究表明,矿区次生演替过程与废弃农田和灾后森林等生境的次生演替过程相似,土壤重金属元素的有效态会随演替发生而降低。研究结果可为矿区废弃地的自然恢复提供参考借鉴。     

中国东南部红壤地区不同植被对土壤侵蚀和土壤养分的影响

The effect of different vegetation systems including bamboo plantation (BP), forest ecosystem (CF), citrus orchard (Ctr) and farmland (FL) on erosion and nutrients of red soil were investigated in hilly region of southeastern China to find effective control measures for soil erosion. The results showed that all the vegetation systems could significantly reduce soil erosion and nutrient losses compared to bare land (Br). The ability of different vegetation systems to conserve soil and water was in the order of Ctr > BP > CF > FL > Br. Vegetation could also improve soil fertility. The soil organic matter, total N and total P contents were much higher in all the vegetation systems than in bare land, especially for the top soils. Vegetation systems improved soil physical properties remarkably. Compared to the bare land, soil organic matter, TP, TK and available K, especially soil microbial biomass C, N and P, increased under all the vegetation covers. However, they were still much lower than expected, thus these biological measurements are still needed to be carried out continuously.     

潮土区不同质地土壤的养分动态变化研究

对华北平原大兴县 1 982— 2 0 0 0年两个时段大量土壤样本的分析结果表明 ,土壤养分含量与土壤质地表现出明显的一致性 ,体现了土壤质地越重 ,养分含量越高的特点 ;土壤质地对土壤养分含量的影响 ,1 982年的大于 2 0 0 0年的 ;但 2 0年来 ,由于土地利用集约度的增强 ,质地对土壤养分水平的影响渐趋减弱 ,不同质地土壤的养分水平渐趋一致     

Soil nutrient changes due to land use changes in Northern China: a case study in Zunhua County, Hebei Province

Abstract. Since the 1980s, land use in rural areas of China has changed greatly as the result of political initiatives. These changes have caused soil nutrient changes which are examined in this paper for Zunhua County, northern China from 1980 to 1999. The areas of farmland, grassland, and paddy decreased greatly and were replaced by increases in forest and residential land. The soils under forest in 1999 transformed from farmland in 1980 increased in organic matter by 21%, total nitrogen by 18%, available nitrogen by 65%, available phosphorus by 17% and available potassium by 17%. Similarly, in the area which was converted from farmland in 1980 to grassland in 1999, soil organic matter, total nitrogen, available nitrogen, available phosphorus, and available potassium increased by 38%, 37%, 71%, 2% and 28%, respectively. Changes from farmland to forest and grassland not only changed land cover but also improved soil fertility and probably reduced soil nutrient losses.     

Wind erosion and sand accumulation effects on soil properties in Horqin Sandy Farmland,Inner Mongolia

Rain-fed agriculture is widespread in Inner Mongolia, northern China, where wind erosion of farmland is very common because of sandy soil and dry, windy weather. However, very little is known about the effects of wind erosion on soil physical and chemical properties in this region. A field experiment was conducted in sandy farmland, where erosional and depositional gradients were established to evaluate the effects of wind erosion and leeward sand accumulation on soil texture, nutrient content, soil water, and soil temperature. The research showed that long term wind erosion could result in significant soil coarseness, infertility and dryness. Severe erosion reduced clay by 59.6%, organic C by 71.2%, total N by 67.4%, total P by 31.4%, available N by 64.5%, available P by 38.8%, and average soil water content by 51.8%, compared with non-eroded farmland in the study region. The sand fraction (particles > 0.05 mm), pH and ground-surface temperature increased by 6.2%, 3.7%, and 2.2 °C, respectively. Accumulated sand also caused a decrease in nutrients and soil water content. Under severe sand accumulation, clay was reduced by 2.0%, organic C by 19.3%, total N by 21.7%, total P by 13.7%, available N by 52.5%, and average soil water content by 26.6%. The sand fraction, pH, available P, and ground-surface temperature increased by 0.2%, 0.9%, 5.8% and 2.8 °C, respectively.     

糯米糍荔枝叶片矿质养分含量充足范围的确定

对深圳市4个典型丰产园糯米糍荔枝叶片7种矿质养分(氮、磷、钾、钙、镁、锌和硼)含量的统计分析表明:采样地点和生育时期均对叶片营养元素含量有显著的影响。四个关键生育时期(末次秋梢老熟期、花芽形态分化期、谢花期和果实成熟期)的单株样与混合(多株)样的供试矿质养分含量之间大部分没有显著差异。本研究根据丰产园糯米糍荔枝叶片混合样的分析结果提出了7种矿质养分的充足含量范围。