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1.
稻田垄作免耕对土壤团聚体和有机质的影响 总被引：10，自引：3，他引：7
该文以1990年建立的耕作制定位试验田紫色水稻土为研究对象,分析了冬水田（FPF）、水旱轮作（CR）和垄作免耕（RNT）3种耕作方式对土壤团聚体组成和有机质的影响。结果表明,垄作免耕减少了对土壤大团聚体的破坏,在0～10 cm土层,垄作免耕大团聚体含量分别是冬水田和水旱轮作的1.48和1.32倍,微团聚体含量则显著降低;在 ＞10～20 cm土层有相同的趋势。3种耕作条件下,有机碳和氮在团聚体中的分布模式类似,均有向大团聚体富集的趋势,但垄作免耕条件下土壤有机碳和氮质量分数显著高于冬水田和水旱轮作。对土壤颗粒有机质（POM）的分析结果表明,垄作免耕0～10 cm土层轻质组分（LF）的质量分数（1.92 g/kg）与水旱轮作（1.70 g/kg）差异不显著,但显著高于冬水田（1.42 g/kg）。冬水田、水旱轮作和垄作免耕的0～10 cm土层,团聚体内总颗粒有机质（total iPOM）质量分数分别为0.96,1.12,2.14 g/kg;垄作免耕土壤团聚体内细颗粒有机质（fine iPOM）分别为冬水田和水旱轮作土壤的3.02和2.46倍,占总POM差异的57%和66%。垄作免耕土壤团聚体内粗颗粒有机质（coarse iPOM）分别为冬水田和水旱轮作土壤的1.56和1.40倍,占总POM差异的18%和19%。在＞10～20 cm土层有相似的趋势,但在＞10～20 cm层土壤粗iPOM的差异对总POM差异的贡献较0～10 cm层大。垄作免耕减少了对大团聚体的破坏并促进微团聚体向大团聚体团聚;降低了团聚体的周转速率,促进了细iPOM的固定,利于紫色水稻土对碳的固定和积累。 相似文献
2.
耕作制度对紫色水稻土有机碳累积及矿化动态的影响 总被引：4，自引：0，他引：4
以稻田长期定位试验为平台,研究常规平作（中稻-冬水田）、垄作免耕（中稻-冬水田）、垄作免耕（中稻-油菜）和水旱轮作（中稻-油菜）4种耕作制度对紫色水稻土有机碳累积及矿化动态的影响。结果表明：实行不同耕作制度均能提高土壤有机碳密度,以垄作免耕（中稻-油菜）最佳。不同耕作制度实施20年后,农田0-10 cm表层土壤有机碳密度已趋于稳定,垄作免耕会提高10-20 cm和20-40 cm土层有机碳密度,而水旱轮作各土层有机碳密度均低于其他耕作处理。不同耕作制度下水稻土中易氧化有机碳数量和有机碳氧化稳定系数差异较大,其中,垄作免耕（中稻-油菜）下水稻土有机碳氧化稳定系数最大。各耕作处理中,土壤有机碳的最大矿化速率差异显著,有机碳矿化率和pH呈显著正相关;在培养期间,垄作免耕（中稻-油菜）的累积矿化量始终显著低于其他处理;常规平作（中稻-冬水田）的总矿化强度最大,垄作免耕（中稻-油菜）最小。 相似文献
3.
稻田长期垄作免耕对水稻产量及土壤肥力的影响研究 总被引：39，自引：3，他引：39
不同耕作条件下的水稻生长发育、作物产量及土壤肥力状况的研究表明,稻田长期垄作免耕,水稻根系数量、白根率、根系活力比常规平作和水旱轮作高,分蘖时间早;垄作免耕水稻的株高、茎粗、穗长、穗粒数增加,11年水稻平均产量垄作免耕比常规平作和水旱轮作分别提高了10.3%和11.3%。垄作免耕改变了土壤的物理、化学性状,土壤容重、土壤养分含量明显提高,土壤微生物数量和酶活性增强,土壤表层松结态腐殖质含量比常规平作和水旱轮作高0.194和0.238个百分点,紧结态腐殖质降低0.098和0.037个百分点。垄作免耕有利于提高作物产量、培肥地力、改善土壤生态环境。 相似文献
4.
保护性耕作对丘陵区水稻土团聚体稳定性的影响 总被引：13，自引：1，他引：12
长期保护性耕作通过增加土壤有机碳而成为稻田土壤结构改良的一项有效措施,而保护性耕作对土壤团聚体稳定机制的影响尚未完全清楚。本文供试土样采自耕作制定位试验水旱轮作、冬水免耕、垄作免耕和厢作免耕耕层（0～ 20 cm）土壤,土样经过糊化作用、湿润作用和再次糊化作用等预处理,用以阐明稻田土壤团聚体的破碎机制。研究结果表明：糊化作用和湿润作用后紫色水稻土团聚体稳定性差异不明显,而保护性耕作显著影响团聚体的稳定性。糊化作用后团聚体水稳性强弱顺序为：垄作免耕＞厢作免耕＞冬水免耕＞水旱轮作,湿润作用后团聚体水稳性强弱顺序为：厢作免耕＞垄作免耕＞冬水免耕＞水旱轮作。糊化作用下团聚体稳定性与有机碳浓度相关性不显著（r＝0.432,p＞0.05）,湿润作用下团聚体稳定性与有机碳浓度呈极显著正相关（r＝0.626,p＜0.01）。因此,研究结果说明保护性耕作有利于紫色水稻土大团聚体有机碳含量提高,进而增强团聚体的水稳性。 相似文献
5.
不同耕作制度对紫色水稻土活性有机质及碳库管理指数的影响 总被引：13，自引：1，他引：13
以长期定位试验点的紫色水稻土为研究对象，研究了耕作制度对紫色水稻土活性有机质和碳库管理指数的影响。结果表明：稻田长期垄作免耕0～10cm土层有机质含量比常规平作高，10～60cm土层有机质含量则比常规平作低；表明稻田长期垄作免耕土壤有机质具有表层富集现象；水旱轮作各土层有机质含量均比常规平作低。垄作免耕各土层活性有机质含量普遍增加，水旱轮作表层（0～10cm）活性有机质含量减少，其余土层变化不大。对活性有机质组分含量的研究表明：与常规平作相比，垄作免耕增加了土壤表层活性有机质各个组分的含量，在其余土层增加了低活性有机质含量，而减少了高活性有机质含量；水旱轮作增加了各土层低活性有机质含量而减少了中活性和高活性有机质含量。垄作免耕所有土层的碳库管理指数都在100以上，水旱轮作除表层（0～10cm）小于100以外，其余土层都在100以上。由此可见，农业管理措施对土壤有机质、活性有机质及碳库管理指数有较大影响。 相似文献
6.
垄作免耕对稻田垄埂土壤有机碳累积和作物产量的影响 总被引：4，自引：0，他引：4
依托稻田免耕长期定位试验,研究了垄作免耕对稻田垄埂土壤有机碳累积和作物产量的影响。研究主要涉及常规平作(中稻-冬水田,简称中稻)、常规平作(中稻-油菜,简称稻油)、垄作免耕(中稻)和垄作免耕(稻油)等4个耕作处理。针对垄作对田面微地形的影响,将垄作小区中所有垄埂当成一个整体,统计其土壤有机碳的累积指标,再与平作处理中同体积或同质量的表土层(对比土层)作比较。结果表明,在对比土层和小区垄埂体积相同时,垄作免耕(稻油)的垄埂土壤有机碳密度要显著高于2个常规平作处理中对比土层和垄作免耕(中稻)的垄埂(p0.05);在对比土层与小区垄埂质量相同时,各耕作处理的垄埂或对比土层中单位质量土壤的固碳量依次为:垄作免耕(稻油)常规平作(中稻)垄作免耕(中稻)常规平作(稻油),且处理间差异显著(p0.05)。这表明,针对垄埂和对比土层而言,垄作免耕(稻油)的土壤有机碳累积效应要优于垄作免耕(中稻)和常规平作处理。与传统的常规平作相比,垄作免耕的水稻增产效应明显,虽然其会导致油菜减产,但不影响水旱两季作物的经济总产出。总体而言,垄作免耕(稻油)是一种能兼顾环境和经济效益的稻田保护性耕作措施。 相似文献
7.
以稻田免耕长期定位试验为平台,研究长期垄作免耕对稻田土壤有机碳剖面分布的影响。结果表明,垄作免耕(中稻)、垄作免耕(稻油)、常规平作(中稻)和水旱轮作(稻油)4种耕作处理实施20年后,稻田0-60cm土体中各土层有机碳含量最高值和最低值分别出现在垄作免耕(稻油)和水旱轮作(稻油)中,且水旱轮作(稻油)中各土层有机碳含量均显著低于其他耕作处理;垄作免耕(稻油)中0-10cm和40-60cm土层有机碳含量与垄作免耕(中稻)、常规平作(中稻)之间差异不显著,但20-40cm土层有机碳含量则显著高于其他耕作处理(P<0.05),可见同传统耕作相比,长期垄作免耕(稻油)稻田的增碳优势主要体现在20-40cm土层。不同耕作处理连续实施20年后,稻田0-60cm土体有机碳密度的高低顺序为垄作免耕(稻油)>垄作免耕(中稻)>常规平作(中稻)>水旱轮作(稻油),且处理间差异显著(P<0.05)。垄作免耕15～20年期间,稻田0-10cm表层土壤有机碳储量基本稳定,但20-40cm土层有机碳储量仍有增加,其中垄作免耕(稻油)增加最为明显,表明20-40cm土层碳累积是长期垄作免耕下稻田发挥增碳功能的重要机制。 相似文献
8.
土壤颗粒态氮作为土壤有机氮中的非稳定性部分,对土壤中氮的平衡有着重要的影响,对作物的生长及增产增收也有着重要意义.试验以西南大学农业部重庆紫色土生态环境重点野外科学观测试验站内于1989年设立的长期免耕试验田为研究对象,研究冬水田平作、水旱轮作、垄作免耕和垄作翻耕等耕作方式对土壤颗粒态氮的影响.结果表明,不同耕作方式下土壤全氮及颗粒态氮含量均具有明显的垂直分布特征,由上到下含量逐渐降低.在0-60 cm的土壤深度内,土壤全氮平均含量依次为垄作免耕(1.53g/kg)>冬水田平作(1.50 g/kg)>垄作翻耕(1.31 g/kg)>水旱轮作(1.16 g/kg);颗粒态氮平均含量依次为冬水田平作(0.55 g/kg)>垄作免耕(0.46 g/kg)>垄作翻耕(0.40 g/kg)>水旱轮作(0.35 g/kg).免耕能够增加土壤全氮含量,但无助于颗粒态氮含量的增加.不同耕作方式下的颗粒态土碳氮比大于全土碳氮比,表明颗粒态土壤有机质易被微生物分解,是土壤营养物质的重要来源. 相似文献
9.
耕作方式对紫色水稻土总有机碳及颗粒态有机碳的影响 总被引：2，自引：0，他引：2
为研究耕作方式对西南地区紫色水稻土总有机碳及颗粒态有机碳的影响,以1989年设立的位于西南大学农场的农业部重庆紫色土生态环境重点野外科学观测试验站内的长期免耕试验田为对象,研究在冬水田平作（DP）、水旱轮作（SH）、垄作免耕（LM）、厢作免耕（XM）和垄作翻耕（LF）5种不同耕作方式下,土壤中总有机碳（TOC）含量、颗粒态有机碳（POC）含量、颗粒态土壤质量分数和颗粒态有机碳分配比在土壤中的分布特点。结果表明,不同的耕作方式主要对表层土壤的TOC、POC分布产生显著影响,其中LM对提高积累TOC和POC贡献最大;0-60 cm土层TOC含量变化范围为7.10～34.45 g/kg,颗粒态土壤质量分数所占比例为30.38%～45.65%,POC含量为1.31～19.39 g/kg,各数值基本变化趋势都是随土壤深度的增加而减小。TOC与POC都可作为评价耕作方式影响紫色水稻土土壤质量变化与固碳能力的有效指标,但相同耕作制度下POC变化幅度更大,对其响应也更为敏感。从TOC和POC的关系来看,不同耕作制度下有机碳的增加与土壤物理保护能力的提高有关,免耕方式有利于有机碳以及颗粒态有机碳的保护和稳定。 相似文献
10.
垄作免耕下紫色水稻土有机碳的分布特征 总被引：13，自引：4，他引：13
土壤有机碳的空间分布特征是研究土壤有机碳储量及其动态的重要内容之一。本文从土壤团聚体、剖面和田块等尺度研究了四川盆地紫色水稻土在垄作免耕下有机碳的分布特征。结果表明：紫色水稻土团聚体含碳量在大团聚体（2～0．25mm）中最高，但有机碳总量主要分布在0．25～0．02mm。其次是0．02-0．002mm；垄作免耕下团聚体有机碳主要富集在0—10cm土层的大团聚体（〉0．25mm）中（富集系数〉1．5），而常规平作、水旱轮作和垄作翻耕下，剖面中土壤有机碳含量分布自上而下缓慢降低；实验田表层土壤有机碳含量及相关土壤特性的空间分布呈条带状和斑块状格局，具有明显的空间变异性。土壤有机碳含量在垄作免耕处最高，达30．71g kg^-1，在常规平作处最低，为16．50g kg^-1左右。长期垄作免耕会导致有机碳向土壤表层大团聚体的相对富集及在土壤剖面的层次分异。 相似文献
11.
长期稻田垄作免耕对土壤性质和水稻产量的影响 总被引：4，自引：0，他引：4
A tillage method of combining ridge with no-tillage (RNT) was employed in lowland rice-based cropping system to study the long-term effects of RNT on soil profile pattern, soil water stable aggregate distribution, nutrients stratification and yields of rice and post-rice crops. After flooded paddy field (FPF) was practiced with RNT for a long time, soil profile changed from G to A-P-G, and horizon G was shifted to a deeper position in the profile. Also the proportion of macroaggregate (> 2 mm) increased, whereas the proportion of silt and clay (< 0.053 mm) decreased under RNT, indicating a better soil structure that will prevent erosion. RNT helped to control leaching and significantly improved total N, P, K and organic matter in soil. The highest crop yields were found under RNT system every year, and total crop yields were higher under conventional paddy-upland rotation tillage (CR) than under FPF, except in 2003 and 2006 when serious drought occurred. RNT was proven to be a better tillage method for lowland rice-based cropping system. 相似文献
12.
The effects of tillage on soil organic carbon (SOC) and nutrient content of soil aggregates can vary spatially and temporally, and for different soil types and cropping systems. We assessed SOC and nutrient levels within water‐stable aggregates in ridges with no tillage (RNT) and also under conventional tillage (CT) for a subtropical rice soil in order to determine relationships between tillage, cation concentrations and soil organic matter. Surface soil (0–15 cm) was fractionated into aggregate sizes (>4.76 mm, 4.76–2.00 mm, 2.00–1.00 mm, 1.00–0.25 mm, 0.25–0.053 mm, <0.053 mm) under two tillage regimes. Tillage significantly reduced the proportion of macroaggregate fractions (>2.00 mm) and thus aggregate stability was reduced by 35% compared with RNT, indicating that tillage practices led to soil structural change for this subtropical soil. The patterns in SOC, total N, exchangeable Ca2+, Mg2+ and total exchangeable bases (TEB) were similar between tillage regimes, but concentrations were significantly higher under RNT than CT. This suggests that RNT in subtropical rice soils may be a better way to enhance soil productivity and improve soil C sequestration potential than CT. The highest SOC was in the 1.00–0.25 mm fraction (35.7 and 30.4 mg/kg for RNT and CT, respectively), while the lowest SOC was in microaggregate (<0.025 mm) and silt + clay (<0.053 mm) fractions (19.5 and 15.7 mg/kg for RNT and CT, respectively). Tillage did not influence the patterns in SOC across aggregates but did change the aggregate‐size distribution, indicating that tillage affected soil fertility primarily by changing soil structure. 相似文献
13.
比较了4个施氮水平下免耕抛栽水稻和常耕抛栽水稻的群体质量及产量。结果表明,在127.5~193.0 kg/hm2施氮水平内,结实率随施氮水平的提高而降低,穗数、穗前干物质生产量、穗后干物质生产量、总干物质生产量、茎叶干物质表观输出量和表观输出率、植株高度、单茎重、粒叶比和根系活力随氮肥施用量的增加而增加,产量随施氮水平的提高而增加。1 9 3.0kg/hm2施氮处理的产量显著高于127.5 kg/hm2处理的。常耕抛栽水稻的有效穗数和粒叶比高于免耕抛栽水稻,但免耕水稻的干物质生产量、茎叶干物质表观输出量、茎叶干物质表观输出率、植株高度、单茎重、根系活力和颖花茎流量比常耕水稻的高,免耕抛栽水稻的群体质量略优于常耕抛栽水稻的。免耕抛栽水稻比常耕抛栽水稻增产2.10%,但差异不显著。 相似文献
14.
栽培方式对水稻氮素吸收利用与分配特性影响的研究 总被引：6，自引：2，他引：4
2006和2007年,在桶栽条件下,以早稻（三系籼型杂交稻金优253）为试材,应用15N示踪技术研究了稻草还田免耕、免耕、稻草还田常耕、常耕4种栽培方式对水稻氮素吸收利用与分配特性的影响。结果表明,1）水稻植株吸收的氮肥数量及其在体内的分配与土壤耕作方式密切相关; 免耕提高了水稻对肥料氮的吸收比率及在子粒和根中的分配比率,但降低了在叶和茎中的分配比率。2）免耕水稻产量和氮素吸收总量与常耕水稻差异不显著,但免耕水稻吸收的氮素中来源于肥料的比例比常耕水稻的大; 免耕水稻的氮肥回收效率高于常耕水稻,但氮素的稻谷生产效率差异不明显。3）稻草还田对氮肥的吸收利用有显著的影响。免耕条件下,稻草还田降低了基肥和分蘖肥氮素的积累量,增加了穗肥氮素积累量,氮肥总积累量呈下降趋势; 常耕条件下,稻草还田提高了各个时期的肥料氮素积累量,氮肥的总积累量增加显著。4）稻草还田提高了免耕水稻和常耕水稻产量,2007年其差异达显著水平。免耕条件下稻草还田降低了氮素的回收效率,但常耕条件下稻草还田提高了氮肥的回收效率。 相似文献
15.
耕作方式对土壤不同粒径团聚体氮素矿化的影响 总被引：4，自引：0，他引：4
研究了常规耕作和垄作免耕两种耕作方式下紫色水稻土不同粒径团聚体中氮的矿化过程。结果表明,不同粒径团聚体氮素矿化强度具有显著差异:潜在矿化势(Np)的最高值均出现在2.0～0.25 mm大团聚体中,最低值在>2.0 mm的宏团聚体中;2.0～0.25 mm团聚体的潜在矿化速率(Vp)和实际矿化速率(Va)比其他团聚体高1.2～1.6倍。常规耕作和垄作免耕两种耕作方式下不同团聚体的净矿化率随时间的变化趋势相同;垄作免耕显著增加了氮素的净矿化量,以原土为例:垄作免耕处理Np比常规耕作处理高33.9%,Vp和Va分别比常规耕作处理高85.2%和52.0%。虽然垄作免耕可以显著促进土壤中氮素的矿化作用,但是耕作方式对不同粒径团聚体内的氮矿化动力学过程并无显著影响,表明耕作方式对不同大小团聚体中可矿化氮和微生物的分布影响较小。 相似文献
16.
不同耕作方式与秸秆还田周年生产力的综合评价(简报) 总被引：9，自引：6，他引：3
该文通过3 a的定位试验,比较研究了稻麦两熟条件下免耕套种秸秆覆盖、免耕套种高茬、翻耕秸秆还田、翻耕秸秆不还田（对照,CK）4个处理对周年生产力的影响。结果表明：免耕套种的小麦产量降低,水稻产量增加,年产量略降,翻耕秸秆还田具较高产量生产力。如考虑节省的秧田种植小麦,则免耕套种的稻麦年产量可与翻耕秸秆还田持平。经技术经济分析,采用稻麦免耕套种秸秆还田,具有明显的节本增收、提高活劳动净产率的效果,在稻麦周年产量不减的同时,比翻耕秸秆不还田处理增收1874.8元/hm2,增加18.0%,经济生产力最高。翻耕秸秆还田比不还田有一定的增产增收效果,如果考虑到耕地持续生产力,秸秆还田后所带来的土壤肥力效应和减少肥料用量,其增产增收效果更为明显。从高产、高效、可持续发展等方面,运用综合评分法对稻麦两熟制不同耕作栽培方式周年生产力综合评价,免耕套种秸秆还田得分最高,周年生产力最好,免耕套种高茬和翻耕秸秆还田居中,翻耕秸秆不还田得分最低,周年生产力最差。 相似文献
17.
不同耕作方式对水稻产量和土壤肥力的影响 总被引：12，自引：0，他引：12
于2005～2006年在双季稻田研究了不同耕作方式对水稻生长、产量和土壤肥力的影响。结果表明:免耕抛秧水稻根干重低于翻耕移栽稻,根系绝大部分分布在表层土壤,根系活力比翻耕处理的高,分蘖时间比翻耕移栽的早而比翻耕抛秧的迟;每公顷有效穗数略低于翻耕抛秧而高于翻耕移栽,结实率高于翻耕处理。随着免耕次数的增加,各处理产量基本持平;免耕1年有利于土壤物理性质的改善,免耕有利于土壤养分在表层土壤富集。 相似文献
18.
This study was conducted to determine a tilth index from tillage induced soil physical properties and grain yield to optimize tillage in rice–wheat system. The experiment was conducted in a silty clay loam (Aquic hapludoll) associated with a shallow water table fluctuating between 0.02 and 0.96 m from the surface. Tillage treatments for rice were puddling by four passes of rotary puddler (PR), reduced puddling (ReP), conventional puddling (CP) and direct seeding without puddling (DSWP) in four replications. Tillage treatments for wheat were zero tillage (ZT) and conventional tillage (CT) superimposed over the plots of rice tillage treatments. Measurements were made of puddling index and specific volume (only in the rice season), bulk density, saturated hydraulic conductivity, infiltration rate, plasticity index, porosity and organic carbon in the rice and wheat seasons. Rice yield in the PR plots was highest and statistically equal to that in the ReP plots but wheat yield was highest in the DSWP plots under ZT condition and was statistically equal to that in the ReP plots.Tilth index (TI) was determined in two ways: one by the model suggested by Singh et al. [Trans. ASAE 35 (6) (1992) 1777] and the second by a proposed regression model. The proposed regression model utilizes soil physical properties having significant influence on crop yield. As per the Singh et al. model, wheat yield increased linearly with increasing TI from 0.75 to 0.89 but rice yield decreased with increasing TI from 0.67 to 0.81. Both TI and its relation with rice yield were contrary to their observations. The proposed regression model showed a value of TI in the range of 0.74–0.87 for rice soils and 0.86–1.0 for wheat soils as indicators of TI for optimum yields of rice and wheat. A high TI corresponds to low tillage both for rice and wheat. The optimum yield with minimum tillage operations coincided with TI obtained in ReP plots of rice and in ZT plots of wheat under ReP conditions. Results thus show that the quality of soil puddle obtained by half the efforts in PR and CP was sufficient for optimum yields of rice. Similarly, wheat sowing by zero-till drill in such a reduced puddling plots of rice was sufficient for optimum yields of wheat in Tarai soils associated with shallow water tables. The proposed regression model is simple and compatible to use in the existing crop growth models, such as in DSSAT 3.5, with suitable alterations. 相似文献
19.
Marcela Pacola Tiara Moraes Guimarães João Paulo Gonsiorkiewicz Rigon Lucas Moraes Jacomassi João William Bossolani Josiane Viveiros Gabriela Ferraz de Siqueira Patrícia Pereira Dias Juliano Carlos Calonego Carlos Alexandre Costa Crusciol 《Soil Use and Management》2023,39(4):1388-1402
Combining deep tillage (DT) with lime application at greater depths may improve sugarcane yield. The objective of this study was to evaluate the impact of conventional tillage (CT) and DT systems and liming on sugarcane productivity and soil physical attributes. The experiment was conducted in a clayey-textured Rhodic Hapludox soil cultivated with sugarcane for two growing seasons (first and third ratoons) using a randomized block design with four treatments and four repetitions. The treatments consisted of DT without liming (DT0), DT with liming (DT2), CT without liming (CT0) and CT with liming (CT2). In addition to sugarcane stalk and sugar yields, macroporosity (MA), microporosity (MI), total soil porosity (TP), weighted average diameter (WAD), aggregate stability index (ASI), soil penetration resistance (SPR), pH, potential acidity (H + Al), total soil organic carbon (SOC), particulate organic carbon (POC), mineral-associated organic carbon (MOC), calcium (Ca) and magnesium (Mg) were analysed. DT2 promoted the best soil conservation effect on sugarcane. In general, DT, regardless of lime application, reduced SOC and POC in soil surface layer. Nevertheless, in the long term, localized lime addition resulted in significant reductions in compaction, reaching values below 2 MPa. The soil fertility improvement provided by DT2 promoted increased sucrose concentrations and stalks yield. Considering that there was an improvement in the physical quality and fertility of soil for better plant development, the deep tillage with localized lime addition can be considered an effective alternative for sugarcane cultivation. 相似文献
20.
Kathrin Rosner Karin Hage-Ahmed Gernot Bodner 《Archives of Agronomy and Soil Science》2020,66(12):1679-1691
ABSTRACT We conducted a field- and pot experiment with peas to investigate the impact of soil tillage and herbicide applications on arbuscular mycorrhizal fungi (AMF), plant growth, phosphorus concentrations, C:N ratio in plants and yield. The field study was carried out in a long-term soil tillage experiment where four tillage treatments have been compared. Field soil from the experimental plots were used for the pot experiment. AMF were not affected by herbicide (MCPB) application, neither in the field nor in the pot experiments. However, AMF root colonization was enhanced by reduced tillage, minimum tillage and no-tillage practices, compared to conventional tillage. In the pot experiment, plant growth and nodulation of pea roots was negatively affected by the high herbicide dosage. In the field experiment neither tillage nor herbicide treatment exert specific effects on root growth parameters, phosphorus concentrations, C:N ratio and plant dry matter. This work demonstrates that an appropriate herbicide usage coupled with conservation soil tillage techniques can favour AMF root colonization and benefit plant growth. Abbreviations: AMF: arbuscular mycorrhizal fungi; CT: conventional tillage; RT: reduced tillage; MT: minimum tillage; NT: no tillage; P: Phosphorus; C:N ratio: carbon:nitrogen ratio 相似文献