羊草草原植物－土壤之间主要营养元素动态的研究

羊草草原土壤中Ｎ、Ｐ、Ｋ含量的季节变化规律是生长季初期较高,６－８月生长旺季较低,生长季末再度升高。营养元素在植物体内的分配是地下部分大于地上部分。地下部分Ｎ的贮量为地上部分的３．６倍,Ｋ为２．９倍,Ｐ为２．８倍。地上部分３种元素含量的季节变化曲线呈单峰型,从生长初期开始上升,最大值出现在８月,生长末期逐渐下降。地下部分的季节变化规律,大体上在整个生长季内呈上升趋势,随着根系的生长,营养元素的积累量不断增加。对植物－土壤之间营养元素动态分析结果表明,随着时间的推移,Ｎ、Ｐ、Ｋ在备状态中的比例趋于恒定。在稳定状态下,３种元素在土壤中的比例逐渐减少,与初始量相比Ｎ、Ｐ、Ｋ的含量分别减少２１．２３％、５．１４％和２．９９％。在其它状态中,３种元素的含量均有提高,特别在枯枝落叶和死根中增加的幅度较大。     

羊草及羊草割草地营养元素的动态研究

本文分析测定了羊草(Leymus chinense)及羊草割草地营养元素的动态变化。结果表明,羊草对N、Mg、Ca、K元素的吸收量大,对Cu元素的吸收量小。羊草对各营养元素的吸收量和积累量以生长初期最高,以后随时间推移,其积累量逐渐下降,但Na元素于生长初期至中期含量一直较低,至生长末期出现急剧增加趋势。Cu在整个生长期中含量都很低,随时间变动不大。 在羊草割草地中,羊草从割草地土壤中吸收营养元素量为40.7kg·ha~(-1)·a~(-1),羊草割草地由于刈割羊草地上部分而输出的营养元素量为25.71kg·ha~(-1)·a~(-1),而羊草凋落物与茎茬中残留的营养元素量为10.58kg·ha~(-1)·a~(-1),归还土壤的营养元素量为4.02kg·ha~(-1)·a~(-1)。由此可见,羊草割草地营养元素的输出量大于输入量,这是永久性羊草割草场土壤肥力日趋下降、草原退化、生产力逐渐降低的重要原因之一。     

羊草群落主要营养元素吸收相关性分析

在羊草（Ａｎｅｕｒｏｌｅｐｉｄｉｕｍｃｈｉｎｅｎｓｅ）群落中,钾与钙、镁、锰、铜、锌五种元素的含量变化之间具倒数关系;钙、镁、锰、铜、锌五种元素间存在着相互制约关系;其中,钙与镁、铜之间的关系密切（ｒ）０．９）;羊草群落吸收较多的钙可防止锰、铜和镁的毒害作用,并对钾的吸收有促进作用．     

羊草草地枯枝落叶中N,P,K变化动态

羊草草地枯枝落叶中Ｎ、Ｐ、Ｋ变化动态郭继勋,祝廷成（东北师范大学国家草地生态工程实验室,长春１３００２４）ＤｙｎａｍｉｃｓｏｆＮ,ＰａｎｄＫｉｎｌｉｔｔｅｒｓｏｎＡｎｅｕｒｏｌｏｐｉｄｉｕｍｃｈｉｎｅｎｓｅｇｒａｓｓｌａｎｄ．￥ＧｕｏＪｉｘｕｎａｎｄ...     

农林业系统沙兰杨-小麦、玉米群落类型氮、磷、钾营养元素循环的研究

农林业系统沙兰杨-小麦、玉米群落类型N、P、K营养元素循环研究结果表明:在整个群落中,元素N和P发生损亏,K基本平衡。在植物组分库和枯落物库中,元素N、P、K均发生累积;在土壤库中,元素N、P和K均发生亏损。土壤表层(0—20cm)N的含量是限制农作物正常生长发育的主要环境因子。土壤库中有效N和速效P的含量是限制沙兰杨正常生长发育的主要环境因子。群落的年输入输出量大,枯落物少,营养元素在各组分间的循环量大等是该群落类型营养元素循环的重要特性。     

内蒙古羊草草原群落主要植物的热值动态

对内蒙古羊草草原主要植物种群的干重热值动态研究表明,热值随植物种类,植物部位,取样时植物所处物候期及气候条件的不同而变化,羊草草原主要植物种群地上部分热值的变动范围在15703－18141J／g之间,其中灌木小叶锦鸡儿（Caragang microphylla)的热值最高,禾草类植物的热值多数较高,而大多数杂类草的热值相对较低,主要植物种群地下部分热值的分布范围为15051－16410J/g。其中根茎型草地下部分热值较高。不同种类植物地下部分热值差异并不与地上部分一致,根茎型禾草地上、地下部分热值差异较小,而须根型植物差异较在,不同种群的植物地上部分热值随植物候期的不同而波动,其变化规律是与植物种群本身的生物学特性相联系的,不同植物种群热值的年际小 规律有所不同,羊草（Leymus chinensis)、大针茅（Stipa grandis)和洽草（Koeloria cristata)的年际热值波动相关显著。但与生长季降水量和生长季累积日照时数之间无明显相关性,在某种程度上,植物热值的 种内变化反映了植物生长状况的差异。     

东北羊草草原主要植物热值

 对羊草(Aneurolepidium chinense)草原55种植物热值进行分析,高热值植物占总数的20％,中热值植物占58.18％,低热值植物占21.82％,55种植物全株平均热值为17949.45J·g-1。因含能物质在各器官的分配不同,同一植物不同器官的热值也存在着差异。务器官的平均热值花19399.28J·g-1>茎18022.58J·g-1>叶17885.17J·g-1>根17206.05J·g-1。不同科植物全株和各器官平均热值存在较大差异,即使同属植物也存在一定差异。菊科、禾本科和豆科3大科植物全株平均热值无明显差异,但豆科植物根的热值明显高于禾本科和菊科根的热值。     

海甘蓝生长过程中植株体内矿质营养元素动态的研究

我们在法国西部的昂热市（Ａｎｇｅｒｓ）试验研究了海甘蓝在不同生长时期内植株生长量、体内矿质营养元素含量、植株对不同营养元素的吸收量的动态变化。结果表明,海甘蓝在５个月生长期内的田间总生长量为１２．２２ｔ·ｈｍ－２（干物质）,移栽后各月内海甘蓝的生长量大小顺序为第五个月＞第三个月＞第二个月＞第四个月＞第一个月。海甘蓝植株体内Ｂ、Ｓ、Ｃａ和Ｐ的含量以移栽后的第二个月最高,第五个月最低;Ｃｕ、Ｆｅ和Ｍｎ含量在第一个月最高,其它时期变化不大;Ｚｎ和Ｍｎ含量随移栽后的时间增加而降低;Ｎａ和Ｋ含量在整个生长季节内均无明显变化。在整个生长季节内,海甘蓝对各种矿质营养元素的总吸收量的大小顺序为Ｋ＞Ｃａ＞Ｓ＞Ｐ＞Ｎａ＞Ｆｅ＞Ｍｎ＞Ｚｎ＞Ｂ＞Ｃｕ。不同生长期,植株对多数营养元素的吸收量的大小顺序为第五个月＞第三个月＞第二个月＞第四个月＞第一个月     

氮磷添加对荒漠草原植物-凋落物-土壤生态化学计量特征的影响

为明确植物、凋落物和土壤养分含量及化学计量比对土壤中添加多种限制性养分的响应,阐明“植物-凋落物-土壤”连续体化学计量动态及各组分之间的协同作用,以宁夏荒漠草原为研究对象,于2018年开始进行氮(N)、磷(P)养分添加控制试验。试验处理包括对照(CK)、N添加、P添加、NP共同添加4个处理。结果表明：(1)NP共同添加显著增加了荒漠草原植物N和P含量、以及凋落物和土壤P含量,显著降低了荒漠草原植物C∶N和C∶P、以及土壤和凋落物C∶P和N∶P。P添加显著增加了荒漠草原植物、凋落物和土壤P含量,显著降低了植物、凋落物、土壤C∶P和N∶P。N添加分别增加了植物、凋落物N含量和N∶P,但对植物N含量影响未达到显著水平。(2)C、N、P含量和N∶P大小均表现为植物>凋落物>土壤,C∶N和C∶P均表现为凋落物>植物。(3)N添加提高了荒漠草原植物对P再吸收效率,降低了荒漠草原植物对N利用效率;P添加提高荒漠草原植物对N再吸收效率,降低荒漠草原对P的利用效率;NP共同添加提高了荒漠草原植物对N和P再吸收效率,降低了荒漠草原植物对N和P利用效率。(4)植物-凋落物-土壤的N、P含量...     

利用叶绿素荧光评估草原植物羊草缺磷缺氮状况北大核心CSCD

羊草(Leymus chinensis)是北方草原的重要牧草。准确评估其营养状况,对维护羊草草原的生产力具有重要意义。以羊草幼苗为材料,利用能同时表征2个光系统光化学活性的叶绿素荧光检测技术,对缺氮和缺磷处理下的叶片光化学活性进行分析。结果表明,缺氮处理20天后羊草叶片叶绿素含量降低近50%。同期缺磷及缺氮处理对PSⅡ功能的影响总体大于PSⅠ。与对照相比,缺氮叶片的Φ(Ⅱ)和Φ(Ⅰ)分别比对照降低了30.3%与38.5%;ETR(Ⅱ)与ETR(Ⅰ)分别降低30.8%和28.9%。缺磷处理组Φ(Ⅱ)和ETR(Ⅱ)的降低幅度约为缺氮的1/2。这些定量研究结果对及时有效地诊断和区分羊草植物氮磷缺乏状况具有重要的参考价值。     

羊草草地枯枝落叶中N、P、K变化动态

On Aneurolepidium chinease grassland, the amounts of N, P and Ktransferred from deadplants into the litters are respectively 0.7227, 0.1137 and 0.4974g·m^-2·yr^-1.After oneyear, the loss rates of them are respectively 59.71, 73.21 and 83.26%.Under imbalancestate, the input of these three elements is larger than their output, being at accumulationstage, while under stable state, their contents in litters are respectively 1.1859, 0.1565 and 0.5963g·m^-2.     

Seasonal and spatial patterns of foliar nutrients in cork oak (Quercus suber L.) growing on siliceous soils in Provence (France)

Cork oak forests in Mediterranean, southeastern France represent animportant ecosystem in terms of both ecological and economical values, but aredeclining due to conservation problems. While management protocols are now inplace for the long-term conservation of this ecotype, we require a betterunderstanding of cork oak nutrition to assist with management. Here we usefoliar nutrient analyses for two objectives: firstly, to assess to what extentvariations in nutrient content are explained by seasonal and spatialvariability, and second, to document the nutrient dynamics of cork oak trees innatural conditions during one biological cycle (16 months) in the Maures massif(western part of the siliceous Provence). Main results showed that time was theprimary factor influencing cork oak nutrition and was mainly expressed by leafageing process. Spatial variability was a 'secondary determinant' of nutrient variations, but was more important at the very early stages of leafgrowth according to leafing and nutrient flushing, and reduced with leaf age.Nutritional responses of cork oak trees fitted general trends observed in theliterature, with some regional differences. The properties of siliceous soilalso influenced the uptake of some nutrients.     

羊草＋杂类草群落数量特征季节动态的研究

本文对肇州羊草＋杂类草群落主要种群、种组及群落数量特征季节动态进行了探讨。结果表明,在生长季内,羊草、蔓委陵菜群种及丛生禾草种组高度和盖度,群落的盖度及密度特征呈单峰型变化,群落最大地上生物量出现在８月５日,其值为１９７３ｇ／ｍ２干物质,而后下降;在生长季内,符合拓广了的Ｌｏｇｉｓｔｉｃ模型增长,其模型为：Ｂ＝２２４６０３８１＋ｅ５．９２８９－５．５３８８×１０２·ｔ－４．８４８４×１０４·ｔ２＋３．５３６５×１０－６·ｔ３     

Influence of Nutrient Availability on the Interaction Between Spotted Knapweed and Bluebunch Wheatgrass

Centaurea maculosa (Lam.) (spotted knapweed) reduces wildlife and livestock habitat biodiversity and increases erosion. Nutrient availability to plants may be used to accelerate succession away from spotted knapweed. Early‐successional plant communities often have high nutrient availability, whereas late‐successional communities are often found on lower nutrient soils. We hypothesized that removal of nutrients would change the competitive advantage from spotted knapweed to Pseudoroegneria spicatum (bluebunch wheatgrass) (late seral). In two addition series matrices, background densities of Secale cereale (annual rye) and Elymus elimoides (bottlebrush squirreltail) (3,000 seeds/m²) were used to remove nutrients from the soil. In another set of addition series matrices, nitrogen (33 kg/ha) or phosphorus (33 kg/ha) were added to the soil. Nutrient analysis of soil and vegetation indicated that annual rye and bottlebrush squirreltail reduced nutrient availability in soils. In another matrix, neither a background density nor nutrients were added. Data were fit into Watkinson's curvilinear model to determine the competitive relationship between bluebunch wheatgrass and spotted knapweed. This allowed comparison of the equivalence ratios (C) generated from each addition series. The C parameters are the per‐plant equivalent of bluebunch wheatgrass or spotted knapweed and can be interpreted as the ratio of intra‐to‐interspecific competition. The C parameters are also the equivalence ratio of the number of spotted knapweed it takes to have equivalent effect on bluebunch wheatgrass or the number of bluebunch wheatgrass having the equivalent effect on spotted knapweed. Without nutrient manipulation, spotted knapweed was more competitive than bluebunch wheatgrass. The C for bluebunch wheatgrass was 0.17, indicating that 0.17 knapweed plants were competitively equivalent to one wheatgrass. Annual rye changed the competitive balance in favor of bluebunch wheatgrass (C = 9.9). Addition of nitrogen, phosphorus, or the mid‐seral species did not change the competitive relationship between the two species. This preliminary study suggests that succession from spotted knapweed to late‐seral bluebunch wheatgrass community may be accelerated by altering resource availability.     

菜地和一般农田土壤主要养分累积的差异

选取不同类型菜地和一般农田 ,测定了 0～ 2 0 0cm土壤剖面的有机质、全氮、硝态氮、铵态氮、速效磷、速效钾等主要养分含量及其分布 .结果表明 ,菜地土壤中养分大量累积 ,其中硝态氮和速效磷累积程度较高 .大棚和露天菜地 0～ 2 0 0cm土层的硝态氮累积总量分别为 15 2 0 .9kg·hm-2 和 135 8.8kg·hm-2 ,比农田高出 5 .2和 4.5倍 ;速效磷分别为 978.1kg·hm-2 和 5 0 3.3kg·hm-2 ,比农田高出 6 .2和 2 .7倍 .而其它养分增加相对较少 .有机质累积总量分别为 2 80 .5Mg·hm-2 和 2 6 9.3Mg·hm-2 ,比一般农田高出 12 .5 %和 8.0 % ;全氮分别为 37.5Mg·hm-2 和 32 .7Mg·hm-2 ,比农田高出 36 .2 %和 18.6 % ;铵态氮分别为 2 11.5kg·hm-2 和 197.8kg·hm-2 ,比农田高出 2 9.6 %和 2 1.2 % ;速效钾分别为 6 5 6 7.8kg·hm-2 和 5 5 2 3 .6kg·hm-2 ,比农田高出 30 .6 %和 9.8% .此外 ,菜地土壤中累积的养分不仅分布在表层 ,在深层土壤也大量存在 ,说明菜地存在严重的养分淋溶现象 .     

Long-term effects of drainage and hay-removal on nutrient dynamics and limitation in the Biebrza mires,Poland

To provide a reference for wetlands elsewhere we analysed soil nutrients and the vegetation of floodplains and fens in the relatively undisturbed Biebrza-valley, Poland. Additionally, by studying sites along a water-table gradient, and by comparing pairs of mown and unmown sites, we aimed with exploring long-term effects of drainage and annual hay-removal on nutrient availabilities and vegetation response. In undrained fens and floodplains, N mineralization went slowly (0–30 kg N ha⁻¹ year⁻¹) but it increased strongly with decreasing water table (up to 120 kg N ha⁻¹ year⁻¹). Soil N, P and K pools were small in the undisturbed mires. Drainage had caused a shift from fen to meadow species and the disappearance of bryophytes. Biomass of vascular plants increased with increasing N mineralization and soil P. Annual hay-removal tended to have reduced N mineralization and soil K pools, but it had increased soil P. Moreover, N concentrations in vascular plants were not affected, but P and K concentrations and therefore N:P and N:K ratios tended to be changed. Annual hay-removal had induced a shift from P to K limitation in the severely drained fen, and from P to N limitation in the floodplain. The low nutrient availabilities and productivity of the undisturbed Biebrza mires illustrate the vulnerability of such mires to eutrophication in Poland and elsewhere. In nutrient-enriched areas, hay removal may prevent productivity increase of the vegetation, but also may severely alter N:P:K stoichiometry, induce K-limitation at drained sites, and alter vegetation structure and composition.