黄淮海平原农林生态系统N、P、K营养元素循环——以泡桐-小麦、玉米间作系统为例

农林生态系统泡桐-小麦、玉米间作类型N、P、K营养元素循环研究表明,在整个群落中,P发生亏损,N和K基本平衡;在植物组分库和枯落物库中,N、P、K均发生累积;在土壤库中,N、P、K均发生亏损。土壤表层(0—20cm)中N和P的含量是限制农作物生长的主要因子。20—80cm土层中P的含量是限制泡桐生长的主要因子。群落内N、P、K的吸收系数分别为0.078、0.014、0.052,利用系数分别为0.95、0.90、0.94,循环系数分别为0.042、0.05、0.063.     

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。     

深圳福田红树林无瓣海桑+海桑群落N、P、K累积和循环

研究了深圳福田红树林无瓣海桑 +海桑群落的 N、P、K元素的累积和循环。结果表明 ,该群落 N、P、K元素的现存累积量分别为 :3 8694.92、 5 848.62、 5 0 861 .47mg/m2 ,其中地下部分分别占 2 8.5 9%、41 .77%、 42 .0 8%。该群落氮、磷、钾元素生物循环中 ,年吸收量分别为 :1 3 2 40 .0 95、 1 887.70 5、 2 0 73 6.1 1mg/m2 ;年归还量分别为 :62 70 .5 85、 979.1 75、 63 5 3 .948mg/m2 ;年存留量分别为 :6969.5 1、 90 8.5 3、 1 43 82 .1 62 mg/m2 ;周转期分别为 :7a、6a、9a。群落各组分的氮含量最高 ,磷含量最低。     

无牧草原生态系统营养元素的生物地球化学特征

以内蒙古锡林河流域的两种优势草原群落羊草草原和大针茅草原为研究对象,探讨了中纬度地区未放牧情况下的草原生态系统植物营养元素的生物地球化学特征．结果表明,两类草原群落土壤-植物系统中土壤分室N、P、K、S、Ca、Mg、Si的贮量远大于植物亚系统的贮量,地上活体和枯草分室的各元素贮量小于根分室．在两类草原群落中,N、P、K、S从枯草分室中消失的速率要大于Ca、Mg和Si．羊草草原的枯草分室元素流失量大于大针茅草原．研究区草原生态系统中,羊革草原物质的生物地球化学循环近于平衡状态,大针茅草原处于失衡状态．物质循环量羊草草原远大于大针茅草原．     

草基-鱼塘生态系统的能量转化与养分循环研究

应用模拟试验的方法,研究了“草基-鱼塘”系统中的能量转化与养分循环.结果表明,该系统中饲草对太阳能的利用率为0.83%,鱼对饲料能的转化率为7.3%.与以粮食作为鱼饲料比较,单位面积草地的产鱼当量是粮食作物的1.6倍.鱼对饲料N、P、K的转化率分别为16.8%、32.3%和2.0%.塘泥沉积的N、P分别占饲料的23.4%和56.1%;猪对饲料N、P、K的转化率分别为20.5%、33.7%和4.6%,猪粪尿回收饲料N为36.4%、P为63.8%、K为39.4%.猪-草-鱼结合的基塘系统其能量和养分转化效率均高于单一的养鱼系统.     

缙云山森林土壤速效N、P、K时空特征研究

研究了缙云山森林生态系统内4个演替阶段群落的土壤速效N、P、K的时空特性,结果表明：①除灌草丛的速效K外,速效N、P、K含量在不同群落的土壤剖面上均具有明显的层次性,即腐殖质层（A）＞沉积层（B）＞母质层（C）。②A、B两层的速效N、K含量随群落演替方向升高,即灌草丛＜针叶林＜针阔混交林＜常绿阔叶林,速效P含量则为：针叶林＜针阔混交林＜灌草林＜常绿阔叶林。C层速效N、P、K含量似乎与群落演替规律无必然联系。③各群落内A、B层土壤速效N、P、K含量均表现出明显的季节动态,动态规律因元素类型和土壤层次而有差别。     

不同生境下骆驼刺与花花柴生态化学计量学特征的比较

以塔克拉玛干沙漠南缘典型荒漠豆科植物骆驼刺(Alhagi sparsifolia)和菊科植物花花柴(Karelinia caspia)为对象,研究单一骆驼刺种群(LTC)、单一花花柴种群(HHC)及骆驼刺-花花柴群落(GSQL)中植物及土壤中碳(C)、氮(N)、磷(P)、钾(K)等养分的生态化学计量学特征。结果表明:骆驼刺-花花柴群落中土壤有效N(AN)、有效K(AK)含量及N∶P、N∶K显著高于单一花花柴种群;骆驼刺-花花柴群落中花花柴叶片的全N含量显著高于单一花花柴种群,骆驼刺-花花柴群落中骆驼刺叶片的全P含量显著高于单一骆驼刺种群。相关性分析显示:不同生境土壤的AK含量与N∶P及AN含量呈显著正相关,而与SOC呈负相关;不同生境下叶片中的全K含量与SOC、全N、全P含量呈显著正相关,叶片中的全N含量与SOC、全P亦呈显著正相关,而N∶P与SOC、全P含量呈显著负相关;土壤中SOC含量与叶片中全P、全K含量呈正相关,而与N∶K呈负相关;土壤有效N含量与叶片N∶K呈正相关,而与叶片4种元素含量均呈显著负相关;土壤有效K含量与叶片中4种元素含量均呈显著负相关,而与叶片N∶K呈正相关;土...     

天坑森林植物叶-凋落物-土壤C、N、P生态化学计量特征

为探究广西乐业大石围天坑森林群落的C、N、P养分循环特征,比较了天坑内外森林群落的植物叶片-凋落物-土壤C、N、P含量及其化学计量比,采用相关性分析和冗余分析等统计方法研究其内在联系和相互影响。结果表明,与天坑外部森林相比,天坑内部森林植物叶片和凋落物呈现出C低N、P高,土壤为C、N低P高的格局。植物叶片C:N、C:P与凋落物C、N:P显著正相关,植物叶片C与土壤P显著负相关;天坑外部森林的植物叶片N、N:P与土壤N:P显著负相关,植物叶片C:N与土壤C、C:N显著正相关,说明天坑森林内部凋落物的C、P养分可能主要来源于植物叶片,而天坑外部森林的植物叶片C、N主要来自土壤。土壤C:N:P对植物叶、凋落物的C:N:P变化的解释率分别为90.7%和50.6%,其中土壤P对植物叶和凋落物的C:N:P计量特征变化的解释度最高,坑内生境植物对P含量变化更为敏感、坑外植物对于N含量变化更为敏感,表明天坑内部森林可能是P素受限位点、天坑外部森林是N素受限位点。喀斯特天坑内部森林和外部森林植物叶-凋落物-土壤的C:N:P的差异和联系,体现了天坑内外森林群落的养分循环特征和植物群落的适应性。     

红松阔叶混交林凋落物-土壤动物-土壤系统中N、P、K的动态特征

根据对小兴安岭凉水国家级自然保护区红松阔叶混交林的凋落物、土壤动物和土壤2a的连续采样及测定主要营养元素N、P、K的含量,研究凋落物-土壤动物-土壤系统中主要营养元素在各分室的动态变化,并通过比较主要营养元素在不同分室中的分异,进而分析了土壤动物在该系统营养循环中的作用。结果表明,研究区内不同凋落叶分解过程中元素含量的动态变化比较复杂,阔叶落叶中营养元素含量的变化大于针叶落叶,但不同凋落叶在分解过程中的元素损失量之间的差异不显著。在研究时段,腐殖土层各种营养元素的含量高于土壤层;蚯蚓、蜈蚣和马陆大型土壤动物体内的营养元素含量之间差别较大,其中蚯蚓体内全N含量最高,而马陆体内全P含量最高,蜈蚣则全K含量最高。土壤动物和土壤中营养元素含量的动态变化和凋落叶中的变化趋势不同。N和P在土壤动物分室中表现出一定的富集,而K的富集不明显。土壤动物可以通过其新陈代谢活动加速凋落物-土壤动物-土壤系统中营养元素的循环速率。不同凋落物分解过程中养分含量变化复杂可能是由于不同凋落物种类特性差异造成的。土壤动物在营养元素循环,尤其是N、P元素循环中具有重要意义。     

福建武夷山黄山松群落的氮、磷累积和循环

本文是福建武夷山森林生态系统研究的一部分,主要讨论黄山松（Pinustaiwanensis）群落的氮磷累积和循环。测定结果表明：（1）群落现存量中氮（N）、磷（P）的库量分别为925．844kghm-2和45．981kghm-2,其中地上部分别为719．438kghm-2（占总库量的77．706%）和35．534kghm-2占77.280％）,地下部分别为206．406kghm-2（占22．294％）和10．447kghm-2（占22.720％）;（2）N、P的生物循环中,年吸收量分别为65．344kghm-2和2627kghm-2,年存留量分别为37．019kghm-2和1．695kghm-2,年归还量分别为28．325kghm-2和0.932kghm-2;（3）氮、磷的富集率分别为1．324和1．083两者均大于1,说明该群落对N、P仍在不断累积。     

农林生态系统中营养元素N,P,K流动的网络分析

对农林业系统沙兰杨－小麦－玉米群落类型中Ｎ、Ｐ、Ｋ流动网络分析表明,系统中Ｎ、Ｐ、Ｋ的循环指数分别为０．０７１、０．０３９、０．１３９,均小于传统的循环系数（ＣＣ等于回归量／吸收量）,而在群落中的总滞留时间分别为２２．４１、７９．７２、２６．５７ａ．     

草基—鱼塘生态系统的能量转化与养分循环研究

应用模拟试验的方法,研究了“草基-鱼塘”系统中的能量转化与养分循环．结果 表明,该系统中饲草对太阳能的利用率为 ０． ８３％,鱼对饲料能的转化率为 ７． ３％．与以粮 食作为鱼饲料比较,单位面积草地的产鱼当量是粮食作物的１．６倍．鱼对饲料Ｎ、Ｐ、Ｋ的 转化率分别为１６．８％、３２．３％和２．０％．塘泥沉积的Ｎ、Ｐ分别占饲料的２３．４％和５６．１％; 猪对饲料 Ｎ、 Ｐ、 Ｋ的转化率分别为 ２０． ５％、 ３３． ７％和 ４． ６％,猪粪尿回收饲料 Ｎ为 ３６． ４％、 Ｐ为 ６３． ８％、 Ｋ为 ３９． ４％．猪-草-鱼结合的基塘系统其能量和养分转化效率均高于单一的 养鱼系统．     

香港芒萁群落养分的研究

本文研究香港芒萁群落养分的分配、季节动态和循环。研究结果表明：(1)N、P、K浓度在活物质大于死物质,地上部分大于地下部分。(2)植物的养分贮量是活物质大于死物质,地下部分大于地上部分。(3)当年生芒萁地上部养分贮量随生物量的增加而增加,但是,干物质生产率超过养分吸收率,使得N、P、K浓度由于生物量的增加而降低。(4)虽然芒萁群落的净第一性生产力大于其邻近的草地和灌木林,但其净第一性生产量中的N和P量却小于灌木林。(5)以土壤中的总N和总P来计算,生态系统中的N和P主要贮存于土壤库中,但以土壤有效K来计算,则有大约36％～50％的K贮存于植被中。(6)在研究期间,立枯体和死地被物中的N、P、K贮量逐渐增加,这表明在火灾后生态系统的立枯体和死地被物养分库有一个累积过程。(7)N、P、K通过枯枝落叶的归还量分别占它们在地上部净第一性生产量中的49.1％、30.8％和13.1％,而地上部净第一性生产量中的N和P的31.2％和46.6％来自于养分的内部循环。     

Atmospheric deposition of nutrients in a coastal maquis ecosystem of northeastern Greece

The deposition of nutrients N, P, Ca, Mg, Na and K from the atmosphere on a coastal maquis ecosystem was studied over a 12-month period (1981–1982). The annual precipitation during that period was 1065 mm. Nutrient input was estimated as 5.72, 0.24, 30.31, 3.40, 23.99 and 1616 kg ha^–1 year^–1 for N, P, Ca, Mg, Na and K, respectively. Chemical analysis of throughfall showed enrichment for all the nutrients studied. It was concluded that nutrient input from bulk precipitation is an important contribution to nutrient cycling of the Greek maquis ecosystem.     

Increased resource use efficiency amplifies positive response of aquatic primary production to experimental warming

Climate warming is affecting the structure and function of river ecosystems, including their role in transforming and transporting carbon (C), nitrogen (N), and phosphorus (P). Predicting how river ecosystems respond to warming has been hindered by a dearth of information about how otherwise well‐studied physiological responses to temperature scale from organismal to ecosystem levels. We conducted an ecosystem‐level temperature manipulation to quantify how coupling of stream ecosystem metabolism and nutrient uptake responded to a realistic warming scenario. A ~3.3°C increase in mean water temperature altered coupling of C, N, and P fluxes in ways inconsistent with single‐species laboratory experiments. Net primary production tripled during the year of experimental warming, while whole‐stream N and P uptake rates did not change, resulting in 289% and 281% increases in autotrophic dissolved inorganic N and P use efficiency (UE), respectively. Increased ecosystem production was a product of unexpectedly large increases in mass‐specific net primary production and autotroph biomass, supported by (i) combined increases in resource availability (via N mineralization and N₂ fixation) and (ii) elevated resource use efficiency, the latter associated with changes in community structure. These large changes in C and nutrient cycling could not have been predicted from the physiological effects of temperature alone. Our experiment provides clear ecosystem‐level evidence that warming can shift the balance between C and nutrient cycling in rivers, demonstrating that warming will alter the important role of in‐stream processes in C, N, and P transformations. Moreover, our results reveal a key role for nutrient supply and use efficiency in mediating responses of primary producers to climate warming.     

Ecological Stoichiometry of Microbial Biomass Carbon,Nitrogen and Phosphorus on Bauxite Residue Disposal Areas

Abstract

Ecological succession by microbial activity on bauxite residue disposal areas (BRDAs) would accumulate nutrients and convert the residue into a soil-like material. However, the role of microorganisms in nutrient cycling remains elusive on BRDAs. Carbon (C), nitrogen (N) and phosphorus (P) ecological stoichiometry is a critical indicator of nutrient cycling in an ecosystem. In order to investigate the changes in nutrients following long-term natural weathering process, the contents of C, N, P, microbial biomass carbon (MBC), nitrogen (MBN), and phosphorus (MBP) were measured in chronological stacks of bauxite residue. Deeply, their ecological stoichiometric characteristics were analyzed. Compared to freshly stacked residue, organic carbon (OC), total nitrogen (TN) and available phosphorus (AP) have increased 89%, 1640%, and 369% after 20?years, respectively. The C/N in 20-year-old residue (BR20) is 12.41, which close to the mean range of soil C/N in China. Bauxite residue C/P and N/P increased significantly with the stacking age increased. MBC/MBN decreased from 6.75 to 4.52 after stacked for 5?years, whilst MBC/MBP increased from 23.74 to 59.16 with stacking age. Data analysis of C, N, P and MBC, MBN, MBP in bauxite residue correlated significantly, indicating that microbial biomass can be used as a biological indicator to evaluate bauxite residue quality. This study revealed that BRDAs ecosystem development reaches homeostasis gradually, whilst CNP and MBCNP substrate ratio can be used as an effective tool to explore the mechanism of nutrient cycling.     

Distribution,Accumulation, and Cycling of Several Mineral Elements of the Lower Subtropical Evergreen Broad-Leaved Forest in Heishiding Nature Reserve

The distribution, accumulation, and cycling of N, P, K, Na, Ca, and Mg in terms of their concentration in the biomass was quite different from those in soil in Heishiding Nature Reserve (111°53′ E, 23°27′ N). The concentrations of N, Ca and P were higher in plant, and much lower in soil. The average content of the elements in different organs was in the order as: leaf>branch>bark>root>wood, although this was not true for all the elements. Trunk and leaf had the most and the least accumulation of the elements, respectively, and branch and root were comparable. In the forest, most of the elements (97 %) were concen- trated in the tree layer. The total amount of elements in the ecosystem was 3324.2 kg· ha-1 among which N amounted 1470.5, P 51.0, K 1097.7, Na 22.6, Ca 566.2, and Mg 116.2. Yearly absorption of the elements was 432.2 kg · ha-1 among which N amounted 207.1, P 6.5, K 144.9, Na 6.9, Ca 52.6, and Mg 14. 1; and element absorption among different organs accounted as 35.0 kg · ha-1 · a-1 in wood, 14.8, in bark, 66.1 in branch, 143.2 in leaf, 25.3 in root, and 147.7 in fine root (D<3 mm). Total return of the elements from litterfall, death and fallen trees was 311.8 kg · ha-1 · a-1, among which N accounted for 154.3, P 4.7, K 102.1, Na 6.2, Ca 34.5, and Mg 10.0. Return from different organs was: wood 10.2, bark 4.3, branch 17.0, leaf 123.0, root (not in- cluding fine root) 9.4, and fine root 147.7. Total retention was 120.4 kg · ha-1 · a-1 among which N accounted for 52.8, P 1.8, K 42.8, Na 0. 7, Ca 18. 1, and Mg 4.1; retention in different organs was: wood 24.8, bark 10.5, branch 49.1, leaf 20. 2, and root 15.9. Ca, Mg and P have higher cycling and utilization efficiencies.     

一个农牧结合生态系统营养循环的源,库,流

一个农牧结合生态系统营养循环的源、库、流曾江海,张玉铭（中国科学院石家庄农业现代化研究所０５００２１）Ｓｏｕｒｃｅ,ＰｏｏｌａｎｄＦｌｕｘｏｆＮｕｔｒｉｅｎｔＣｙｃｌｉｎｇｉｎａＣｏｍｂｉｎｅｄＡｇｒｏ－ＡｎｉｍａｌＨｕｓｂａｎｄｒｙＥｃｏｓｙｓｔｅ...     

氮磷共限制青藏高原高寒草甸生态系统碳吸收

随着人类活动加剧,青藏高原高寒草地面临外来资源输入的威胁,而外源资源输入如氮、磷、钾(N、P、K)及其交互作用如何影响高寒草地生态系统碳循环尚不明确.本研究在藏北高寒草甸进行了连续3年N、P、K元素交互的添加试验,测定群落盖度和生态系统碳交换等数据,旨在阐明资源添加对高寒草甸生态系统碳交换过程的影响.结果 表明:在植物...