森林转换对地表径流可溶性有机碳输出浓度和通量的影响

米槠次生林转换成米槠人工幼林和米槠人工促进天然更新幼林(以下简称"人促幼林")后,以这三种森林类型为研究对象,连续监测每次降雨后地表径流量及径流水中可溶性有机碳(DOC)的含量及通量,比较不同森林类型观测结果的差异,并分析降雨对实验结果的影响。结果表明:米槠人工幼林单次产流量是米槠次生林的1.5—19.0倍,观测期间总径流量为5.9倍;米槠人促幼林单次径流量和总径流量均与米槠次生林无显著差异(P0.05)。观测期间米槠次生林、人工幼林、人促幼林径流水DOC浓度值范围为5.9—18.4 mg/L,4.3—13.5 mg/L和3.2—9.9 mg/L,米槠次生林径流水浓度均值(12.6 mg/L)分别是米槠人促幼林(7.6 mg/L)和米槠人工幼林(5.3 mg/L)的1.6和2.4倍。回归分析表明,径流水中DOC浓度与降雨前土壤含水率呈显著相关;降雨前土壤含水率20.8%是一个临界值,含水率低于20.8%时,径流水DOC浓度与降雨前含水率呈显著正相关(P0.05);高于20.8%时,径流水DOC浓度与降雨前土壤含水率呈显著负相关(P0.05)。米槠人工幼林地表径流DOC输出通量是米槠次生林的0.7—5.4倍,观测期间总输出通量为2.1倍;米槠人促林DOC单次通量和观测期间总通量均与米槠次生林差异不显著(P0.05)。三种森林类型DOC输出通量均与降雨量呈显著相关(P0.05)。可见,米槠次生林转变成米槠人工幼林后DOC输出浓度降低,但径流量显著增加,导致DOC输出通量增加;而转变成米槠人促幼林后DOC输出浓度也降低,但径流量并未增加,因而并未增加DOC输出通量。     

鼎湖山针阔叶混交林水文学过程中总有机碳动态

2002年7月～2003年7月对鼎湖山针阔叶混交林生态系统水文学过程中总有机碳(TOC)总量和浓度进行了初步研究.结果表明,观测期间,林外大气降水输入的TOC总量为41.80kg·hm^-2·yr^-1,地表径流和地下水(50 cm土壤渗透水)输出分别为17.54和1.80kg·hm^-2·yr^-1,输入输出之差为22.4kg·hm^-2·yr^-1,系统TOC为正平衡.各类型水中TOC总量月动态基本上与大气降水月动态变化趋势一致.大气降水的TOC平均浓度为3.4 mg·L^-1.经过森林林冠淋洗和树干淋溶后,穿透雨和树干流中TOC的平均浓度分别比大气降水中TOC浓度增加了.10倍和7.39倍.地表径流、25 cm和50 cm土壤渗透水中TOC平均浓度分别为12.72、7.905和3.0 mg·L^-1.穿透雨和树干流中TOC浓度的月变化相似,生长季初(3月),TOC浓度开始增加,9月后逐渐下降,12月又有所回升.降水量较大的月份地表径流中TOC浓度较高.25 cm和50 cm土壤渗透水中TOC浓度无明显的月变化规律.不同树种树干流中TOC浓度差异很大.大气降水、穿透雨、25 cm和50 cm土壤水中TOC浓度随降水量的增加而规律性递减,树干流和地表径流中TOC浓度与大气降水量之间无明显相关关系;除树干流和土壤水外,水文过程各分量水中TOC浓度随着大气降水强度的变化呈现规律性波动.     

控释氮肥对洞庭湖区双季稻田表面水氮素动态及其径流损失的影响

用渗漏池模拟洞庭湖区2种主要稻田土壤(河沙泥和紫潮泥),研究了施用尿素(CF)和控释氮肥(CRNF)对双季稻田表面水pH、电导率(EC)、全氮（TN）、铵态氮（NH₄⁺-N）和硝态氮（NO₃^--N）浓度变化规律及TN径流损失的影响.结果表明,双季稻田施用尿素后,表面水TN、NH₄⁺-N浓度分别在第1、3天达到高峰,然后迅速下降;NO₃^--N浓度普遍很低;早稻表面水pH在施用尿素后15 d内(晚稻3 d)逐渐升高;EC与NH₄⁺动态变化一致.与尿素相比,施用CRNF能显著降低双季稻田表面水pH、EC、TN和NH₄⁺-N浓度,70% N控释氮肥的控制效果最显著;但后期NO₃^--N浓度略有升高.径流监测结果表明,洞庭湖区种植双季稻期间施用尿素的TN径流损失为7.70 kg·hm^-2,占施氮量的2.57%;施肥后20 d内发生的径流事件对双季稻田TN径流损失的贡献极为显著;与施用尿素相比,施用控释氮肥显著降低了施肥后10 d内发生的第1次径流液中的TN浓度,施用CRNF和70%N CRNF的氮素径流损失分别降低24.5%和27.2%.     

Heavy metal leaching from mine tailings as affected by organic amendments

A column experiment was conducted to investigate Zn, Cd, and Pb leaching from mine tailings as affected by the addition of organic amendments. Composted yard waste, composted cattle manure, and cattle manure aged for one month increased heavy metal leaching from mine tailings when compared to an unamended control. Aged cattle manure and composted cattle manure significantly increased Zn concentration in the leachate. The maximum Zn concentration in leachate from the manure-amended treatments was as high as 3.7 mg/L, whereas Zn concentrations from the control were less than 0.7 mg/L. All organic amendments increased Cd leachate concentrations. The presence of aged cattle manure greatly increased Pb concentrations in the leachate from less than 10 microg/L for the control treatment to higher than 60 microg/L. Lead concentration in leachate was positively correlated with inorganic carbon, total organic carbon, total carbon and bicarbonate. Although organic amendments increased Zn, Cd, and Pb leaching when compared with the control treatment, Zn concentrations were lower than the 5 mg/L secondary drinking water standard, and Pb concentrations were only minimally higher than the 15 microg/L drinking water standard. Cadmium concentrations from manure treatments exceeded the 5 microg/L drinking water standard but only during the first 15 days. Organic amendments may encourage establishment of vegetation in mining areas that may minimize heavy metal contamination through runoff and erosion. However, increased risk due to heavy metal leaching in the presence of organic amendments should be carefully considered.     

Accumulation of weathered pp'-DDE in xylem sap of grafted watermelon

Movement of weathered p,p'-dichlorodiphenyldichloroethane (p,p'-DDE) from contaminated soil to the rhizosphere pore water to the xylem sap of grafted watermelon was studied under green house conditions. p,p'-DDE concentrations in pore water and xylem sap was compared in intact plants, homografted, and compatible heterografts of Cucurbita pepo spp. pepo and Citrullus lanatus plants. An average p,p'-DDE concentrations in pore water of contaminated soil ranged from 0.36 microg/L to 0.55 microg/L and there were no statistically significant among the cultivars. Conversely, the xylem sap p,p'-DDE concentration of heterografted watermelon having a zucchini rootstock and watermelon scion was 71 microg/L and it was greater than intact watermelon plants (0.49 microg/L) but less than that of intact plants of zucchini (141 microg/L). Homografting showed no effect on xylem sap p,p'-DDE concentrations of the identical cultivars. The bio-concentration factors (BCFs) which is an average p,p'-DDE concentration in xylem sap over average p,p'-DDE in pore water were 344, 325, 197, 1.28, and 0.89 for intact plant of zucchini, homografted zucchini, heterografted watermelon, homografted watermelon, and intact plant of watermelon, respectively. Xylem sap p,p'-DDE concentrations of the heterografted watermelon plants were clearly influenced by plant phylogeny and enhanced by the zucchini rootstock compared to intact watermelon plants.     

老爷岭多年冻土小流域春季冻融期径流溶解性有机碳变化特征

溶解性有机碳（DOC）的输移过程是流域碳循环中重要的组成部分,对全球碳循环产生重要影响。以大兴安岭多年冻土区的典型森林小流域-老爷岭流域为研究对象,获得2021年4月9日到6月30日冻融期降雨量、气温、土温等气象数据及逐日径流量、径流DOC浓度,计算了冻融循环期（4月9日-28日）和融化期（4月29日-6月30日）流域径流DOC的输出通量,揭示了径流DOC浓度及输出通量的影响因素。结果表明：（1）研究时段内,老爷岭流域径流DOC浓度变化范围为3.88-33.75 mg/L,流域上游的径流DOC浓度变化趋势与下游基本一致,DOC浓度随着温度的升高呈现下降趋势,4月份平均径流DOC浓度明显高于5、6月份。（2）研究时段内流域径流DOC总输出通量为3215.48 kg/km²,其中5月径流DOC输出通量高于4、6月份。径流量与径流DOC输出通量存在显著正相关关系（P<0.05）,是流域DOC输出通量的主导因素。（3）研究时段内流域DOC浓度与平均气温呈极显著负相关（R²=0.5048,P<0.001）;降水样品中的DOC浓度变化范围为1.06-9.42 mg/L,显著低于径流DOC浓度;土壤中DOC含量变化趋势与径流DOC变化趋势一致,0-10 cm、10-20 cm土壤平均DOC浓度范围为77.57-133.99 mg/L。（4）冻融循环期平均日径流DOC浓度（24.02 mg/L）显著（P<0.05）高于融化期（14.64 mg/L）,而融化期平均日DOC输出通量（48.02 kg/km²）是冻融循环期（9.52 kg/km²）的5倍。研究结果揭示了大兴安岭多年冻土小流域春季冻融期径流DOC的输移特征及其影响因素,对理解多年冻土区碳循环有重要意义。     

大气二氧化碳浓度变化对禾谷缢管蚜种群动态的影响

利用开顶式熏气室研究了大气CO₂浓度和土壤水分对禾谷缢管蚜Rhopalosiphum padi (L.)种群动态的影响,并分析了禾谷缢管蚜密度与被处理小麦叶片化学成分的关系。结果表明：（1）禾谷缢管蚜种群密度随CO₂浓度升高而持续增大并与土壤水分密切相关,各CO₂浓度下均以60%田间持水量时的密度最大;（2）CO₂和土壤水分对小麦叶片化学成分有明显的影响,麦叶水分、可溶性蛋白质、可溶性糖、淀粉含量随CO₂浓度和土壤水分含量上升而增加,纤维素含量随CO₂浓度上升而增加、随土壤水分含量上升而降低,单宁、丁布（DIMBOA）含量在CO₂浓度为550 μl/L时最高,但单宁含量随土壤水分上升而增加,丁布含量在60%田间持水量时最低;（3）禾谷缢管蚜密度与叶片水分、可溶性蛋白质、可溶性糖、淀粉含量呈正相关,与丁布、单宁含量呈负相关。结论：在未来的气候条件下,随着CO₂浓度升高禾谷缢管蚜种群可能会持续增长,这种增长在半干旱区更加突出。禾谷缢管蚜种群增长的原因之一是大气CO₂和土壤水分条件改变了植物的化学成分构成。     

Effect of growing Sesamum indicum L. on enhanced dissipation of lindane (1, 2, 3, 4, 5, 6-hexachlorocyclohexane) from soil

The effect of growing Sesamum indicum L. on the dissipation of lindane (gamma-HCH) was studied in spiked soil. For this, S. indicum was grown with four different concentrations of lindane (5, 10, 15, and 20 microg g(-1)). Plant growth, yield, photosynthetic pigments, soluble protein, microbial biomass carbon, lindane uptake, residual lindane concentration in soil and percentage dissipation of lindane from soil were analyzed at 25, 90, and 124 d. The accumulation of lindane in test plants was linearly related to the soil concentration (r2 = 0.897-0.979). At maturity, the accumulation of lindane in S. indicum grown with four spiked concentrations reached up to 7.98, 13.72, 23.71, and 33.29 microg g(-1) dry matter, respectively. There was a marked difference in the dissipation of lindane in vegetated and non-vegetated soils (p < 0.01). After final harvesting, the residual lindane concentrations in four spiked concentrations were reduced by 77.56, 70.12, 62.51, and 58.7%, respectively. Agronomic practice for the onsite application of this species is discussed. Based on the present study, it was calculated that S. indicum could accumulate 2237-2611 mg lindane per acre after 124 d cultivation. S. indicum could thus be used for the phytoremediation of lindane contaminated soil.     

模拟降雨下喀斯特坡耕地土壤养分输出机制

喀斯特区坡耕地水土及养分流失不仅是该区土地质量退化、土地生产力衰退主要原因,同时也是该区地下水质污染的重要因素。为揭示喀斯特坡耕地地表和地下二元空间结构下的土壤养分流失机制,以喀斯特坡耕地为研究对象,通过模拟其地表微地貌及地下孔(裂)隙构造特征,采用人工模拟降雨试验研究不同雨强下喀斯特坡耕地地表及地下水土及其氮、磷、钾流失特征。结果表明:(1)小雨强(50mm/h)和中雨强下(70mm/h),喀斯特坡耕地坡面产流主要以地下产流为主;大雨强下(90mm/h),地表径流高于地下径流;产沙方式则表现为由小雨的地表和地下产沙并重到中大雨强的地表产沙为主的一个转变过程。(2)在降雨侵蚀过程中,径流各养分输出浓度均表现出一定的初期冲刷效应,受土壤吸附作用影响,雨强对全钾(TK)和全氮(TN)的影响较全磷(TP)明显。(3)地表径流、地表泥沙和总泥沙各养分输出负荷均随雨强增大而增加,坡面径流泥沙总的TK输出负荷以泥沙为主,而TN和TP输出负荷则以径流为主;TP和TN在径流的输出负荷上以地下径流输出为主(其中TP地表负荷比在11.6%—46.2%,TN在7.0%—48.5%之间),而TK则以二者并重(地表负荷比在43.5%—57.0%之间);各养分在泥沙的输出负荷上则均以地表泥沙流失为主,其负荷比均在54.5%以上。研究结果可为喀斯特区坡耕地水土流失及养分流失的源头控制提供基本参数和科学依据。     

大气二氧化碳浓度变化对禾谷缢管蚜种群动态的影响

利用开顶式熏气室研究了大气CO₂浓度和土壤水分对禾谷缢管蚜Rhopalosiphum padi (L.)种群动态的影响,并分析了禾谷缢管蚜密度与被处理小麦叶片化学成分的关系。结果表明：（1）禾谷缢管蚜种群密度随CO₂浓度升高而持续增大并与土壤水分密切相关,各CO₂浓度下均以60%田间持水量时的密度最大;（2）CO₂和土壤水分对小麦叶片化学成分有明显的影响,麦叶水分、可溶性蛋白质、可溶性糖、淀粉含量随CO₂浓度和土壤水分含量上升而增加,纤维素含量随CO₂浓度上升而增加、随土壤水分含量上升而降低,单宁、丁布（DIMBOA）含量在CO₂浓度为550 μl/L时最高,但单宁含量随土壤水分上升而增加,丁布含量在60%田间持水量时最低;（3）禾谷缢管蚜密度与叶片水分、可溶性蛋白质、可溶性糖、淀粉含量呈正相关,与丁布、单宁含量呈负相关。结论：在未来的气候条件下,随着CO₂浓度升高禾谷缢管蚜种群可能会持续增长,这种增长在半干旱区更加突出。禾谷缢管蚜种群增长的原因之一是大气CO₂和土壤水分条件改变了植物的化学成分构成。     

施磷对稻田土壤及田面水磷浓度影响的模拟

通过施用不同剂量磷肥稻田土壤淹水培养试验,研究了施磷对稻田土壤及田面水磷浓度的影响.结果表明,土壤速效磷（Olsen-P）浓度在施磷后迅速下降,60 d后趋于稳定.随施磷量的增加,土壤速效磷和缓效磷库量均递增,Olsen-P与施磷量呈正相关关系(y=21.49+0.086x),表明该土壤有很高的固磷潜力.施磷后田面水中全磷浓度呈先迅速上升后又缓慢下降趋势,施磷120 d后,田面水中全磷浓度与施磷量呈指数相关关系(y=0.3 72e^0.0022x),施磷量在400～800 kg·hm^-2之间田面水全磷浓度加速增长,如果施磷量达到或超过800 kg·hm^-2,则磷容易进入田面水并导致流失,低于该施磷量时,则磷进入田面水中的量较少.利用分段回归模型模拟土壤Olsen-P与水面全磷关系,预测出导致田面水中磷激增的土壤Olsen-P浓度“突变点”为82.7 mg·kg^-1,即施磷量为712 kg·hm^-2.因此,土壤Olsen-P浓度可作为预测田面水中磷损失程度的指标.     

鼎湖山季风常绿阔叶林水相沉积元素分布及其相关性研究

2001年2月~ 2002年3月在鼎湖山季风常绿阔叶林对大气降水、穿透水、土壤水 (30和 80cm层 ) 和溪水中的沉积元素进行监测, 拟通过不同水相元素浓度的比较及相关关系分析, 揭示系统的营养循环功能状况以及对区域化学条件变化的响应, 阐明因素在环境中的迁移转化规律。结果表明 :林冠与大气间强烈的相互作用, 极大地提高穿透水中Mn2 + 、Sr2 + 、K+ 、Mg2 + 、Ca2 + 浓度。水与土壤作用后, 极大地提高水相中Al3 + 的浓度。 30cm土壤溶液和溪水中的Al3 + 浓度分别是大气降水 (0.32 9mg·L-1) 的 4.8和 3.7倍。溪水中的Al3 + 主要来源于土壤的淋溶。大气降水平均Pb2 + 浓度为 0.0 6 2mg·L-1, 存在着一定程度的Pb2 + 污染, 其浓度分别是穿透水和溪水的 5倍和 10倍。林冠吸收和土壤过滤吸附是森林生态系统净化Pb2 + 等重金属污染物的主要过程。大气降水、穿透水、土壤水和溪水中Na+的浓度逐步增加, 但增幅不大。元素浓度的变异系数在 5 1.1%~ 2 36.7%之间。水相中的离子浓度与雨量有关, 大气降水、穿透水、土壤水中的沉积元素浓度大部分是干季大于湿季, 而溪水中是干季小于或近等于湿季。元素相关分析发现, 与元素Mg相关的元素最多, 穿透水所含相关元素对最多, 不同水相间元素相关状况差异与其元素的来源和外部环境条件有关系。Pb与金属元素Al、Mn在大气降水中极显著相关, Mn_Al、Mn_Mg、Mg_K在所有水相中显著相关, Al_Sr、Mn_Sr、Ca_K、Ca_Mg在除溪水外的所有水相中显著相关, Na_K、Na_Mg在除大气降水外的所有水相中显著相关, 而Pb_Na、Pb_K在所有水相中都无相关关系。结果说明, 季风常绿阔叶林系统已经遭受一定的外界环境压力, 但是其物质循环功能依然稳定。     

Review of distribution of nitrogen and phosphorus in riparian zones of Chinese inland water bodies

This review tries to explain the effects of river infiltration and the interaction between groundwater and surface water on nitrogen (N) and phosphorus (P) distribution in riparian zones. On the basis of previous studies, this review summarized the distribution characteristics of N and P of 7 different riparian zones in China, compared the water quality of water bodies adjoining these riparian zones, proposed the distribution regularity of N and P in diverse riparian zones. The concentrations of N and P in the riparian zones with better water quality have increasing trend from riverside to upland. And those rivers with poorer water quality have decreasing trend. If the infiltrated concentration of runoff pollutant is more than river pollutant infiltration, the upland soil may obtain higher contaminants. On the contrary, if the concentration of river infiltration is more than that of the runoff, the riverside soil will show higher concentration. Similarly, if those two effects are equivalent, the concentration of N and P in the riparian zone will be low on riverside and upland, and somewhere in the middle will be higher than elsewhere. Clean rivers and polluted rivers taken with different quantity of contaminants will infiltrate diverse concentrations of N and P. It is expected that this review can provide a new theoretical basis for revealing the environmental effects of riparian zones and managing, protecting and restoring the riparian ecosystems.     

Serum manganese concentrations in a representative sample of the Canarian population

Serum manganese (Mn) concentrations of 368 individuals 6–75 yr of age (179 males and 189 females) living in the Canary Islands were determined by graphite furnace atomic absorption spectrometry. The mean manganese concentration was 1.06 ± 0.62 μg/L, ranging between 0.19 and 3.33 μg/L. Most of the analyzed samples (63.3% of the samples) fall within the reference interval (0.54–1.76 μg/L) for apparently healthy people. Individuals from Fuerteventura presented with mean Mn concentrations significantly higher than individuals from the rest of the islands. This could be attributed to differences in the Mn content of soil and/or differences in dietary habits of the population. Serum Mn concentration did not vary with gender, and individuals younger than 18 yr old had the highest mean Mn concentration, compared to the rest of the age groups considered. No relation to socioeconomic status, educational level, and tobacco or alcohol consumption was found. However, the serum Mn concentration tended to decrease when increasing the consumption of wine or beer. Sportsmen presented significantly higher serum Mn concentrations than the rest.     

三峡库区土质道路侵蚀产沙过程的模拟降雨试验

以三峡库区王家桥小流域为研究区,通过野外调查选择了5个典型路段,在1.0 mm min~(-1)模拟降雨条件下研究了土质道路降雨-径流-泥沙关系.结果表明,土质道路被高度压实,但使用强度和管护方式差异致使容重、路面浮土、杂草盖度、饱和导水率等差异显著.土质道路仅需1～3 mm降雨就能产生地表径流,7～10 mm的降雨使径流趋于稳定,径流系数超过60%,特别是车流量较大干道的径流系数超过70%,平均和峰值径流量达0.69 mm min~(-1)和0.84 mm min~(-1).土质路面大量浮土致使初始径流含沙量高,然后快速下降并趋于稳定.由于路面浮土量大和在降雨过程中能形成人工细沟的车辙等导致较大车流量干道的土壤流失率是其它路段3～4倍.土质道路的容重和路面浮土与径流系数和土壤流失量呈显著正相关,饱和导水率则呈显著负相关;路面杂草能显著减少径流,防治路面侵蚀.     

亚热带森林林分更新对地表径流4种盐基离子浓度的影响

地表径流不仅是水循环的重要组成部分,也是森林物质迁移的重要途径,其动态过程可能受林分更新的调控,目前仍缺乏必要的关注.通过对福建省三明市米槠(Castanpsis carlesii)次生林、杉木(Cunning-hamia lanceolata)人工林、杉木人工幼林和米槠人工幼林近5年的定位观测,探讨林分更新对地表径流...     

Effect of slope farmland soil and water and soil nitrogen and phosphorus loss based on different crop and straw applications and ridge patterns in the basin of the main stream of the Songhua River

For soil and water erosion control in slope farmland, field experiments consisting of corn?+?no straw application?+?longitudinal ridge (CNL-CK), corn?+?stubble standing?+?cross ridge (CSSC), corn?+?straw application?+?cross ridge (CSC), soybean?+?straw application?+?cross ridge (SSC) and alfalfa?+?straw application?+?cross ridge (ASC) were conducted. Compared with the traditional CNL cropping pattern, soil loss in CSSC, CSC, SSC, and ASC was decreased 43.6%, 48.6%,58.2% and 62.1%, respectively, soil nitrogen loss load was decreased 53.8%, 50.8%, 62.1% and 66.2%, respectively, and soil phosphorus loss load was decreased 50.7%, 50.7%, 60.0%, and 66.7%, respectively. Runoff volume was decreased 42.4%, 52.3%, 54.6% and 61.0%, runoff nitrogen loss load was decreased 52.8%, 56.8%, 46.1% and 50.2%, respectively, and runoff phosphorus loss load was decreased 46.9%, 78.2%, 67.2%, and 62.7%, respectively. Soil and water erosion control of soybean and alfalfa were better than that of corn. Soil loss was decreased 19.2% and 26.7%, soil nitrogen loss load was decreased 22.9% and 31.3% respectively, soil phosphorus loss load was decreased 18.9% and 32.4% respectively, runoff volume was decreased 4.8% and 18.4% respectively, runoff nitrogen loss load was decreased ?24.9% and ?15.3% respectively, and runoff phosphorus loss load was decreased ?50.4% and ?71.2% respectively. Though runoff volume of SSC and ASC were lower than CSC, the concentration of nitrogen and phosphorus in SSC and ASC runoff liquid were higher than CSC, so the runoff nitrogen and phosphorus of SSC and ASC were increased. The runoff nitrogen and phosphorus loss load could be negligible because the soil nitrogen and phosphorus loss load were large. The concentration of nitrogen and phosphorus of all treatment runoff liquid was less than the environmental quality standards for class III surface water, so the runoff from slope farmland did not influence the water quality of the Songhua River.     

浙江赋石水库集水区板栗林土壤氮素迁移特征

本研究通过在板栗林地设置径流小区,于2013年1—10月间采集径流水样进行测试,同时结合雨季前后土壤氮素数据,分析了浙江北部赋石水库集水区板栗林土壤氮素迁移特征.结果表明: 板栗林地的10次地表径流事件中,各径流小区径流水量差别较大,最大达0.51 m³;其中氮是主要的流失元素,硝态氮(NO₃^--N)、铵态氮(NH₄⁺-N)、总氮(TN)和化学需氧量(COD_Mn)的浓度分别为0.02～1.87、0.04～3.53、1.69～5.33和5.30～14.07 mg·L^-1,各水质指标受径流水量影响较大,且用一元一次方程可以较好地拟合氮素流失量与径流水量之间的相关关系;雨季前后板栗林地径流场上部、中部和下部3个位置的土壤中,氮素含量差异较大;总的变化趋势是随着海拔升高氮素含量增加,随着土层深度加深氮素含量降低.比较雨季前后4种土壤氮素(NO₃^--N、NH₄⁺-N、TN 和水解性氮Hydro-N)的差异发现,差异较大的为Hydro-N和TN,平均差异值为20.21和307.49 mg·kg^-1.该区氮素随径流流失风险较大,对赋石水库水体富营养化构成潜在压力,需重点关注.     

刺参养殖池塘颗粒悬浮物结构及其沉积作用

对不投饵刺参养殖池塘的颗粒悬浮物结构及其沉积量和沉积速度进行了研究.结果表明:(1)各池塘总颗粒悬浮物重量(TS)为(73.1±20.5)mg/L,变动于46.0～132.0mg/L之间;颗粒无机物(IS)含量为(50.6±12.6)mg/L,变动于28.5～76.5mg/L之间,占总颗粒悬浮物的69.13%;浮游生物干重(PZ)为(0.675±0.706)mg/L,变动于0.064～2.814mg/L之间,其中浮游植物干重(DWP)为(0.541±0.622)mg/L,变动于0.062～2.582mg/L之间,浮游动物干重(DWZ) 为(0.135±0.200)mg/L,变动于0.002～1.160mg/L之间;颗粒腐质为(21.91±19.59)mg/L,变动于4.18～83.86mg/L之间,占总颗粒悬浮物的比例为29.95%.(2)总颗粒物沉积量为(19.44±16.34)g·m-2·d-1,变动于6.33～91.98g·m-2·d-1之间,沉降速度为(0.30±0.30)m·d-1,变动于0.08～1.63m·d-1之间,新生态颗粒有机物沉积量为(5.09±7.30)g·m-2·d-1,变化于0.14～31.27g·m-2·d-1之间,总颗粒物沉积量和新生态颗粒物沉积量均是底层高于表层.     

Resorption of nitrogen,phosphorus and potassium from leaves of lucerne stands of different ages

Background and aims

Nutrient resorption from the senesced to the green leaves can help a plant re-use elements, thus improving adaptability and persistence. How the resorption of nitrogen (N), phosphorus (P) and potassium (K) varies among differently aged lucerne (Medicago sativa) stands and how they correlate to their stoichiometry in the leaves and soil remain uncertain. This study aimed to analyze the resorption efficiencies (REs) of N, P and K and their possible correlations with stoichiometric ratios in the plant and soil.

Methods

The concentrations of plant N, P and K and soil N, P, K and carbon (C) were measured under lucerne stands established in different years, and stoichiometric ratios and REs were calculated. The relationships of REs with stoichiometric ratios were analyzed.

Results

The nitrogen resorption efficiency (NRE) was quite variable among the different stands and tended to rise and then drop with stand age, ranging from 4.6 to 33.7 % with an average of 16.2 %. The phosphorus resorption efficiency (PRE) tended to increase with stand age, ranging from 11.1 to 38.3 % with an average of 27.3 %. The potassium resorption efficiency (KRE) increased with stand age, ranging from 21.0 to 49.8 % with an average of 36.9 %. The KRE was generally highest, followed by the PRE, and the NRE was lowest. Leaf N:P and N:K generally decreased and then increased with stand age, while the K:P increased and then decreased. In the green leaves, total N concentration increased significantly with NRE and PRE, and total P concentration rose significantly with PRE, while in the senesced leaves, total N concentration decreased significantly with NRE and KRE. The N:P in the green leaves decreased significantly with PRE and the K:P in the senesced leaves dropped with NRE. Furthermore, the REs decreased with total soil nutrition status if there was any correlation. The REs increased significantly with soil ammonium N concentration, while the NRE decreased significantly with soil nitrate N concentration. In addition, soil available P concentration at most depths led to significant increases in NRE and KRE. However, the REs were rarely influenced by stoichiometric ratios of soil N, P, K and C.

Conclusions

The NRE rose and then dropped, and the PRE and KRE both increased with stand age. Leaf N:P and N:K generally decreased and then increased with stand age, while K:P increased and then decreased. The concentrations of N, P and K increased in the green leaves and decreased in the senesced leaves with REs if there was any correlation. The REs decreased with total soil nutrition status if there was any correlation. However, the REs hardly changed with stoichiometric ratios in the leaves and soil under differently aged lucerne stands. There appear to be no correlations between REs and element stoichiometries.