凉水和帽儿山地区低级溪流生境和水质状况

为研究不同植被景观土地利用下低级溪流的生境状况和水质差异,对凉水国家级自然保护区红松原始林内和帽儿山国家森林公园境内天然次生林植被和农田背景下各3条溪流生境和水质状况进行调查。对溪流生物特性（悬浮藻、附着藻）和理化性质（温度、混浊度、溶解氧（DO）、pH、NH4^＋-N、NO3^-N、PO4^3-P、总氮（TN）和总磷（11P））以及细小颗粒有机物质（FPOM）和粗大有机物质（CPOM））进行测定。研究结果表明,凉水地区原始林溪流的生境状况好于帽儿山地区的次生林,帽儿山地区农田溪流生境最差。原始林溪流具有稳定的溪底生物生活基质,稳水区和急流区均匀分布,稳水区尺度变化大,受淀积物沉降干扰小,河道较弯曲,河岸稳定,河岸植被覆盖度高;次生林溪流以急流区为主,稳定基质相对较差,并受到一定程度的淀积物沉降干扰,河岸尚稳定,有一定程度的人为干扰;农田溪流基质不稳定,受到强烈淀积物沉降影响,渠道化严重,河岸带植被严重破坏。3种景观背景下溪流总磷（11P）、溶解氧（DO）、混浊度、温度、氮磷比值（N／P）（P〈0．05）存在显著差异。原始林溪流NH4^＋、DO、TP、TN、悬浮藻浓度和pH较高、附着藻数量较多,温度较低、FPOM和CPOM的数量较少;次生林溪流的NO3^--N、N／P和TDIN较高。 浊度较低;农田溪流浊度、温度、PO4^3--P较高,DO和pH较低,附着藻数量较少。景观尺度上的土地利用对溪流生境具有深刻的影响,同时决定溪流的水质状况。     

五川源头溪流系统氮的迁移和转化

利用氮稳定同位素法、综合常规水样监测以及微环境培养方法探讨了五川农业溪流沿程氮的迁移转化过程.结果表明,溪流沿程NO3-N浓度变化范围为0.5～4.5 mg L-1,平均为1.26 mg L-1,且多数月份总体上呈逐渐升高的趋势,同时NO-3的δ15N存在降低趋势,两者呈线性负相关(R2>0.80),表现明显的硝化过程典型特征.各采样点的NO2-N、DO、DOC浓度与NO3-N也存在一定的线性相关关系,说明了硝化过程的发生和氮在不同形态之间的转化.溪流水体微环境培养实验证明了水体中的NH4-N和NO3-N浓度在培养期内并无明显变化,以上数据和相关关系充分表明了流域沿程地表径流氮素输入和溪流系统沉积物和水体界面的硝化过程共同作用可能是五川溪流沿程NO3-N与NH4-N浓度升高,而NO-3的δ15N值减小的主要原因.因此,在农业流域的污染源评价中,需要重新审视和调查河道系统内部氮的转化和贡献.     

溪流大小及其空间位置对鱼类群落结构的影响

2008年10月和2009年10月分别对黄山地区阊江流域与青弋江流域1-3级浅水溪流中鱼类群落结构进行了研究,着重探讨了溪流大小及其空间位置对鱼类群落空间分布的影响。研究共捕获35种鱼类,阊江和青弋江分别为26和29种,其Jaccard相似性系数为57.1%;两流域间每样点的物种数差异显著,个体数差异极显著。在溪流级别梯度(1-3级)下,鱼类的物种数和个体数都呈上升的变动趋势,且物种数的变化相对个体数较显著。综合相关分析、逐步多元回归分析与典范相关分析的结果,阊江和青弋江中鱼类物种数的空间变化主要与下游量级相关,而个体数的空间变化主要与水宽相关。因此,阊江和青弋江1-3级浅水溪流中鱼类群落结构的空间分布格局是溪流大小和空间位置的共同作用结果,且溪流大小和空间位置分别决定鱼类的个体数与物种数的空间分布。       

高寒森林溪流微生物群落结构的季节性变化

高寒森林溪流不仅是区域河流的源头,而且是联系陆地与水域的生态纽带。微生物活动可能成为控制溪流生态系统过程的关键因子,但其结构与动态过程缺乏必要关注。因此,结合同步温度动态监测,采用实时荧光定量PCR和DGGE技术,在2014年到2015年冻融季节和生长季节关键时期对比研究了川西高寒森林溪流和森林林下土壤中微生物群落的动态特征。研究结果发现,高寒森林溪流具有较低的真菌和细菌群落丰度;与森林土壤相同,溪流在冻融季节表现出相对生长季节更高的真菌/细菌比,而且从冻融季节到生长季节,溪流微生物丰度动态也表现出明显的季节性变化特征。与森林土壤不同的是,溪流中细菌和真菌的丰度及其Shannon-Wiener多样性指数的最高值均出现在生长季节而不是冬季冻融季节,并且溪流中细菌丰度在季节性变化的不同时期具有显著差异(P0.05)。此外,森林土壤细菌类群以芽孢杆菌属(Bacillus sp.)比例相对较高,真菌类群则以格孢菌属(Pleosporales sp.)、曲霉属(Aspergillus sp.)和其他一些子囊菌门(Ascomycota)的类群为优势;而溪流细菌类群以红球菌属(Rhodococcus sp.)为主,真菌类群则以曲霉属和空团菌属(Cenococcum sp.)为主。同时,季节性变化中温度、p H、水溶性有机碳和溶解氧等环境因子可显著影响溪流微生物群落结构及其组成,这些环境因子在高寒森林溪流微生物群落的季节性变化过程中具有重要的作用。     

污染物在农田溪流生态系统中的动态变化

氮是地表水体发生富营养化的主要因子,河流系统是氮输出的主要运移通道,养分在河流生态系统中的持留和趋向控制着污染物的输出。以巢湖流域一个受人为活动严重影响的农田源头溪流——六岔河为研究对象(包括4个渠道型、1个水塘型和3个河口型断面,对应长度分别为1．3km、0．15km和0．36km),设置9个监测点研究总氮(TN)、硝酸盐(NO3-N)、氨态氮(NH4^ -N)和总悬浮物(TSS)在溪流生态系统中的持留,评价人为严重干扰下的农田溪流生态系统在非点源污染物运移中的生态功能。结果表明：TN、NO3-N、NH4^ -N和TSS在溪流中的持留、释放受溪流的河流形态影响,水塘型和河口型断面是污染物持留的主要区域;TN、NO3-N、NH4^ -N和TSS在水塘型和河口型断面内的持留量分别占溪流持留量(基流、径流持留量的和)的61％、47％、75％和56％。降雨-径流过程中发生的持留是污染物持留的主要部分,TN、NO3-N、NH4^ -N和TSS的持留量分别占溪流持留量的93％、97％、89％和96％;渠道型断面是溪流最主要的内在污染源,污染物释放量占溪流释放量的90％以上;受水塘型断面出口处的水坝影响,位于水塘前的渠道型断面在基流和降雨-径流过程中均有效地持留污染物,而其余渠道型断面在不同水文条件下呈现出不同的持留特性。非点源污染物在溪流中的持留和释放的空间动态变化是溪流生态系统对自然和人为干扰的一种综合响应,有必要恢复溪流生态系统功能,控制农业非点源污染。     

亚高山森林溪流镉储量与分配的动态变化特征

镉(Cd)是一种有害重金属元素,能够伴随溪流水体流动和物质沉积影响下游流域的生态环境安全,但缺乏必要关注。为了解森林溪流Cd储量及其分配的动态变化特征,以岷江上游亚高山森林集水区的溪流为研究对象,在长度10—50、50—150、150—260m区间内各选取5条典型溪流,研究Cd元素在亚高山森林-溪流-河流集合生态系统中的迁移过程。结果表明:亚高山森林溪流的Cd储量介于2.57—128.46mg/m~2之间,主要储存于沉积物中;森林溪流上、中、下游的Cd储量没有显著差异;森林溪流的Cd储量以秋季凋落物高峰期最高,春季凋落物高峰期最低;森林溪流的上、中、下游Cd储量均在秋季凋落高峰最高,上、中游在春季凋落高峰最低,下游在非凋落高峰最低;凋落物的Cd储量与溪流水文特征密切相关。可见,亚高山森林溪流Cd储量动态具有季节性变化和一定的自净能力,这些结果为进一步了解Cd元素在水-陆生态系统的生物地球化学循环提供了新的角度。     

短期内15N标记的铵盐和硝酸盐在青藏高原高寒草甸中的运移规律

运用15N稳定性同位素示踪技术,对高寒草甸植物和土壤微生物固持沉降氮的能力及沉降氮在小嵩草(Kobresia pygaea)草甸中的运移规律进行了研究.施肥2周后,NO-3-15N和NH+4-15N的总恢复率分别为73.5%和78%.无论是NO-3-15N,还是NH+4-15N,植物所固持的15N总是比土壤有机质或者是土壤微生物固持的多.4周后,70.6%的NO-3-15N和57.4%的NH+4-15N被固持在土壤和植物中.其中,土壤有机质所固持的15N均下降了很多,而植物所固持的15N却变化很小.同前面的结果相比,较多的NO-3-15N为土壤微生物所固持.在施肥6周和8周后,NO-3-15N的总恢复率分别为58.4%和67%,而NH+4-15N的总恢复率分别为43.1%和49%.植物和土壤微生物所固持的NO-3-15N比NH+4-15N多.在整个实验期间,植物固持的NO-3N较多,而且比土壤微生物固持了较多的15N.由于无机氮的含量一直很低,无机氮库所固持的15N一般不超过1%.上述结果意味着短期内植物在高寒草甸中对沉降氮的去向起着决定作用.     

凉水、帽儿山低级溪流中水生昆虫的群落特征及水质生物评价

在东北林业大学凉水国家级自然保护区和帽儿山实验林场,对3种类型低级溪流中水生昆虫进行采集、鉴定,分析水生昆虫群落组成、季节优势集中性和取食功能群,并应用指示生物法、Shannon-Weiner多样性指数、群落相似性系数和BI指数对溪流水质进行生物评价。共采集到水生昆虫4907个,分别隶属于8目38科,其中,毛翅目、蜉蝣目、横翅目和双翅目为四大优势类群,个体数量占水生昆虫总数量的91．13％。原始林溪流中水生昆虫个体数量最多,占总数的58．98％,次生林溪流次之,农田溪流最少。次生林溪流水生昆虫物种多样性要高于原始林和农田溪流,且其各种取食功能群比例较均衡。齿角石蛾科、鳞石蛾科、新蜉科和黑横科昆虫可以作为溪流清洁水质的指示生物。水生昆虫季节优势集中性与Shannon-Weiner多样性指数水质评价结果之间具有相关性,即随溪流水质污染程度的加重,水生昆虫的物种多样性逐渐减少。群落相似性系数的分析表明,原始林溪流和次生林溪流水质对水生昆虫的群落组成没有影响,农田溪流则产生中等影响。生物指数（BI）评价结果显示除了农田溪流10月的水质为轻污染外,其余时间3种溪流的水质都能达到清洁标准以上。     

长白山二道白河森林流域溪流倒木调查研究

溪流倒木是森林生态系统对水生态系统最重要、最直观的输入和干扰之一,也是两系统之间的主要联结,对于溪流生态系统的稳定、水生生物多样性、河槽形态及其变化过程有着重要的作用。重点对长白山北坡溪流倒木现存量进行了调查和研究,在调查的红松阔叶林植被带内４５００ｍ长河道内,共发现溪流倒木４２５株．分属于１７个树种;其中ｌ、ｗ级腐烂占相当大的比重,与林地倒木Ｉ、ｌ级腐烂占忧有所不同,其原因可能与分解环境的不同有关。所有溪流倒木的总材积为７７．９８ｍ＾２,故溪流倒木的现存量为１．７３３ｍ＾３／１００ｍ和１０．８３ｍ＾３／ｈｍ＾２。溪流倒木的树种组成和不同树种的材积与河岸带植被密切相关,但存在差异。研究表明林分形成倒木并进入河流在时间上可能是均匀或随机的,但不同树种间,其形成倒木并进入河流时的树木材积或生长年龄存在较大差异。溪流倒木和林地活立木的个体数量的径级分布基本上为反Ｊ型,而它们材积的径级分布均为典型的Ｊ型。     

不同种植模式的茶园对溪流大型底栖无脊椎动物群落的影响

茶园对溪流水质和底栖动物群落的影响正日益受到关注。于2007年4月调查了浙江富阳、建德、武义和松阳县,受不同种植模式茶园（低山林地改植茶园、高山林地改植茶园和农田改植茶园）影响的溪流及无干扰参照溪流共17个样点的水质和大型底栖无脊椎动物。结果表明：受茶园影响溪流的铵态氮、总氮、总磷、COD_Mn和电导率都高于参照溪流,低山茶园影响溪流的总氮5.506 mg·L^-1和总磷0.053 mg·L^-1比高山茶园影响溪流的总氮2.069 mg·L^-1和总磷0.028 mg·L^-1高出约2倍;低山林地改植茶园影响溪流的底栖动物物种丰富度显著低于参照溪流(P<0.01),高山林地改植茶园影响溪流与参照溪流之间的差异不显著（P>0.05）;群落相似性的非度量多维尺度(nMDS)分析表明（stress value=0.09）,参照溪流和高山茶园干扰溪流的物种相似性最高,农田改植茶园与农田影响溪流之间也具有较高物种相似性。     

Nutrient concentration-stream discharge relationships during storm events in a first-order stream

The relationship between nutrient element concentration and stream discharge during storm events was studied in a nutrient-rich first order stream. Stream concentrations of NO₃-N, phosphate-P, Ca, and Mg were determined during the course of and following thunderstorms. Nutrient element trajectories were constructed for the elements monitored and some recognizable and reproducible patterns in nutrient concentrations emerged. NO₃-N and phosphate-P generally increased in concentration during the early stages of increasing stream discharge resulting in a general clockwise trajectory. Ca and Mg consistently showed decreases in concentration during rising water, but the pattern of the trajectories was less constant. The patterns seen for NO₃-N and phosphate-P suggest surface run-off as their origin while the patterns for Ca and Mg reflect their primary origin in groundwater. The ability to detect these differences from the analysis of nutrient trajectories suggests the use of this technique for determining the source of other elements in streams.     

Use of stream order and biological indices to assess water quality in the Osage and Black river basins of Missouri

Significant variations in four biological measures of water quality with stream order and river basin were demonstrated for streams of the Black and Osage river basins of Missouri. Water quality criteria specific for each order and basin were then developed.Benthic macroinvertebrates from springs and stream orders 3–8 in the two river basins were sampled quarterly for one year with riffle nets and artificial substrate samplers. A total of 548 samples were taken at 137 stations. The average annual macroinvertebrate density, index of diversity, number of taxa, and number of mayfly and stonefly taxa were determined for each station. These measures showed significant differences (p < 0.05) across stream order within and between the two river basins. Total taxa, total mayfly and stonefly taxa, and diversity were highest in orders 4 and 5 with decreased values in lower and higher stream orders. Maximum organism densities occurred in intermediate order streams. These differences were attributed to the succession of physical changes from headwaters to mouth within each river and to the unique geomorphology of each catchment basin.Water quality criteria based on three of the four measures described above (with 95% confidence limits) were established for each stream order in each river basin. Criteria for the Osage River basin were then used to identify three streams in the basin affected by environmental disturbances (stream impoundment, channelization and sewage discharge). The use of order- and basin-specific criteria assures that the biological differences between streams caused by environmental disturbance can be distinguished from the natural biological differences between streams of different orders and drainages.     

Anthropogenic disturbance and streams: land use and land‐use change affect stream ecosystems via multiple pathways

1. Ecosystems are strongly influenced by land use practices. However, identifying the mechanisms behind these influences is complicated by the many potential pathways (often indirect) between land use and ecosystems and by the long‐lasting effects of past land use. To support ecosystem restoration and conservation efforts, we need to better understand these indirect and lasting effects. 2. We constructed structural equation models (SEM) to evaluate the direct and indirect effects of contemporary (2002) land use (agriculture and development) and change in land use from 1952 to 2002 on present‐day streams (n = 190) in Maryland, U.S.A. Additional variables examined included site location, system size, altitude, per cent sand in soils, riparian condition, habitat quality, stream water NO₃‐N and benthic macroinvertebrate and fish measures of stream condition. Our first SEM (2002 Land Use) included the proportions of contemporary agriculture and development in catchments in the model. The second SEM (Land Use Change) included five measures of land use change (proportion agricultural in both times, developed in both times, agricultural in 1952 and developed in 2002, forested in 1952 and developed in 2002 and agricultural in 1952 and forested in 2002). 3. The data set fit both SEMs well. The 2002 Land Use model explained 71% of variation in NO₃‐N and 55%, 42% and 38% of variation in riffle quality, macroinvertebrate condition and fish condition, respectively. The Land Use Change model explained similar amounts of variation in NO₃‐N (R² = 0.72), riffle quality (R² = 0.57) and macroinvertebrate condition (R² = 0.44) but slightly more variation in fish condition (R² = 0.43). 4. Both models identified pathways through which landscape variables affect stream responses, including negative direct effects of latitude on macroinvertebrate and fish conditions and positive direct and indirect effects of altitude on NO₃‐N, riffle quality and macroinvertebrate and fish conditions. The 2002 Land Use model showed contemporary development and agriculture had positive total effects on NO₃‐N (both through direct pathways); contemporary development had negative effects on macroinvertebrate condition. The Land Use Change model showed that contemporary developed land that was forested in 1952 had no effects on NO₃‐N; current developed land that was developed or agricultural in 1952 showed positive effects on NO₃‐N. Forests that were agricultural in 1952 had negative effects on NO₃‐N, suggesting reduced NO₃‐N export with reforestation. The Land Use Change model also showed negative total effects of all types of contemporary developed land (developed, agricultural or forested in 1952) on benthic condition. Developed land that was forested in 1952 had negative effects on fish condition. Forest sites that were agricultural in 1952 had negative effects on fish and macroinvertebrate conditions, suggesting a long‐term imprint of abandoned agriculture in stream communities. 5. Our analyses (i) identified multiple indirect effects of contemporary land use on streams, (ii) showed that current land uses with different land use histories can exhibit different effects on streams and (iii) demonstrated an imprint of land use lasting >50 years. Knowledge of these indirect and long‐term effects of land use will help to conserve and restore streams.     

Nitrogen transformations in a small mountain stream

Ammonium, urea, and nitrate were added to Bear Brook, a second and third order stream in the Hubbard Brook Experimental Forest, New Hampshire. Removal of ammonium and urea during downstream transport coincided with the release of nitrate. Nitrate removal did not occur when it was added alone or with dissolved organic carbon. Laboratory experiments showed that coarse particulate organic material (detritus) and bryophytes taken from the streambed were active in the removal of ammonium from enriched stream water, and in the release of nitrate upon the addition of ammonium.The patterns of removal and release observed in these experiments suggest a biologically mediated, oxidation process. Budgetary calculations show that the in-stream transformation of nitrogen inputs during summer and autumn could represent 12 to 25 percent of the nitrogen exported as nitrate during winter and spring from heterotrophic streams like Bear Brook. This type of internal cycling affects the timing and form of nitrogen export from small streams draining forested watersheds in the northeastern United States.     

Meta‐community theory and stream restoration: evidence that spatial position constrains stream invertebrate communities in a mine impacted landscape

Mining activities, particularly acid mine drainage, often result in adverse effects on stream diversity and ecosystem functioning, and increased concern about these effects has generated a focus on restoration of mine‐impacted waterways. However, many stream restoration projects have not led to increased stream diversity and ecological recovery. One reason for this failure may be that restoration practitioners focus on local environmental conditions and fail to consider the importance of dispersal as a driver of stream invertebrate composition. To test this hypothesis, we used a meta‐community analysis to compare the influence of the local stream conditions with the regional supply of colonists. Invertebrate communities and physico‐chemical conditions were sampled in 37 streams across a mine‐impact gradient on the Stockton Plateau, West Coast of New Zealand's South Island. We found that pH, temperature, dissolved metals, and sediment significantly influenced invertebrate community composition. Furthermore, the spatial location of streams was a good predictor of stream diversity and invertebrate communities, independent of local environmental conditions. This result indicates an important role for regional dispersal barriers in determining stream invertebrate communities. Consequently, consideration of both the locations and strategic preservation of future colonist source streams and potential dispersal barriers during mine planning would enhance post‐mining restoration.     

Leaf litter decomposition and macroinvertebrate assemblages along an urban stream gradient in Puerto Rico

Urbanization is a major land use form that has large impacts on ecosystems. Urban development in the watershed impacts stream ecosystems by increasing nutrient and organic matter loads, altering hydrology, and reducing biodiversity. Puerto Rico is an ideal location to assess and monitor the effects of urbanization on streams, because it is increasingly urbanized and streams do not receive inputs of untreated sewage, characteristic of many other tropical urban areas. The objective of this study was to determine how leaf litter decomposition and aquatic macroinvertebrate assemblages varied along a tropical urban gradient. We conducted the study in the Río Piedras watershed, San Juan Metropolitan Area, in six low‐order streams that formed an urban gradient ranging from 10% to 70% urban land cover. At each stream, we placed six 5 g leaf bags of Ficus longifolia in three different pools and collected one bag on each sampling date. Decomposition rates were fast in forested streams (range 0.021–0.039/day) and decreased with increasing urbanization (range 0.007–0.008/day). Rates were strongly and negatively correlated with percent impervious surface cover (R = 0.81, p = 0.01). Functional feeding group diversity was higher in forested streams, with the presence of shredders. Decomposition rates were significantly and positively correlated with functional feeding group diversity and abundance (R = 0.66, p = 0.04). Overall, our results show that urbanization affected the environment and macroinvertebrate diversity resulting in large negative effects on stream ecosystem function. Abstract in Spanish is available with online material.     

Response of aquatic hyphomycete communities to enhanced stream retention in areas impacted by commercial forestry

1. Aquatic hyphomycetes are an important component of detritus processing in streams. Their response to enhanced stream retentiveness was tested by manipulating three streams located in Kielder Forest (northern England), a large plantation of exotic conifers, and two streams in Montagne Noire (south-west France) dominated by native broadleaf woodland. Treatment was by placement of logs or plastic litter traps into a 10–20 m stream section. Fungal spores were collected from stream water upstream and downstream of the treated sections over 1–2 years.
2. The average concentration of fungal spores in reference sections was nearly 10× greater in the French streams than in the English streams. The number of hyphomycete species was also higher in the French streams. These differences between regions were probably a consequence of the much lower standing stock and diversity of leaf litter in the English streams.
3. Despite these large regional differences, the treatment had a clear effect in all streams. Detrital standing stocks were enhanced in treated sections by up to 90% in French streams and 70% in English streams.
4. Mean spore density below treated sections increased by 1.8–14.8% in French streams and 10.2–28.9% in the naturally less retentive English streams. The number of fungal species increased significantly below the treated sections of the English streams, although not the French ones.
5. In biologically impoverished plantation streams, input of woody debris can increase detritus retention and enhance hyphomycete diversity and productivity. This may have consequent benefits for detritus processing and macroinvertebrate production.     

Inter‐regional comparison of land‐use effects on stream metabolism

1. Rates of whole‐system metabolism (production and respiration) are fundamental indicators of ecosystem structure and function. Although first‐order, proximal controls are well understood, assessments of the interactions between proximal controls and distal controls, such as land use and geographic region, are lacking. Thus, the influence of land use on stream metabolism across geographic regions is unknown. Further, there is limited understanding of how land use may alter variability in ecosystem metabolism across regions. 2. Stream metabolism was measured in nine streams in each of eight regions (n = 72) across the United States and Puerto Rico. In each region, three streams were selected from a range of three land uses: agriculturally influenced, urban‐influenced, and reference streams. Stream metabolism was estimated from diel changes in dissolved oxygen concentrations in each stream reach with correction for reaeration and groundwater input. 3. Gross primary production (GPP) was highest in regions with little riparian vegetation (sagebrush steppe in Wyoming, desert shrub in Arizona/New Mexico) and lowest in forested regions (North Carolina, Oregon). In contrast, ecosystem respiration (ER) varied both within and among regions. Reference streams had significantly lower rates of GPP than urban or agriculturally influenced streams. 4. GPP was positively correlated with photosynthetically active radiation and autotrophic biomass. Multiple regression models compared using Akaike’s information criterion (AIC) indicated GPP increased with water column ammonium and the fraction of the catchment in urban and reference land‐use categories. Multiple regression models also identified velocity, temperature, nitrate, ammonium, dissolved organic carbon, GPP, coarse benthic organic matter, fine benthic organic matter and the fraction of all land‐use categories in the catchment as regulators of ER. 5. Structural equation modelling indicated significant distal as well as proximal control pathways including a direct effect of land‐use on GPP as well as SRP, DIN, and PAR effects on GPP; GPP effects on autotrophic biomass, organic matter, and ER; and organic matter effects on ER. 6. Overall, consideration of the data separated by land‐use categories showed reduced inter‐regional variability in rates of metabolism, indicating that the influence of agricultural and urban land use can obscure regional differences in stream metabolism.