找回密碼
 To register

QQ登錄

只需一步,快速開(kāi)始

掃一掃,訪問(wèn)微社區(qū)

打印 上一主題 下一主題

Titlebook: Biogeochemical Monitoring in Small Catchments; Refereed papers from Ji?í ?erny,Martin Novák,R. Kelman Wieder Book 1995 Springer Science+Bus

[復(fù)制鏈接]
樓主: Eisenhower
21#
發(fā)表于 2025-3-25 05:15:39 | 只看該作者
22#
發(fā)表于 2025-3-25 09:26:41 | 只看該作者
23#
發(fā)表于 2025-3-25 13:04:45 | 只看該作者
Randomized Intervention Analysis of the Response of the West Bear Brook Watershed, Maine to Chemicall acidification and therefore provided an objective basis for determining whether changes in the geochemical behavior of West Bear Brook were temporally associated with the chemical manipulation. RIA analysis using weekly data yielded higher probabilities of stream water chemistry effects being temp
24#
發(fā)表于 2025-3-25 15:59:25 | 只看該作者
25#
發(fā)表于 2025-3-25 20:53:05 | 只看該作者
Biotic and Abiotic Processes Controlling Water Chemistry During Snowmelt at Rabbit Ears Pass, Rocky en ion was hypothesized to be generated from nitrification in overlying soils, and subsequently exchanged with other cations, particularly Ca...Solute concentrations in streamwater also decreased as snowmelt progressed. Variations in groundwater levels and solute concentrations indicate that most of
26#
發(fā)表于 2025-3-26 01:43:16 | 只看該作者
The Relationship Between Dissolved Organic Matter and Percolation Water Chemistry in Northern Finlan cm in the percolation water. Organic matter thus plays an important role as an anion in percolation water, and regulates water pH in the surface soil. A high proportion of dissolved Al was in the form of organic complexes. Total dissolved Al levels were well below the toxic limits for pine.
27#
發(fā)表于 2025-3-26 07:12:01 | 只看該作者
28#
發(fā)表于 2025-3-26 12:16:56 | 只看該作者
29#
發(fā)表于 2025-3-26 13:10:34 | 只看該作者
30#
發(fā)表于 2025-3-26 19:54:30 | 只看該作者
Sulfur and Oxygen Isotope Ratios in Sulfate During an Acidification Reversal Study at Lake G?rdsj?n,f sprinlding water S with a larse reservoir of Sin the catchment. Oxygen isotopes in SO. suggest that less than one third of the SO.in runoff is secondary SO. formed within the soil profile. This is, however, no evidence for net mineralization of S. The SO.in runoff in the roofed catchment is a mixt
 關(guān)于派博傳思  派博傳思旗下網(wǎng)站  友情鏈接
派博傳思介紹 公司地理位置 論文服務(wù)流程 影響因子官網(wǎng) 吾愛(ài)論文網(wǎng) 大講堂 北京大學(xué) Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點(diǎn)評(píng) 投稿經(jīng)驗(yàn)總結(jié) SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學(xué) Yale Uni. Stanford Uni.
QQ|Archiver|手機(jī)版|小黑屋| 派博傳思國(guó)際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-5 23:06
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved
快速回復(fù) 返回頂部 返回列表
香格里拉县| 陇川县| 巴南区| 文山县| 城口县| 健康| 通许县| 顺义区| 凤城市| 大庆市| 双鸭山市| 绥中县| 甘肃省| 成武县| 长汀县| 长治县| 铜川市| 聊城市| 闻喜县| 闽侯县| 墨江| 休宁县| 平凉市| 万荣县| 老河口市| 邯郸市| 濉溪县| 邓州市| 禄丰县| 三江| 长春市| 乌拉特前旗| 宁乡县| 康定县| 静宁县| 留坝县| 北海市| 勐海县| 宝兴县| 利辛县| 铜陵市|