Integrating security services into active network by Mandala, Satria

“…The results demonstrated that the authentication based on RIPEMD320 was faster than MD5 and SHA-512., and SHA-512 is more secure than the others.…”
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Seasonal variations in the production of singlet oxygen and organic triplet excited states in aqueous PM_2.5 in Hong Kong SAR, South China by Y. Lyu, Y. H. Lam, Y. Li, N. Borduas-Dedekind, T. Nah, T. Nah

“…The steady-state concentrations of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M24" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">1</mn></msup><msubsup><mi mathvariant="normal">O</mi><mn mathvariant="normal">2</mn><mo>∗</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="3384aa7ffb179d44625d28560eedc465"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-9245-2023-ie00006.svg" width="20pt" height="16pt" src="acp-23-9245-2023-ie00006.png"/></svg:svg></span></span> (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M25" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mo>[</mo><mn mathvariant="normal">1</mn></msup><msubsup><mi mathvariant="normal">O</mi><mn mathvariant="normal">2</mn><mo>∗</mo></msubsup><msub><mo>]</mo><mi mathvariant="normal">ss</mi></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="35pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="3dc8809c0abfc5c578d475066b7ec0cf"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-9245-2023-ie00007.svg" width="35pt" height="16pt" src="acp-23-9245-2023-ie00007.png"/></svg:svg></span></span>) in the illuminated aqueous extracts ranged from <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M26" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1.56</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">14</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="61pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="9c5a326545b955cc9b0d562ee1f5e4db"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-9245-2023-ie00008.svg" width="61pt" height="14pt" src="acp-23-9245-2023-ie00008.png"/></svg:svg></span></span> to <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M27" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1.35</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">12</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="61pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="60822f320d98056184688cb2abd07f09"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-9245-2023-ie00009.svg" width="61pt" height="14pt" src="acp-23-9245-2023-ie00009.png"/></svg:svg></span></span> <span class="inline-formula">M</span>, with a study average of <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M29" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>(</mo><mn mathvariant="normal">4.02</mn><mo>±</mo><mn mathvariant="normal">3.52</mn><mo>)</mo><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">13</mn></mrow></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="101pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="4bf043ac094446adaada68d8bc2e7280"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-23-9245-2023-ie00010.svg" width="101pt" height="15pt" src="acp-23-9245-2023-ie00010.png"/></svg:svg></span></span> <span class="inline-formula">M</span>. …”
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Performance assessment of state-of-the-art and novel methods for remote compliance monitoring of sulfur emissions from shipping by J. Beecken, J. Beecken, A. Weigelt, S. Griesel, J. Mellqvist, A. V. Conde Jacobo, D. van Dinther, J. Duyzer, J. Knudsen, B. Knudsen, L. Ntziachristos

“…The two UAV-borne systems showed total uncertainties of 0.07 %S<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><msub><mi/><mrow><mi>m</mi><mo>/</mo><mi>m</mi></mrow></msub></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="12d9eb1e045e9dfbf3e43b362e1bac69"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-16-5883-2023-ie00003.svg" width="21pt" height="11pt" src="amt-16-5883-2023-ie00003.png"/></svg:svg></span></span> and 0.09 %S<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><msub><mi/><mrow><mi>m</mi><mo>/</mo><mi>m</mi></mrow></msub></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="21pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="64d1c2f2157ab0fae55f99226af90828"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-16-5883-2023-ie00004.svg" width="21pt" height="11pt" src="amt-16-5883-2023-ie00004.png"/></svg:svg></span></span> (confidence level: 95 %). …”
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Nonlinear increase in seawater ⁸⁷Sr&thinsp;∕&thinsp;⁸⁶Sr in the Oligocene to early Miocene and implications for climate-sensitive weathering by H. M. Stoll, L. D. Pena, I. Hernandez-Almeida, J. Guitián, J. Guitián, T. Tanner, H. Pälike

“…<p>The <span class="inline-formula">⁸⁷</span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="fb147fccdcf98a9911cf3d26a8f6dc33"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00004.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00004.png"/></svg:svg></span></span> <span class="inline-formula">⁸⁶</span>Sr of marine carbonates provides a key constraint on the balance of continental weathering and hydrothermal Sr fluxes to the ocean, and the mid-Oligocene to mid-Miocene period features the most rapid rates of increase in the <span class="inline-formula">⁸⁷</span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="165b352473919034209a9d51d0eaf41d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00005.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00005.png"/></svg:svg></span></span> <span class="inline-formula">⁸⁶</span>Sr of the Cenozoic. …”
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All about nitrite: exploring nitrite sources and sinks in the eastern tropical North Pacific oxygen minimum zone by J. C. Tracey, J. C. Tracey, A. R. Babbin, E. Wallace, X. Sun, X. Sun, K. L. DuRussel, K. L. DuRussel, C. Frey, C. Frey, D. E. Martocello III, T. Tamasi, S. Oleynik, B. B. Ward

“…These measurements and comparisons to data from previously published OMZ cruises present additional evidence that <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="91b2e19ca239409a7665981c17575147"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-2499-2023-ie00002.svg" width="25pt" height="16pt" src="bg-20-2499-2023-ie00002.png"/></svg:svg></span></span> reduction is the predominant OMZ <span class="inline-formula">N</span> flux, followed by <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">2</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="5437eb9d658a57482749982e166d9cca"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-2499-2023-ie00003.svg" width="25pt" height="16pt" src="bg-20-2499-2023-ie00003.png"/></svg:svg></span></span> oxidation back to <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">NO</mi><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="25pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="8a872e45f44a0fc3c08e466e371cfb3a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-2499-2023-ie00004.svg" width="25pt" height="16pt" src="bg-20-2499-2023-ie00004.png"/></svg:svg></span></span>. …”
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Impact of seawater sulfate concentration on sulfur concentration and isotopic composition in calcite of two cultured benthic foraminifera by C. Thaler, C. Thaler, G. Paris, M. Dellinger, D. Dissard, S. Berland, A. Marie, A. Labat, A. Bartolini

“…<p>Marine sediments can be used to reconstruct the evolution of seawater [SO<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">4</mn><mrow><mn mathvariant="normal">2</mn><mo>-</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="13pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="fa6a3d1c655e3a1a9feb31b6a98317a5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-20-5177-2023-ie00001.svg" width="13pt" height="17pt" src="bg-20-5177-2023-ie00001.png"/></svg:svg></span></span>] and <span class="inline-formula"><i>δ</i>³⁴</span>S over time, two key parameters that contribute to refine our understanding of the sulfur cycle and thus of Earth's redox state. …”
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Mercury emissions: is there a global problem? by Agamuthu, Pariatamby, Mahalingam, R.

Igelströmite, Fe³⁺(Sb³⁺Pb²⁺)O₄, and manganoschafarzikite, Mn²⁺Sb³⁺₂O₄, two new members of th... by D. Holtstam, J. Langhof, H. Friis, A. Karlsson, M. Erambert

“…The chemical formulae obtained from microprobe data are (Fe<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M25" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.59</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="d43d1c6a3be7ea5d73cd4f08ab914c56"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00005.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00005.png"/></svg:svg></span></span>Mn<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M26" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.29</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="b5c2d6f052ef8a3fee22175c0ad1dfb3"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00006.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00006.png"/></svg:svg></span></span>As<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M27" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.06</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="0707f5b25701720c5fba3eaa01f3f3c3"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00007.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00007.png"/></svg:svg></span></span>Fe<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M28" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.06</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup><msub><mo>)</mo><mrow><mi mathvariant="normal">Σ</mi><mo>=</mo><mn mathvariant="normal">1.00</mn></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="48pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="1e37653d7511c381dd72e410d5c64d41"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00008.svg" width="48pt" height="17pt" src="ejm-36-311-2024-ie00008.png"/></svg:svg></span></span>(Sb<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M29" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">1.24</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="f4ca1d81a3c46e11fbcb87c6e933beb4"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00009.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00009.png"/></svg:svg></span></span>Pb<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M30" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.65</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="45b81d3d5fba892b6553eba8f35ae914"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00010.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00010.png"/></svg:svg></span></span>As<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M31" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.11</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup><msub><mo>)</mo><mrow><mi mathvariant="normal">Σ</mi><mo>=</mo><mn mathvariant="normal">2.00</mn></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="48pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="9f7f0f2df4270ea5d5e63ae6b0c533b8"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00011.svg" width="48pt" height="17pt" src="ejm-36-311-2024-ie00011.png"/></svg:svg></span></span>O<span class="inline-formula">₄</span> and (Mn<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M33" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.64</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="051214e530adde4de45aa309d1d71f93"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00012.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00012.png"/></svg:svg></span></span>Fe<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M34" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.25</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="70b75d55936a4c5fb54e336b44634e75"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00013.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00013.png"/></svg:svg></span></span>Mg<span class="inline-formula">_0.08)_Σ=0.97</span>(Sb<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M36" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">1.97</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="57b733a4b1b09ec3d3267384ff391792"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00014.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00014.png"/></svg:svg></span></span>As<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M37" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.03</mn><mrow><mn mathvariant="normal">3</mn><mo>+</mo></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="18pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="445868f998f29d252be01d28d4510b44"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00015.svg" width="18pt" height="17pt" src="ejm-36-311-2024-ie00015.png"/></svg:svg></span></span>Pb<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M38" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">0.01</mn><mrow><mn mathvariant="normal">2</mn><mo>+</mo></mrow></msubsup><msub><mo>)</mo><mrow><mi mathvariant="normal">Σ</mi><mo>=</mo><mn mathvariant="normal">2.01</mn></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="48pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="5820e6cc1507d90bde2b0a2a617105b7"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-36-311-2024-ie00016.svg" width="48pt" height="17pt" src="ejm-36-311-2024-ie00016.png"/></svg:svg></span></span>O<span class="inline-formula">₄</span>. …”
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Pick Your Nose: Customizable, Low-cost, Biocompatible Implants for Craniofacial Reconstruction by Gillian O’Connell, George Corpuz, Hector Salazar Martinez, Nicholas Vernice, Xue Dong, Jason Spector, MD

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LeFort I Horizontal Osteotomy: Defining the Feasibility of the “High Osteotomy” by Alexandra Verzella, Bachar Chaya, MD, Jill Schechter, Andre Alcon, MD, Pradip Shetye, Roberto Flores, MD

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Used electrical and electronic devices - is it a waste or resource? by Agamuthu, Pariatamby, WenJi, A.

Single use sin cre poducts and its waste management challenges by Agamuthu, Pariatamby

Challenges in public health and sanitation for greener environment by Agamuthu, Pariatamby

Editorial: extended producer responsibility (EPR) by Agamuthu, Pariatamby, Venu Mahendra, M.

Editorial: waste pickers: the unspoken friends of the environment by Agamuthu, Pariatamby, Rubashiny, V.

Food security, the environment and a brave new world by Agamuthu, Pariatamby, Khidzir, K.M.

Feeling the heat of global warming by Agamuthu, Pariatamby, Khidzir, K.M.

Waste management in the wake of a disaster - are we prepared? by Agamuthu, Pariatamby, Khidzir, K.M.

The Asian Tsunami of 2004 - lessons learnt by Agamuthu, Pariatamby, Khidzir, K.M.

Solid waste management in developing economies - need for a paradigm shift by Agamuthu, Pariatamby